TABLE OF OONTENTS BY VOLUME NUMBER Volume Number Table of Contents INTRODUCTION I. PRE-EXPLORATION ENVIRONMENTAL RECONNAISSANCE SURVEYS II. ENVIRONMENTAL BASELINE MONITORING PROGRAMS A. Hydrology and Water Quality ie Streans 2. Springs and Seeps 3. Ground Water Air Quality 1. Air Quality and Surface Meteorology 2. Low Altitude Meteorology 3. Upper Air Studies ae Vasibi lity. 5. Atmospheric Diffusion Studies ee tee ED, TV References Gees brolosy. 1. Terrestrial Wildlife Studies 2. Aquatic Studies 3. Terrestrial Vegetation Srudies 4. Soil Survey and Productivity Assess- ment Studies Vv ieee Cine. STUDEES A. Fish and Wildlife Management Plan (inactive) B. Revegetation Program C. Microenvironmental Program D. Aerial Photographic Program (inactive) E. Archaeological Studies (inactive) F. Scenic Values Program (inactive) at “y Seggabtorna i oe a2 bg oc thas i =e 7 ,- a OO oe ee Pid . > a ve 2 : 2o% ~ if : cr r ie = : 7 7 ; — -" - ==: Pe 7 fo ges Nig nu 96 : iene es ieee ~ a. ee a reas ee) gr) 7 i a al 7 > : 7 1 - a ; _ Pi * iu i Peer e / FF in , 7 ‘oe : ¥ = ‘ > § é J : @ = a Dad 5 ¢ - “ ALR MONITORING REPORT FOR €=p "SHALE MOLL P ROUECT MARCHVALO 7:7 REPORT NOv 31 20 June 1977 Presented to: C-b Shale Oil Project United Bank Tower Denver, Coi1orado 80202 Peeparea by Ragan Sear e IT B-1098 RADIA CORPORATION TABLE OF CONTENTS I. GENERAL DESCRIPTION OF AIR MONITORING PROGRAM-------- II. DESCRIPTION OF INSTRUMENT SYSTEMS-------------------- A. Air Quality Instrumentation---------------------- B Calibration Procedures--------------------------- C. Data Acquisition System-------------------------- D. Meteorological Instrumentation------------------- IIL. MICROMETEOROLOGICAL AND TERRAIN FEATURES ------------- IV. OPERATING TIME ANALYSIS FOR EACH SITE---------------- V. MONTHLY METEOROLOGICAL SUMMARY ----------------------- A. Summary of the Meteorological Conditions over North America during March 19/77------------------ B.: Summary of the. Meteorolosical® Conditions in Northwesterm amd West Central Colorado during March 1977--------------------------------------- C. Summary of the Meteorological Conditions in the Oi] Shale Trace s€=b Region during March 19/7--—-—- VI. DATA PRESENTATION AND SUMMARY------------------------ II B-1099 Page {1 B-110¢ RADIAN CORPORATION TABLE +E TABLE IT TABLE -ELE Rist OF. TABLES Page DOWNTIME HOURS FOR C-b SHALE OIL PROJECT Site 023-------------------------------------- II: B-1123 Site 023-------------------------------------- -1124 Site 023-------------------------------------- 1125 FEDERAL AND COLORADO STANDARDS------------ rai -1141 AVERAGES FOR MARCH 1 THRU 31 Nitrogen Oxides (NO,)---------------~---------- ~1145 Nitrices.O0xide ((NO)-5—---—-<-- 5-5-2 ee -1143 Nitrogen Dioxide (NO,)------------------------ -1143 Sulfur Dioxide (S02) -------------------------- “14:43 Pyranometer----------------------------------- ~AAS Hydrogen Suifide------------------------------ -1143 Total Hydrocarbons---------------------------- -1143 Methane= 22 = = a ew == 1143 Non-Methane----------------------------------- ~1143 Carbon Monoxide------------------------------- -1143 Ozone--~------~--------~---------------------- =1145 Barometric Pressure-~------------------------- =1143 Total Precipitation--------------------~------- -1143 Particulate--------~---~-------~----~----------- -1143 Wind Speed------------------------------------ -1144 WandwpareC G1 Os = 2 = ease = a a ne ee ae -1144 Relative Humidity----------------------------- -1144 hemp eimatutea ===> a ee ee en -1144 fi B-1100 RADIA CORPORATION LIST OF TABLES (contd) Page a TABLE IV DALLY AVERAGES FOR MARCH 1 THRU 31 TABLE V Nitrogen Oxides (NO) ~------------------------ II B-1146 Nitric Oxide (NO) ----------------------------- -1146 Nitrogen Dioxide (NO,)------------------------ -1146 Sulfur Dioxide (S0O,)-------------------------- Say Pyranometer----- === <= - 2-9 3 == - -1147 Hydrogen Sulfide------------------------------ =—1147 Total Hydrocarbons------------~--------------- -1148 Methane----~-------~--+-------------- ~---------- -1148 Non-Methane Hydrocarbons---------------------- -1148 Carbon Monoxide------------------------------- -1149 Ozone-- --------------------------------------- -1149 Barometric Pressure--------------------------- -1149 Total Precipitation----------------~----------- -1150 Particulate----------------------------------- -1150 Wind Speed------------------------------------ ~lislg Wind Direction-------------------------------- S52 Relative Humidity----------------------------- =155 Temperature----------------------------------- =1154 MAXIMUM FIVE-MINUTE AVERAGES AND TIME OF OCCURRENCE FOR MARCH -E-THRU TSE Nitrogen Oxides (NO. ) ~~~ ----------------- ----- -1156 Nitric Oxide (NO) ----------------------------- -1157 Nitrogen Dioxide (NO,)------------------------ -1158 Sulfur Dioxide (SO,)---------~----------------- -1159 Pyranometer----------------------------------- -1160 Hydrogen Sulfide---=----------------=<---------- =116ol Total Hydrocarbons ---------------------------- =IOZ Methane--------------------------------------- =LE6S Non-Methane Hydrocarbons---------------------- -1164 Carbon Monoxide------------------------------- -1165 Ozone-- ----------- - - rrr rrr rrr -1166% IT B-1101 RADIAN CORPORATION List OF TABLES (contd) Page PABEE. MAXIMUM FIVE-MINUTE AVERAGES AND TIME OF TABLE VEL OCCURRENCE FOR MARCH 1 THRU 31 Barometric Pressure--------------------------- Th BoL67 Total Precipitation--------------------------- 21168 Wind Speed-Wind Direction--------------------- -1169 Relative Humidity----------------------------- 1170 Temperature----------------------------------- “1171 THE FIVE MAXIMUM INDEPENDENT SLIDING AVERAGES FOR MARCH 1 THRU 31 Nitrogen Oxides------------------------------- “157.9 Nitric Oxide---------------------------------- = 1175 Nitrogen Dioxide------------------------------ 11/5 Sulfur Dioxide-------------------------------- =A Sulfur Dioxide - 24-hour---------------------- -1174 Hydrogen Sulfide------------------------------ -liy5 Total Hydrocarbons---------------------------- shI7S Methane--------------------------------------- “1176 Non-Methane Hydrocarbons---------------------- =r, Carbon Monoxide - 1l-hour---------------------- =1178 Carbon Monoxide - 8-hour---------------------- =i 79 Ozone------------------------------- eer -1180 | Particulate----------------------------------- =1181 FUNCTIONAL DEPENDENCE OF RECORDED PARAMETERS UPON WIND DIRECTION Nitrogen Oxides (NO. ) ----~----------~--------- =1183 Nitric Oxide (NO) ----------------------------- -1184 Nitrogen Dioxide (NO,)------------------------ -1185 Sulfur Dioxide (S0O,)-------------------------- 21186 Hydrogen Sulfide (H2S)------------------------ =LLe7 Total Hydrocarbons ---------------------------- -1188 SBS 1107 BPA A ed J CORPORATION LISY OF TABLES: Ccontd) Pace TABLE WEE EUNCTIONAL DEPENDENCE OF RECORDED PARAMETERS TABLE Vitt UPON WIND DIRECTION Methane--------------------------------------- II B-1189 Non-Methane Hydrocarbons---------------------- -1190 Carbon Monoxide------------------------------- -1191 Ozone----------------------------------------- =1TOZ DIURNAL VARIATION OF VARIOUS RECORDED PARAMETERS Nitrogen Oxides------------------------------- = 1194 Mastic Osc ce =AIgS Nitrogen Dioxide------------------------------ -1196 Sulfur Diextde@— === =. eee eee ee eee eae -1197 Hydrogen Sulfide------------------------------ -1198 Total Hydrocarbons-~---------------------------- =1 199 Methane-------------------------------+-------- -1200 Non-Methane Hydrocarbons---------------------- -1201 Carbon Monoxide-------=++---=345--=+-<--<-_-2- -1202 Ozone-- ----------------------------~----------- -1203 Hourly Total Precipitation-------------------- -1204 Wind Speed 8 feet-----------------------+------------ -1205 30 feet-----------------~------------------ -1206 100 feet----------- --—-------------- pee ee -£207 200 feet----------------------------------- -1208 Wind Direction @ feet 262650 = = ee ee ee -1209 30 feet----------------------------------- =12700 100 feet----------------------------------- -1700 200 feet---------------+-+------=-~-----=---=- -1212 EL SB1103 RADIAN CORPORATION LLSE OF GABLES (|Ceontd) TABLE WiLL DIURNAL VARIATION OF VARIOUS RECORDE PARAMETERS Wind Direction Standard Deviation Horizontal Wind Direction Standard Deviation 30 feet------------------------ DO UEckeOe ba a= ee ee eee ee ee ee eee Relative Humidity WO Gein ee hese a a a ae a eee ee DOMES 6 be = 2 ee Sar ee ee Fee ee Temperature DOO kets =a ae a es Houciky= LObal. colar Radiation —-=—=—— = Temperature Change from 30' to 100'- Temperature Change from 30' to 200'- Barometric Pressure----------------- Bi-~Vane Wind Speed BOushe Cie ee ee ee ee eee eee II B-1104 D ire 2A D9 TA CORPORATION bist OF TABLES (€eonted) TABLE VELL DIURNAL VARIATION OF VARIOUS RECORDED PARAMETERS Horizontal Bi-Vane Wind Direction 30 rice ha sae ae See ee ee eS Vertical Bi-Vane Wind Direction 30 teero == 25 Se er ae See ee Nitrogen Oxides--------------------------- Nitric Oxide------------------------------ Nitrogen Dioxide-------------------------- Sulfur Dioxide---------------------------- Hydrogen Sul fide-------------------------- Total Hydrocarbons------------------------ Methane-- --------------------------------- Non-Methane Hydrocarbons------~----------- Carbon Monoxide-----~---------------------- Ozone- ------------------------------------ Hourly Total Precipitation---------------- Wind Speed 200 i B=-a105 Page r TT B-1255 S250 RADIAN CORPORATION BESt OF TABLES (Ceonitd) Page TABLE” VIELE DIURNAL VARIATION OF VARIOUS RECORDED PARAMETERS Relative Humidity 8 feet----------------------------------- II B-1260 30 feet----------------------------------- -1261 100 feet---------~------~------------------- -1262 200 feet----------------------------------- -1263 Temperature 8 feet--------------------+--------------- -1264 30 feet----------------------------------- -1265 100 feet----------------------------------- -1266 200 feet----------------------------------- s207 Barometric Pressure------------------- 2-2-5" -1268 Solar Radiation------------------------------- -1269 Bi-Vane Wind Speed 30 feet---------------------------------- “1270 100 feet---------------------------------- -1271 200 feet----------------~------------------- Led 2 Horizontal Bi-Vane Wind Direction | 30 feet~---------------- ~--------~-------- =t27/3 100 feet---------------------------------- =k274 200 feet---------------------------+------- -1275 Stability Class Determination Using Pyranometer Recording------------------------- -1276 Stability Class Determination Using DT/DZ (Level 1)------------------------------- =i277 Stability Class Determination Using DT/DZ (Level 2)------------------------------- -1290 II B-1106 RADIAN CORPORATION EIST OF TABLES Ceontd) : Page APPENDLX A - STABILITY WIND ROSE DIAGRAMS= ----=-2=---==>2>- II B-1304 200-f£oot lével== Stability Class“As->--—--——-— SOK Class B----------- -1308 Class C----------- -1309 Class D----------- =1510 Class E----------- = 1501 Class F----------- -1312 Clases total-2--=-4 = GS Percentage of Occurrence of Wind Direction for 200 Foot Level-------~------------------------ -1314 ET BaviG7 RADIAN CORPORATION Les GENERAL DESCRIPTION OF AIR MONITORING PROGRAM Radian Corporation, under contract to the C-b Oil Shale Project, is performing the data compilation and reporting of air quality/and meteorological data at one monitoring site in Northwest Colorado. The site measures and records concen- Exaetons) Of Pareloulates sulfur dioxide, }oxides of nitrogen, hydrogen sulfide, total hydrocarbons, methane, and carbon monoxide. A 200-foot meteorological tower provides wind direction, wind speed, temperature, and relative humidity data aterour. levels 0S, 305) 100 and 200 feet)!" Other meteorological variables measured at the tower site are insolation, barometric pressure, “and precipitation. Evgure tleshows the confieuration o£ the monitoring station. The station provides a sturdy and protective covering for the monitoring equipment. ET B-8108 NOITLIVLS ONiY¥OLINOW HO NOLavduGidNOd SATE RA RIE BE NY St — | | | ! | ROvaS XUOM A YOSS3udKOS ee ee y | pees oN | ; i | YaUV LNSHNULSNX YALA | : : 1 ] f | j! A, A/C | | | — | qovas wuon | Fora { a2Ho ell Aan same: © ae Paes Se, igen a ead tae Pate L sees IH Bi rt . s = z 3 | Beaheatete Salk | \ t ' bass == La--~J agen malas = 3 ~ : af at) th ' YILEJANZ ——— SIVYOLS AYIALIVZ hoou FILLod 3A01V O | YIV 0xaz O) |: —— ee ee YLV OUSZ II B-1109) RADIAN CORPORATION ee DESCRIPTION OF INSTRUMENT SYSTEMS A. Ate Quality Instrumentation Nitrogen oxides are measured with a Meloy Model NA520 analyzer. This dual-channel analyzer is based on the chemilu- minescent principle and continuously monitors both NO, and NO. A subtraction circuit in the instrument provides a continuous NO>. Output. .bweos not used in Radian’s system....NO, is cal- culated once a second by the computer by subtracting the NO value from the NO, value, thus avoidine any drift, which might occur in the NO, output of the instrument. This instrument has a minimum detectable sensitivity of 5 ppb (parts per billion) GG wa plein aiken Oi. 2 hoe Both sulfur dioxide and hydrogen sulfide are measured with Meloy Model SA185 sulfur analyzers. The hydrogen sulfide analyzer uses a Meloy Model NO,-1 sulfur dioxide scrubber and the sulfur dioxide analyzer uses a Meloy Model H,S-1 hydrogen sulfide scrubber. The Model SA185 is a continuous analyzer and “utilizes the flame photometric principle of operation. The minimum detectable sensitivity is 5 ppb and the linearity is +1%. Ozone is measured with a Meloy Model OA350 analyzer. This instrument, based on the chemiluminescent principle, pro- vides continuous measurement of ozone. The minimum detectable Sleris tiiewaney, SOND. DpDmendsthe linearity 1s 217, Total hydrocarbons, methane, and carbon monoxide are monitored with a Bendix Model 8200 gas chromatograph analyzer. This instrument, which uses a plume ionization detector, has a minimum detectable sensitivity of 5 ppb for all three components. The Model 8200 works on a five-minute cycle, i.e., one air sample is analyzed every five minutes, and the results are dis- played for five minutes via a sample and hold circuit. Dil) Sead al a0) RA DIAM CORPORATION The air sample is drawn in through a glass cane and manifold supplied by the Ace Glass Company. The system has a 25mm diameter, through which a constant air flow is provided by an air pump rated at 60 cfm at O" head pressure. The manifold has sampling ports to which 1/4" teflon lines to the instrument are connected. All joints in the sampling system are secured by O-ring compression fittings. The manifold ts contained in a heated (100°F) chamber to prevent condensation of moisture. The teflon lines from the manifold to the instruments are insulated with 1/8'' wall thickness rubber tubing. The trailer has four heavy duty high volume particu- late samplers (Hi-Vols). Fiberglass filter paper is used for the collection of particulate samples, after which each filter is brought to a controlled humidity before weighing. Each Hi- Vol has a flow recorded to permit correction for changes in air flow as the filter becomes loaded with particulates. Each Hi- Vol runs for a 24-hour period (midnight to midnight) and is turned on and off by the computer. The Hi-Vols, which were manufactured by Radian, were designed following guidelines re- commended by the Environmental Protection Agency. In addition to the normal Hi-Vol particulate samples, a duplicate Hi-Vol sample is collected every sixth day on special filter paper for trace element analysis. Once each quarter these samples are composited and analyzed for gross radioactivity and trace element content. B. Calibration Procedures The trailer contains a Meloy Model RAD-1 calibration unit. This instrument provides a zero air supply, SO, span gas from an SO. permeation tube, and NO span gas obtained by precisely ET Bat) RADIA CORPORATION diluting bottled NO span gas. The computer-controlled calibration of all instruments is automatically performed once a day. « gLacheiarstaument aus siirs.t tswitchedptopzero; ‘the computer monitors the output of each channel and takes a new zero reading after, a stable »zero signal has been.reached.. This zero reading is compared by the computer to the zero reading obtained 24 hours be fone, ratid +1. gamdruni: tim excess .o£.10 «ppb .has,occurred, an excess zero drift light.for the channel .in question is turned on on the System Status Panel. Next, span gas is supplied to each channel and the computer decides when a stable span value has been reached. This value is recorded and compared to the previous day's value. An excess span drift light on the System Status Panel is BUGRed On pl — vaedrlet -excecdime, 10 ppb joccurs..0ihesinstruments are then returned to the monitor mode and after two minutes the com- puter resumes data taking. The bottled NO gas used at each site was obtained from Precision Gas Products. Pre-purified grade hydrogen is used in the SO, analyzers. The SO, permeation tubes were manufactured by Metronics Association, Inc. Their output, has been verified by comparison to the output.of National, Bureau of Standards tube 10-42. Both SAL85 analyzers in each trailer are calibrated with the SO... from the permeation tube. This instrument responds to the number of sulfur atoms per molecule; thus, SO, can be used to calibrate both the H,S..and SO>. monitors. The Model OA350 ozone analyzer has its own calibration system which provides a zero check and a span check. The ozone Galibwatton system 1s, veri tiedsby comparison, to, a,.calibrated ozone generator maintainec in Radian's laboratory in Rifle. PL B-1t42 Be Sida CORPORATION a The Model 8200 total hydrocarbon, methane, and carbon monoxide analyzer is calibrated with undiluted span gas obtained from AirCo's Rare and Specialty Gas Division. This span gas con- tains methane and carbon monoxide in air, the methane being used to calibrate both the total hydrocarbon channel and the methane channel. The Model 8200 is zeroes with air from a Bendix Model 8834 zero air uit. “in addition, the ‘instrument “is ‘electronically re-zeroed. at the start of every five-minute cycle. The Hi-Vol particulate samplers were calibrated using a Calibration Kit from General Metal Works. C> ‘Data Acquistit2 on. System The basis of the data’ acquisttionssystem is ay Data General NOVA 1200 minicomputer. The NOVA, which has a basic cycle time of ‘1.2 yseejiis equipped with automatic program load — and power fail/automatic restart features. The computer utilizes 16K 16-bit words of core memory. Analog-to-digital conversion is accomplished via an ADC built by Radian, Comperation. The input/output unit for the system is Texas Instrument's KSR 733 keyboard/printer. This model teletype provides keyboard entry and hardcopy printed output. The data are also recorded on a cassette magnetic tape unit with three drives. The cassette unite is’ werlized’ for: program -storage.-and loading as well sas for recording. To reduce wear on mechanical parts, the power to the teletype and cassette units is turned on only when the unit(s) is (are) to be used. Several important functions in the instruments as well as in the computer and the trailer are monitored by means of lights on a System Status Panel. These data lights are written onto cassette tape to monitor the complete status of the system every five minutes. The Data Acquisitiom System also monitors the presence of 100V power from the power lines. In its absence, e. the computer, which is powered by batteries, switches all trailer J fog 3 lB RADIAN CORPORATION systems to battery-provided power. If the line voltage is restored before the batteries are discharged to a specified level, the trailer system is switched back to line power. De Meteorological ins triumen tat Lon 200-Foot Meteorological Tower The tower has instrumentation at four levels: 8 feet, 30 feet, 100 feet, and 200 sftect;,.At all four levels, there are: wind speed, wind direction, and temperature and relative humidity sensors in a power-aspirated radiation shield. Temperature difference thermistors (also in power-aspirated radiation Snietds) sandrthnerr assocratedycineuLtry take, lapse: rate umeasure= ments for sthe 30-foot to; l00-foot: Layer and the: 30=foot :to 200 -footu layer, pi inweaddition » thisrsite nas a PrecisioneSpectral Pyranometer, a barometer, and a tipping bucket rain/snow gage. The wind direction and speed apparatus used at each measurement level of the tower is the Model 1074-2 wind sensor by Meteorological Research, Inc: (MRI). This sensor has a 540° potentiometer for wind direction and a light chopper for wind speed. This sensor is rugged, with an all-weather coaxial cup and damped vane assembly. The prototype model has been in operation for years under the most demanding weather conditions, performing continuously with the utmost reliability. The wind sensors on the tower have been specially treated with a black paint which will promote warming of the exposed surfaces of the sensor and thereby reduce ice and snow accumulations on the MOVIN oparespomythegapparatus. Lihetspeci fications ion .the Model 1074-2 are as follows: Ba RADIAN CORPORATION Wind Speed Starting Threshold: "10.75 mph. Résponse Distance: “16 feet (637, recovery). Flow Coefficient. 7.19 Leer /Revolution. Accuracy: +0.4 mph or 1% (whichever is greatest) Wind Direction Starting “Thresholds =:0275> mom. Delay Distance: 4 feet (50% recovery). Dampine “Ratio 22 -0'co co. se Accuracy (540° system): 1%. Ranges 0 eo" 540 ~. The relative humidity and temperature sensors are mounted within a power-aspirated radiation shield at each tower level. All aspirators and sensors are of the Model 840 Series by MRI. ‘The aspirated shielded housing is designed to provide maximum radiation protection to the sensor. Ambient air is drawn into the shield and across the sensors at approximately 15 feet per second. This intake air is essentially sampled from a hemispherical space which is approximately 3-inch radius rom the tube opening. Speed of the incoming air at the perhiphery of this hemisphere is approximately 1 mph. The temperature sensor is comprised of a dual thermistor and resistor network. This circuit provides a linear resistance change with an air temperature change. The relative humidity sensor is placed alongside the temperature elements inside the shield where it is exposed to a constant flow of air. Circulation to both sides of the sensing element produces accurate monitoring with a good response time. The specifications on the sensing ele- ments are as follows: TE B-1255 Dati CORPORATION Temperature Accuracy : £OL25. Ge Ranger.) -90°C to 450° C- Humidity ANeeuracy='r+3.07, Rox Range: 07, to L007, Relative Humidity. Measurements of temperature difference are taken for two layers, the 30-foot to 100-foot and the 30-foot to 200-foot layer. Uline thermistors andecircuitry used for these measurements are separate from the thermistors measuring air temperature. The use Of separate thermistors and circuitry to measure AT allows for much greater accuracy and resolution in the measurements, which is necessary for stability assessments. Two AT thermistors are at the 30-foot level, one is at the 100-foot level, and one is at the 200-foot: hevel. All of these AT, thermistors: are mounted within power-aspirated radiation shields. The specifications on the AT instrumentation areas follows’: Accuracy: +0.1°C. Range of AT Circuit (Lower Level-Upper Level): +9F° to -9F°. All instrumentation, except at the ground level, is mounted at the end of 12=foot retractable booms. These beoms are B-aneh box beams which are ‘om rollers and’ can’ be- retracted to the instrument platforms for instrument maintenance. The meteorological tower itself is a 200-foot Rohn Model 80 Guyed Tower, designed for 40 pounds per square foot wind oad wither: at cadtalmce per ELA’ Standard RS-222-B to EERE SIG CORPORATION support four levels of meteorological equipment. The material © consists of tower sections with a tapered base, three retractable booms 12-feet long, three outside work platforms, an inside ladder for climbing, two base ground kits and one anchor ground kit. The cable-type Safety Climbing Device consists of a cable and attachment mechanisms with a locking sleeve and safety belt. The tower is lighted and painted according to FAA specifications. The signals from the tower instrumentation are fed from multiple signal cables into transmitters mounted at the base of the tower. After signals have been converted to analog signals, they are fed into a junction box, also at the tower base, where they are assimilated into one coaxial cable. The signals.are. then. run. underground within:3". PVC conduit to the A-to-D assembly, where they are processed. The transmitters are shielded and insulated from the elements. The signal cable is run underground in PVC conduit.in order to minimize damage from > the weather or from various rodents in the region. The auxiliary equipment at the tower site consists of a heated tipping bucket rain/snow gage, an analog barometer, and a Precision Spectral Pyranometer. The rain/snow gage is the Model P511-E unit by Weather Measure... In. the case of this gage, the durability and reliability of a tipping bucket gage are combined with heavy-duty electric heaters to make this an all- purpose precipitation sensor. This gage may be used to measure both snowfall and rainfall. An insulating cover of poly-vinyl chloride and a thermostatic control insure the proper gage temperature. The thermostatic control is adjustable from 0 to 35°C. Snow falling into the inlet funnel is melted. The resulting water (from rain or snow) drains into a precision tipping bucket mechanism which activates a mercury switch each time the bucket fills ‘and tips ...,The gage is constructed of durable corrosion- resistant materials to provide many years of service. The . ET ‘B=f117 RADIAN CORPORATION specifications for this gage are as follows: Omistice., Uj6- inches.. Calstbratvont-er OF O01 lanchs Aeeumacy «MOM om Cal i baated at: Or; 5oinm/hr) . Sensor: Chrome-plated tipping buckets. Swisteh= p Mercury, 00l-second sclosure. Heat. Control yihermostat adjustment, 0 to 35°C. The barometer is the B242 Analog Output Barometer by Weather Measure. This barometer provides an output voltage that is linearly propontional’ to pressure. “The specifications on’ this instrument, which is mounted inside the monitoring trailer at the Siee. are as follows’: Range: Specially designed for the 100 millibar imeenvial i£nOm 7251 middda barse to 825 millabars: Resolution. Infinite. bimnéanuty-) 20.5 millibar, over the 100 milinbar Intervals The pyranometer at the site is the Eppley Precision SpecteralyPyranometer. ~0his instrument is usedifor)the measure- ment of sun and sky radiation totally or in defined wavelength bands. The pyranometer is levelled and mounted atop a wooden stand 4% feet from the ground surface. Care has been taken to eliminate the effects from all outside influences, such as reflection or shadows, on the pyranometer. The instrument Chacacterista cs) are vasy fol lows’. Sensttiviitv: govmy. | pier cal/cm°/min. Independence: 300 ohms. Temperature dependence: Sensitivity constant to within +l percent over the ambient temperature range from -20 to +40°C. HW B-di 18 RADIAM CORPORATION Linearity: Response linear up to intensities of 4 cal/cm?/min. Response time: 1 second (i/e signal). All instrumentation -1s ‘factory-calibrated and is field- calibrated at vartousTintervals') Stine -psychrometers are used to calibrate the humidity sensors; known temperatures and/or resis- tances are used to calibrate the thermistors; and an rpm cali- brating wnit is used to. calibrate the vanemometens, “ine wand direction instrumentation is aligned to true north (reference direction) by means of a surveyor's transit. TY B19 RADIAN CORPORATION igGile MICROMETEOROLOGICAL AND TERRAIN FEATURES The Piceance Creek Valley and C-b Shale Oil Tract are Situated such that many microscale meteorological phenomena affect the region where the ambient air monitoring unit is located. Trailer 023 and its associated 200-foot meteorological tower are located atop a plateau to the south of the valley, high enough to be affected mostly by gradient flow conditions. The elevation at the meteorological tower site (Trailer 023) is 6940 feet above sea level. The largest gradients in eleva- ELON, im this area,, Of course, occur at the Piceance Creek Valley walls. However, the northern valley walls are slightly steeper than those at the southern boundary of the valley, which then slopes upward gradually toward the C-b Tract. . The Piceance’ Creek Valley decreases in elevation from’ east ‘to west in this area, so that nighttime katabatic cold-air drainage flows advect from east OrWwie oner Site 023- is approximately 2.5° miles*‘south of the Preeance Greek Valley" This Yocation is relatively high’ com- pared to its surroundings, with the nearest point having an eleva- tion greater than 7000 feet being .5 miles to the south of the tower. The tower itself is om the £op of a small knoll located between Scandard and Sorghum Gulches. Because of its location and the irregularities of the suxrounding terrain, meteorological patterns are varied here. Wind instrumentation is mounted at four levels of the meteorological tower: 8 feet, 30 feet, 100 feet, and 200 feet. Tne top level of the tower generally remains in gradient wind flow. © (nat as. the winds at, that level “are mormally generated fel Bel 20 RA DAA CORPORATION by synoptic-scale features and are usually separated from terrain features and mrerometeorotocical-~crreulations. occasionally a weak anabatic flow influence is experienced. However, such is not the case with the three lowest measurement levels. To varying degrees, these levels are influenced by both the katabatic and anabatic circulation cells. However, when strong pressure gradient forces exist in the region and the synoptic-scale wind flow is strong, all four tower levels will reflect a gradient wind flow as the winds increase in strength and height. The terrain atop the plateau is generally barren and fairly rugged, with a few scattered small trees. The topsoil dries rapidly and is very fine, resulting in blowing dust when dry, windy conditions exist. “Im the. Piceance Creek Valley tne terrain is fairly grassy and flat, with steep valley walls on either side. Surface winds are normally rather light in this valley unless channeling effects occur. During clear nights with rather light pressure gradient- induced winds, rapid radiational cooling will oceur in the reerven because of the barren nature of the terrain and the generally dry character of the, air in this: poreronm Of Ene. countm.. = Aca result, the diurnal range of temperatures will be extremely large. Because of the katabatic flow in the valley, nighttime temperatures will generally be lower in the valley than on the plateau. During the winter, especially, temperatures in the valley may be 20F° lower than they are on the plateau during the early morning hours. fi B-di2t RADIAA CORPORATION EV. OPERATING TIME ANALYSIS FOR EACH SITE ihitse seceron presents the operating statistics for each of the major subsystems contained in the monitoring station. Tabde ei shows tehee speci ire number of-hours -that .each.of these subsystems were inoperative for the month. The column labeled “DEGLOPIZING SYSEEM = amdicates the- entire data acquisition system; therefore, downtime hours appearing in this column means total loss Of data.” These instances. imclude,-in «addition to computer downtime, power failures, no power available, and self-automated shutdown periods’such as during air conditioner malfunctions. Calibration time is not considered to be downtime and ES jenererOne, snot included) im=the downtime figures. » The amount Of time used in calibrating the instruments is given atthe bottom of the downtime analysis table and is reported as total Calibration hours for each channel for the entire month. As is evident in the calibration figures, channels can be calibrated independently of one another. No calibration time is given for particulate monitoring since Hi-Vol calibration occurs infre- quently and only during the off-duty“ cycle-for each Hi-Vol while another Hi-Vol is taking data. 1g 3 eed Ll Wt > -} ed {} $0) th fy ') () (i ua) © 2 hy EN = ISA o 11 nt 1) ae) Fa | Gera} t. | arte (1 ale 1 2 0 () oun t} ai) ' . 1 (a es mh caer ay Phan 'y ~ ay !) ar ie gal a Pai) 1\ ey {1 Sei hy = tt e ‘ W t) Spee i bam i ba fh 1) oi \ es { is Vy ey ao oy 1) oy i) Paths ) be ‘) ear {og Ci 3 | MOIAVHOAUOD AIT TAP y ‘ , . yf € ip © ~ Sa Lf — ae ~ mm 21a 1G) Tess =A ) ‘) =a() tre qui ‘) Ws g>t ia) 1a) ty bys Sic nL, 1) e “ 4) oan “1 Sin 1) Stipes Sais ee 0) al ea A) Gers F oO Ne 1) ae * Pig? =) hie Lar i are) Serf y re Onn Ome - 1) ae ie) eA) 2 id oan Vie Oni mle =) hen ai atte? “1 . Sails) SC Nhaes a Whig? 210) Calli a “1 are, CA) oat | 7? *1) Say eri) tir? “1 ooh) oar) ie. "71 Sine P| crerie| {TAPES Speen: 2) } yen | cr NOMwWNRoANOD ~ eS SS +r 1tB-1i24 ~ SS Os SS ~~ a - ar con ~~ SN gh FNS! BN EE ora CO el ig) 56) ey 4 Sy a nae *() Sale XH) Sityied 1) Saliies mat) "ne? aa Ste 4) eho will) rate 0 a (he. 2) stares “ty "61 sat lie “a(t "ti? a(t "te ea) “ti? mai) eth? a0) ote 0 she 0) a hc a) ae Fe ab) * te oa) * tr aa) “he CUSIA “Sr Sk 5 a “1 ° 1) “4 5 orn 5 on . oi . cl “$e att) elke, = Sue =A) Ste at) Sitti? > ( whe = () thé? it) Oe wat Pan tnves ati me fine? “aa ealine eat) male aa) Taeyal =A) "2 sat) ith Sati ot =) tHe 1) “2 an ai) arf "Ve mae wi Ce 24) alti =i) a Fed CUGA 2G L/ ‘A 0 )) bi? haga atin cay ariel Ler Soi eo = ih) sail 3 ca! | iy) { e a Ve > ee a bet 7) “4 ee es a 2 Ba We e > Sve sats J 7 e Wee e ce . aby? tr? « at 2 oa Hires . ate ON ed . Se? * he . Sa tities! ering? ° ase, Gore: . tn oie ° pa i beep “hie . Ste Pe) . OR, "he * * sibel . s Oi ie . ( s “we > a rd eta? . 2-6) ars . ee ee * ba ae e ee e “tre “ti s ty > fiat es Chie ai es . "2 aan aired e beet res oa D e “hie? 5 tre? i FrCUSe sy —Gapeey Ft) Lee yal 1) =i) att ) Sty Sot | Sey kl ero 7 Qf catites ory Vie hie mt tien? mabe: ear Sa ete Salli i? Sale? “yy iv? Mth ye Eat Wiles ~ 2 malt teed “19.2 =a) ae? Nee Salt ty be baat 4? ro? ma V2 nd at bie aa) cd a ud Att toe: Piles mat} tr f mts || 0 pe Salles sae be? “We “(i ty J ata ee, dar yo ing = a0 tee avid "u art *t¢ mall ji? aes ei) Wie? rahe cf $) a ou the? “HH? a) ne "aed me thes Sle? *() eG * PWG odes pie | 1 “1, oy ae a) mat) 2G) ak i () Ai) rae mail 3 ti Cen oy @ 1 s “4 ony eu oar a J 4) can or ® ‘) te nae bath ° {) Sra =H) ali ? t) * 1 on lei oe #4 Ore Orn . ft sath raft seats > c) oan “(1 or . (1 mle =a) mals . ) “4 eet aa as (! may =i) = o (\ th fis Laan ° {3 sai ei ° rs tis bar Cons bea fT} . {\ sa) be lar e ( Sal ah Cr cat * ( = meal sity a) oat) Sty * ‘ ) bat Sat) + a ( ar dat) ey * f ea ae mi 7 aie at ei i () rl) at) . « () Son SiN Shin . () =) ae eit e () en aaa . « 1) ee wry Saath : (\ ory ety ern bs Mie Cot (Gig, ore ese get , ‘ NOATUeduUo2a / / i 4? SS oe ™ ON SSeS Ne Re ON ESS NS ENS SS OSS Do on a a a iW B=1t25 Lt ve ef Othe a Ce elle eth. a a ng RADIAN CORPORATION V. MONTHLY METEOROLOGICAL SUMMARY A. Summary of the Meteorolocical, Conditions over North America during March 1977 March 1977 brought warmer than normal temperatures to the eastern two-thirds of the United States. The Rockies and West Coast experienced near normal temperatures. Monthly precipitation totals were quite variable over most sections of the country. The polar front jet stream was somewhat less developed than in earlier months and also changed its orientation. The long wave circulatory pattern for March featured a mean trough in the western United States and a long wave ridge in the eastern United States. The reverse was true during the winter months preceding March. The ridging in the eastern and central sections of the country accounted for the above normal tempera- tures in thosé-areas)durine.March. The long wave circulation was zonal (west-east) from the” 7th through’ the 9en-and “che, loth throweh thes 22nd,"-*Spiie Elow occurred om the 2nd and’ 3rd trom,the, lth throtgh the Lethe and’ from the Zoth throwsh= the S0th! —~Meridional’ (north- south) flow. oceurred.on the lst, from the- 4th through. the 6th, on-the- 10th, “the: 14th... amds 1 oich, from tie 23rd through: the’ 25th’, and’ on’ the Sisit- Extratropical low pressure systems were frequent in Ene United States during March. these low pressure systems” typically increase in number during the spring months because of the interaction between warm and cold air. The region most affected by these low pressure systems was from the Rockies G@astward sehwzough, ithe Great Plaims.... The, dates and locations. of these low pressure systems were as follows: IT B-1126 RADIAN CORPORATION Este 2nd: Sparel 4th- (sick Qehr: LOtheatZehe IPs elgie EACh:: PSth— eta: layed ae TSth: 1S al ghee 20th: 22nd: 23rd: 24¢h: 2 Sittin: Vl fad ae 28th-30th: SS tis Sen : On a sectional basis” Southwest Rockies Great Plains Lakes AtLlantre Seaboard Great Pacific Northwest Great Plains Great Lakes New England West Coast Rockies Great Lakes Northern Rockies Atlantic Seaboard Atlantic Seaboard Great Lakes, Great Lakes, New England, Pacific Northwest New England, Northern Rockies Rockies Northern Rockies Creat Plains New England precipitation anomalies existed during March. Section Northeast Atbantuc..Seaboard North, Centrad Central Southeast Southwest Rockies West ‘and Pacirftire Northwest Temperature Much above normal Much above normal Very much above normal normal Much above normal Above normal Slightly above normal Variable Near normal Variable Near normal SB 27 Variable; the following temperature and Precipreation Much above normal Near normal mostly above Near normal Below normal Slightly below normal RADIA CORPORATION B. Summary of the Meteorological Conditions in Neonthwes tern sand West, Central-Colorado, during March 1977 Grand iJunmetion)sCollomado,.sixty miles: to the,south- southwestcotutherinact iC=bis neceived a -totall of .0.. 50, inch of precipitation sdurime March xewiich is, 0.25 -inch below the: monthly normaksor On/asginchas Grand Junction received 2.3:sinches of; snow during March. Measurable precipitation occurred on the lst, 2ad= 10th jo2 56h 226th). cand 32th. q,dhe- regiom received./8, percent of the possible monthly sunshine. Sky.-cover by cloudiness averaged 5.5 out of a possible 10 during the daylight hours and 4.7 4OuUEVOE pa possi bile.10, duxing,.the entire tmomth.'. The region had eight clear days, thirteen partly cloudy days, and ten cloudy days during the month. Air mass changes were frequent during March. Eight frontal passages occurred during the month. These frontal passages occurred regularly as an upper-level trough dominated the western United States throughout the month. Temperatures in the Tract C-b were cool due to seasonal influences. Transport winds over the region as a whole were stronger in March than in February. Maritime spolar Jcold tfronitalwpacsages -oecurred::on the) list,a:8th; Genewi3thselothiw24th.) and. 2/thepoAnweale-contamental)polar cold frontal passage occurred on the 20th. ET B-1128 Fe AD igard CORPORATION C. Summary of the Meteorological Conditions in the Oil Shale Tract €-b Region during March 1977 An upper-level trough which had a mean position over the western United States was responsible for the increased frequency of cold frontal passages and increased number of precipitation ‘occurrences’ duxing March so Precipi tatronsoceusred on? the bsp f 2nd > beth Ss -ESthi a Zorn. 26ene andaZzoth vos Marcher Temperatures in the Tract C-b region were near normal during March compared to the above normal temperatures which occurred in the easter United “States. Eight cold frontal passages occurred during March. Maritime polar ‘cold frontal passages ‘oceurred.on”“theslse , “Sth; 9th, 13th, loth, 24th, -and 27th =: A weak continentalspolarc. cold frontal passage occurred on the 20th. The monthly average temperatures recorded at the meteorological tower during March were: 28.4°F at 8 feet; 27.7°F ati 30 feet; 27.8°F at 100 tfeet; sand-26-4°F -at <200bfeet. These averages are approximately 1F° lower than those recorded in February. The warmest days of the month were the 9th, 23rd, and the 24th. The coolest days were the 4th, 5th, and the 29th. The highest temperature recorded at the meteorological tower during March was 56°F at the 8-foot level om the 23rd. The coldest temperature recorded at the meteorological tower was 4°F at. the 30-foot bevel on the morming of ther 29cm. Monthly average relative humidities during March were higher than they had been in February in the Tract C-b region. This increase can be attributed to a decrease in monthly average temperatures. At the meteorological tower, the monthly average relative humidities were: /0.2 percent-2@ 6 feet: 74.1 percent at 100 feet; and 69.6 percent at 200 feet. These relative II B-1129 RADIAN CORPORATION humidities correspond to dew points of 1Oe Srey, 20 Seek and 17°F, respectively. The relative humidity sensor at the 30-foot level was inoperative for most of the month. The most humid days of the month were the! 2nd, 3rd, 4th,: 10th, and 26th. The driest daycuwerey Ehescchta ith .1eh loth, 23nd; Destin, moni SS . Wind speeds on the meteorological tower during March were stronger on the average than the winds that prevailed during February. Resultant wind vectors at the meteorological cower during Macch were as follows sm 216.8 degrees at 2: /emiles per Houraty Onieet; 2iy/.S degrees tate3..94 milles;per. hour! at 30 feetrwre20 49 decrees «ates. Simi les: per hourat 100.ceett: ands 226. 9 degrees at 5.4 miles per hour at 200 feet. The scalar average wind speeds associated with these resultant windsvectorss were. 6s 8.10". and, 11. mides. per. hour, respeetavelys |= Therikman spiralwand Ekmanyeftecti,, d.e:4-a) veering in direction and increase in speed as a function of increasing height above the surface, were in evidence during most of March. A reference, to the March wind rose. For. the meteorological tower indicates that the winds at that location were primarily southwesterly. The windiest days of the month at the meteorological Gowers wener Chie. 9thyi LOthie 1Sthd 4 2Gthe ) andy ithe :725th is, dhesdavys having. the, Uichtest wandsy were) the 3xdi,. 5th,» 22nd... and: the; 26th. The highest five-minute average wind speed recorded at the tower duning March. was; (40 miles pexm hour’ at, ithe: 200-foot: level. on. the 2 Brahe. Precipitation totais: in, the, bract. C-b Monitoring .Net- work during March were generally below normal. Although precipitation occurrences were more numerous than during February, amounts were light. RE B= 50 RADIAN CORPORATION Only 0.45 inch of precipitation was recorded at the meteorological tower during March. The largest daily precipi- tation total recorded in the network during March was 0.13 inch on March 2nd. The greatest five-minute precipitation total re- corded during the month was 0.02 inch (a precipitation rate of 0.24 inch/hour), tecorded om the Vstsul/th. and 26th») Measurabte precipitation (+701 inch) ° was recorded at «Che meteorological tower ‘on’ the= ls 39 2nd dy the. Sth 2othey och tande2oehe em cme precipitation was in the form of snow. The monthly average station pressure during March was 783.9 millibars at the meteorologieal. tower 92 This treading is 6.7 millibars lower than the February average station pressure of 790.6 millibars. The highest daily average station pressure occurred on ‘the’ Sth® throtigh’ the: - Sth .sven> 2ist2and the 22nd. The lowest daily average station pressures occurred on the lst, 2nd. 17th, and the 23th Cloudiness increased in the Tract C-b region during March, compared to the February cloud cover and insolation statistics .- The region received an“insolation cotal of 4057224 langleys, which is equivalent to a daily average insolation total of 346 langleys/day. This average is below the normal for March of 440 langleys/day in the’ Tract C=b- ‘region-2-0n’ a’diurnal. basis, the greatest solar radiation rates occurred between 1200 and 1300 hours. The greatest daily radiation totals were received on the Sth, 22nd, 23rd, and the 27th: *ihe- Lowes @ daidly solar tadiation totals were received on! the. 2nd, 4th). LOth® W7th- and the:/29th- The greatest five-minute radiation total received during March was 7.80 langleys (a rate of 1.56 langleys/minute) , which occurred om the 30th.’ The largest™hourly’ insolatrom total re- ceived ‘during March-was /1 Langleys~ which eccunred son ther? 7th between 1200 and 1300 hours. II B-1131 RADIAN CORPORATION Because of the progressively increasing solar elevations and the increasingly longer periods of daylight that prevailed during March, the total possible solar radiation which could be received during a day increased monotonically throughout the month. Therefore, even though cloudiness increased during March compared to February, the actual amount of solar radiation received also increased. The increase in cloudiness which affected the Tract C-b during March caused the "very unstable" stability classes to become less common than they had been in February. Using the Pasquill method of stability determination, "D" stability (neutral stabality)=was the most common>stabilrty “occurring during 189 daytime hours, or 54 percent of the time. In de- creasing order of Erequency, “"C’ (slightly unstable) stability ecclsred: durimne LiZeiours, or 32 percent of ‘the time’, andd"B” (very unstable) stability occurred during 46 hours, or 13.1 percent of the time. "A" (extremely unstable) stability occurred during only three daytime hours. Using the lapse rate method of stability determination ey thegneveral ('D”) » sitently stable ("E"), and extremely stable ("F") stability classes were the most prevalent during March. In general, stable and/or neutral conditions prevailed during the nighttime hours and unstable and/or neutral conditions prevailed during the day. The following table is a diurnal breakdown of the various stability classes. As one proceeds frome Ay to. UF", the stability class ranges from extremely unstable to extremely stable. The column labeled "number of oecurrences indicates the number of times a particular stability elass (OCecusredaduring Eheamoneh on an hourly basis.< Level: I presents the temperature change versus height values eo Ene were considered between 30 feet and 100 feet. Level II indicates the, values that were considered between 30 feet and 200 feet. fl B=115Z CORPORATION RADIAN 09 Cole 2 Gabe Eo OO HO. 0! = O20" *0s0. O90) 0 <6 ck “64 Saeko Ge Ss “ a7! ClmaGG (Gi Tt Cl-7 40, 407 (0: 80> 0. 030 O60: 0. 9 68 iG. 60> KCL eCT acl. 2 7a 02¢ Gy On “Groat 2 eS SOladl yb bh el vw et. OTL 9.30138 S685) Ghat 49 met 8S TC. OG. ok AG tC BOL Gh: ONG Mie a” See RC eo oO! AB At eC ee 20 8ct GO G ute Ue. 9 +6 MALL GL GL Once ig OL GS 6: 72 GG 97 OSL: OH A SY mi G6 CAC STC = ale Ae ee a ee, SG ED OE aay EY eee. Ae 8 iG aL 7V FOIA IO V6 cco. LG OC Gl BE LE SIL ET Cl RL3OL 6 8: 2 9S % © Ce al anol/ SSPETO JO °ON AATTEWeIS ZP Lanes A225 00 OF ASF OF C4) TI TWAgT aTqeris Ayowaryx9 3; eTqeas ATAYSITS 34 [eijneu :q aTqeqysun ATAYyBTTS :9 eTqeaisun ADA 3G atTqeasun Ajyowsaaqyxo iy SLT Otel Cl Gl be0..0' 0:0 90 —C- 0:50 “0O-.02 9 AL Vt Yl Ot 8k Vt ul ar Cor Ses oiee Ll (OCnee 20s O20: AO. 60: “00-20 <¢c) 4th iay 9s = G 658 68 7a €SZ Mea 6 o nso AO Uk Viol Ch GLuel Glee TL aclGb 1) al 8° 8-6 - 8 -( Gc? Cpe OrerOre rt: SOM 20 eis Oh D0) 3 Pr Oe Ge Ges Cl ek Oe 0-8 ad 0 20 70 68 OFe0) 20 = 0: 0.20 eS OL SEL ULE G O29 2£ 0° 20-0 0-0) 10-0. = 0 > EE PSO Oe ™ 0) aOR On me Ne Sab Se rey: 2G Seg TO OO SO Ore): 40 30 :V SQOUSAIMNIIO! BVG (66 366 16 OG GL Sl -£L OL St Ol el cL-bL O16 8 £ 9° S & Ge TL ino} / SSeTo jO “ON AATTEWQeIAsS 199J OOT 01 1995 OF Ss) IL THADT IT B-1133 RADIAN CORPORATION Using the standard deviation of the horizontal wind (o.) method of stability determination, yDe= stability waisi-the hose common stability classification at the meteorological tower at the 200-foot level because of the moderately strong winds that normally occurred at that*location. )*The stability distributions for the 8-, 30-, and 100-foot levels were unavailable due to instrumentation problems. The bivanes at the 30-, 100-, and 200-foot levels of the meteorological tower indicated a pattern of upward vertical motion (negative vertical directions) during March. Upward vertical motion was more pronounced during the nighttime and early morning hours at the 100-foot level during March (probably because of low wind speeds). Upward motions were less pronounced at the 200-foot tower level during the early morming hours. At the 30-foot level, downward vertical motions were greatest during the daytime hours, a result which is quite unusual con- sidering the proximity of the sensing level to the ground. Upward vertical motions were greatest during late evening and nighttime hours. No comparison may be made of o 5 values between the bivanes and standard wind instrumentation because of instru- mentation problems. PiB- Pis4 RADIAN CORPORATION ae DATA PRESENTATION AND SUMMARY This section includes summaries for various recorded data at the monitoring sites. The data presentations indicate the variability of pollutant concentrations and meteorological parameters with .location»and’ time.ssin-addition,.the presenta- tions indicate the functional dependence of pollutant concentra- tion with wind direction. All data except suspended particulates (24-hour samples) are sampled once each second, but recorded as five-minute arithmetic averages of the one-second samples. This averaging technique tends to smooth instantaneous maximum values, and is especially evident when comparing wind gusts to local weather bureau data. Inherent to any data acquisition system is random noise both from the recording instruments and quantization in the ana- log-to-digital conversion. The lower threshold for all analytical instruments is twice the maximum noise level generated by the instruments: This Lower threshold iso ppbi'‘for all anstruments , except for the ozone analyzer, for which it is 0.5) ppbse There fore, any values appearing in the data presentations that are less than 5 ppb indicate only a trace of pollutant in question and should not be construed to be absolute levels. In addition, the recorded quantity is simply random noise and averages tend toward zero. Thus, when concentrations are below the lower threshold of the analytical instruments they may appear as a zero entry in the data presentation which does not indicate absolute zero concentration. All pollutant data (execept.for partieulate data) is taken at the monitoring site in integer parts per billion (ppb) but is presented here in micrograms per cubic meter (yg/m?) EE B= 1155 RADIAN CORPORATION assuming standard temperature and pressure of 25°C and 760 mmHg COS 72; militbars ) 7 Gespecoively a “Lhe scale cfactions: required EO Convert Ue/m uae seandard conditions back {to.ppb for sthe VarLous, pollutanes sare given iIn-the folleowangitable. TO CONVERT ug/m? AT 25°C AND 760 mmHg TO ppb MULTIPLY BY POLLUTANT . 034 54 234 .384 a pea: A, O50 15,56 sOplal we The units of the meteorological parameters are given in the table. It should be noted here that inside temperature is monitored ’andiréecordednas;a,£unctional part ofthe system but is NOE presentedsinyChishixreport: Table III displays the monthly statistics for each MOND COmine (stati om combhenmonih.uvio. insure statistical sig- nificance, and to reduce the possibility of introducing a bias in the presentation, averages are computed only when at least 30 percent of the samples are present, except for relative humidity and temperature, in which case 75 percent of the samples are nequired.9 Dftlesstthan «the required samples are present for a particu Vax jparameter,; that .mtryy will be blank. The number of II B-1136 RADIAN CORPORATION samples present for a particular channel is detuned sas the total possible number of five-minute samples for the averaging time less the computer downtime less the channel downtime less the channel calibration time. .The averages in Table III are arith- metic averages with the following exceptions: « Wind speed and wind direction are computed using a vector averaging technique where the wind speed is treated as the vector magnitude. - Particulate averages are computed as the geometric mean. Table IV displays the daily averages. Again, 50 percent of the five-minute samples are required in order to compute an average except for the cases of relative humidity and temperature which require 75 percent. A blank entry indicates an insufficient number of five-minute samples present for that day. Wind speed, wind direction, and particulate averages are computed the same way as described in Table IIL. Table V presents the maximum daily five-minute average retained in the data base as well as the time of occurrence. A five-minute maximum average is printed if any samples are present for that day. Therefore, the maximum five-minute] average for a channel which experienced considerable downtime or calibration time during the day in question may be mMisnepresentative of, the maximum expected for that channel on that day. Table VI indicates: the! fiveiilarcest® averages for various averaging times. The table shows the period of time covered by the average. Maxima are chosen so that time segments EY-B-£037 RADIAN CORPORATION are independent. The maximum averages reported are found using a 'sliding average' technique with the exception of the 24-hour particulate average, which is computed from midnight to midnight. For averaging times less than or equal to three hours, the slid- ing average is stepped one five-minute sample at a time. For longer averaging times the step size is twelve samples or one hour. For averaging times less than or equal to one hour 100 percent of the five-minute samples must be present to compute an average. Averaging times greater than one hour require 90 percent. Whether or not a sliding average is computed is solely determined by the number of samples present in that averaging time and is independent of daily and monthly averaging criteria. To demonstrate the functional dependence of recorded parameters upon wind direction, Table VII shows pollutant con- centration displayed in a bi-variate distribution with wind direction. The tables display the total number of five-minute samples occurring in each concentration and wind speed class. The mean concentration for all samples occurring in each wind class are also shown. This distribution demonstrates the dependence of high pollutant concentrations upon wind direction. Appendix A shows the stability wind rose diagrams. The wind speed classifications used in Appendix A are based on the Beaufort wind scale classification system. This is a system of estimating and reporting wind speeds, invented in the early nineteenth century by Admiral Beaufort of the British Navy Uri wassoricinally based on the effects of various wind speeds on the amount of canvas that a full-rigged frigate of the period could carry, but has since been modified and modernized. Im ats present form for amternational meteorological use it equates: (a) Beaufort force (or Beaufort number); (b) wind speed; EB Lise RADIAN CORPORATION (c) descriptive terms; and (d) visible “effects upon land objects or the sea surface. One land adaptation is the NRM wind scale. The six basic wind speed classifications used in the report are: » L-3 knots, 4-6 knots. J-l0 knots. LI-16 knots, 17-21 knots, and winds of greater than 21 knots. The following table is a complete description of the Beaufort Wind Scale, taken from Physical Climatology, by Helmut Landsberg, 1969. BEAUFORT WIND SCALE FOR CBSERVATIONS AT LAND STATIONS Specification for Use at 10 meters ab.grd. 5 Mi/hr. j “Knots! 70 g/m? 55 ug/m* 45 ug/m* 24 Hr. Max.* 260 150 150 200 180 150 Sulfur Oxides Annual 80(.03ppm) =~ 60(.02ppm) 25(.009ppm) 10(.004ppm) 24 Hr. Max.* 365(.14ppm) 15(.005ppm) 300(. 1lppm) 150(.05ppm) 55(.02ppm) 3 Hr. Max.* -- 1300(.5ppm) ~~ -- ~- -- 1, Hr. Max.** -- -- -- 800(.28ppm) 300(.lppm) - Oxidant 1 Hr. Max.* 160(.08ppm) 160 8 Hin. “Max. * -- == Annual a — Cc Hydrocarbons 3 Hr. Max.* 160(. 24ppm) 160 6-9 a.m. Carbon Monoxide Max. 8 Hrs.* 10000 (9ppm) 10009 Max. 1 Hr.* 40000 ( 35ppm) 40000 Nitrogen Dioxide Annual 100(.05ppm) 100 Units are micrograms per cubic meter and ppm in parenthesis. *Not to be exceeded more than once per year. **Not to be exceeded more than once per month. II B-1141 RADIAM CORPORATION TABLE -i£f1 AVERAGES FOR MARCH 1 THRU 31 Il B-1142 II B-1143 = oe & ow & Of a = =O ot se ae Fe oo om ae Se am Oe 6b 68 ee we 8 SO oe ee a ee oo © et SB eS a et ee Se 8 oe oe 8 rm) ne OO ee oe oe me OF ew 8 ee SO mY em be me ee 8 eR a a OH oe e ° 5 g 4h 620) yo mE aS TPM IN OT Leite eT fy ea a Aoi] A R24 Hey fs G21) ; ¢ 1) bat PS as PASSING DTN anna Woe Jap Cueto apse oe we ey oe oe ae ee Oe a ee we ey a om we ome ae i ee ee om OY OW Ow OW Oe OP ah mt me Ge ae em ee ee et me ey ee se sO eet ee ee ew me ee he et te ee te me try As eee 4° GOS bP avd tee g 2 $7% $ 2K) dss SNOMHMVOOMGAR ANVIL QWenNge 4dauVeid date Gees prpraech aad py pe ee ee ee ee ee ee ee ee eee On ee ee eed oe eit eS ee LO ee §20 % 4) Sigrid 417s IL AIG NIDQONGAH MAL AMON SoA CEOS Feet Or TES e° 2° a ¢2n G70 wr ow A — - C20) AarKeOtad NAO Te (ON) AAT YO DENI (2 VS gee} eo Cre nie a SQJHINT=NOTLVITATIA a PSYVOT TIL We TGS aed POAATI YT We bed aii add SN SRL OW LITASIAM HLTM SAIN aceny LP you Gate fp aaa 4 8 749M) ae Tey] yea M1 SMNOH MAA SQTwengJae Ang Pe gb au Ape) Mad ShyhoeazCeeGeap leah more e bbe) TS MeL of ve Mod Gay dav FLEE 4 psewd NOLLYWUuOdNOD II B-1144 b°92 G°/e PA2 pee (l4-002) Cl4ecgol) (}4-09 ) (1 j= ) Se Anos AMIDE VA ad 9° 9 ote 2 Mice) Cis=002) Ch 4deoot) Cl 4—e0g (L4e4) ALVTOP!onH AALty14y h*922 6° Ade Ts urate (14-002) (14-007) (t4-95 ) (l4ea ) gan alte NOTIOAINTO ON os fie emt) Aes eee (14=002) CtL4denot) (L4-o¢g ) (1 fev ) Scie = IAI TES “+ VIYIdS Cope CSIRO TSMR VIF AT VINA SMUT TIN anes age 292 FIST Tesi aay ering os SHIN Ful Of 1DIAS 4! LTE SINAN ema ly 7 pepo Gupte PLU Veit dette Gy ded Dead bore ager gy SHNOH MA SAVE e-49dS atte Puagtae aang wda SUV VAT les Gey PE yonl a wm ye Sf Tne) Acie alT 13) bi SI AES! = Se Sepa oor Te) Thelen iyi| ( f RADIAN CORPORATION TABLE IV DAILY AVERAGES FOR MARCH 1 THRU 31 II B-1145 Svit=d Tt y° n° Oe Le 43 () ¢ le os us/y BHP7SY ws ' Os tr 'y® “LGLS i) es ie ud/ys ()° Qs ie ueS4 (Gm we ans Wess Qt ts ioe Creeps cal (is a | Calas LS i ig | [ess Q* (ie ae VIS Qs (Nie as NISS Ui (ARM (is wt /S Oy (ys ne PECTS ().2 ac’ fy atsy o° Ors iy CaleZs 1 ie ae | TAWA) Tosa 6° Lee $lv$ Oy (We ‘t ?1/4 ie 0:2 [*¢ 11/5 2 os a > of OS oe et os be oe oe 8 oo 68 ow aD 28 6S St oe oe te OE OS ot oe OS £e ot am oe oe UY oe On om oe me SS on OY ow te ee OD oh om ow ae ee A omy Oe ee oe a Ge OD me OY om ud om te ee SO OS GY Oe a be Be ey ty he os ee ey oo ee ot ee OR St ee ee ee es ee 0° * ae we n¢ ‘re Bye (Seif 4) Oi Ou (Vs ey A; (\¢ (is iv $ pod fos Ou (| Dag QP IS On () 281 ee | uf ic m, 0 me aon Te. 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CCT: / VALS 6 Wiel Q] HTt7$ : Wilig/aS LISS “l/s § GUs$ VW fae $175 CL/S iF WGA) Pa Oe I NESS § (Ri iA 2 il WETS ’ l ‘4 | ty f ] 7 oli 2 G Gt? if oO 8 od SE RD le st ee es OD OS DO et OP ee 88 a Oe Gs om Ge Be ow SS me ot os G oy ot oF at ot OD eS SH oe me aH div 20 Siqill 10S DUP EH UNG eae (Mei) niin ae oe eC eS eR MUG Y GAMA AMAL YUN ade Uy] SEVAGOMITYMGMOTI VULNS Maret Pat) iva “ay. adavi NOMwWuUOduOD RAW hen ae oA 4 7S 7S 7S 75 7% /$ Ts ESti=€ —» ie Sp BOOT 0546 Sy) ven IS /F ae tS: ee oe VOSG /°R Sage eo" §) Gon WIS Ona (at Gents ean? 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CAG O° OHS Oe iS: Bie Ss Paty) pees 9°25 b* Sts O° 905 Gis eaee (9 T°S9S$ pe 2g 2° bbe2 I" G5? 2 PS: 6° T6I gry G*an] heyy ez: (l4-“002) (L4=-001) (LaeQ¢ J (| dey ) Jiu NOTID IU bQ sre CSJHINLTENOLSIME TAD D Aad LSM VSTT VID ee TYG pid LGA ITONW TD Wy baM dy Qo g cd SHIMON FHL OL LDFISYM WIT SQyMo deni Plog AVEM 2b EP aeN Quy 4d SAQM ye date gid at PHMOK Had SAA Head addS OMEN 4M ALAN ALIN adel SUVHOON DI 4=SrHa lL LV dea wus Lp) TS frail t Ads Hdd SAJOVUIAV ATIT¥YA SAT 21 NOMYWUOdANOD e ¢ RCH aa 4 cSti=a. it wl - ss G° at Fag Salty cea Ay eee ay 9 0* 09 y* ho Sey Ge pera 4G 7S ey GH Q°u/ Lys £6] a ID) ee ey} we IG G*°tL oh: Cage) EGAS bbe [° 6 ie as Q2/S Hot! PS Ss tate A Peo T° e’S pec aity HPfs O° Gt Gu fesode S$e/S Pains O° 1% Oo iss Cade 6°80 ete), Gey ayes Gacy g° A] Lies Deh UN Le /°y9 eats) iv (ZS 2° 0 yp uye 1 eg WEISS 7° 19 & * Fy MQ GeAG I) LE WAS S° ot tr set, n° YD Oh (ZAG: §*59 1°49 Gra G14 Gory 6° AW fe gt Visy 2° bh Les aly eA 6°99 OZ Gel. G 8g CANS eo’ eR * $24) iy 54 Liltay C26 1° RG ph MAS G°Gh ef wh oa b 7S b°* St) G2 ab Ky ty 590 1G Gos Levis CG Laas 1° R39 HO GQd wed Ora /3e R° HQ OP OL Qe hy G 45 9°16 2216 ae Leys) be Sb 1°94 Q* 2h § 75. 0° 94h Lit L°YA Cae: h* ng g* yy Q°Gy lo AS (14-002) Ci deeot) (lL4eng y (Lae) Alyse 6 Pt. Bre Pal OEE OE EN Ae (SAPINTRENOTIWIL TAT I 24 PSY OLTITESAYNSS Tad POA GT TD WW Lb erat arty a SHIMON JH! Of 21909dS3M HLIM SFQMO FMD OTP DIC Gis SPP aR YM ys Sa a ae aed eM ded dd CHNOH YId SIV HHI Ids GTA Cab de ITAND aad SUVAGOAITE “SNOLLVatN aide Gd bed) TE MHL 1 MVE MO4 SQOUMGAY AiTva SAL atavd HOMUNOdGNOD INI NCH we al VoLL-d 1a G°?s LABS CES Ges io F5 rk 1°ee le? fom Wie No 75 rest tr T arte eee B24 6°SI Peet aN ee We/S O° HS 6° 4S ASS KEG TAS ; tHe aa 2°05 i ny casey a y GS pee) 9° SS G25 h° ep G°on G° oh o° 5h bess G2Sit eet) $9) 2G ty Si CZLS R° GS O° Us eS Ww Gs CePsy PG g* a? 2° ae eu 12/5 Giese A Ge Pe core L/S co hid Ceo? by tie ai? HIS 9°6T CSAC Stee We Sa YTS 6°S2 yet? bated Ad LOWS 6° 4S O° 1S 1°74 ay 5 QL | 4 ee rs tie Canc, GT/S 6°) Qe)? ere Neo? Ps G°ss H°us G*as he ug vs Lee [ tre’. n°¢g? Nah CVSS (peg | OAT f° eI eure LEAS Lei hq? WO? ee ONS, 9° HF Reet) 5° 0h O° Ob & /S (Sg (ain% bean LOGS &°NG n SY ets &° Os Fae Ss 2° GS a a 2*te WG? aM ye q°G? G 7S g°Cl a ta | q*Gt fo G /§ G*ht ga in| g° Ol Si te aS g*Q] 5 °ol 7° at g* ie G 75 EO LOT 2°61 Ge ef § LE? Y*62 Le tS ES: 1 ss (14-902) (Laeogt) C(t4e0$ ) (Jde2 ) 4At{vc $21 BEES ype Made al CSUHIRIMNOTLIVITALTI Fd FSV T Vie =| dnss dae GA QIN CIV IOP aad) dtodd PHIHON FHL OL LIAASIM HIEIM SAAMOAMeAN AEE DIME Gt SP TAM peed Gg dee TOE op dd a | PHNOM M4Ad SAVIN GeTM faah de ATA Fd SHH Qos ee Sea; tye tr due geG eT) TG Ny 7 W¥t AOA SIOVNAAY Atlva SAT A yew] MOMWUOdNOD é NV ACAYY a 4 RADIAN CORPORATION TABLE V MAXIMUM FIVE-MINUTE AVERAGES AND TIME OF OCCURRENCE FOR MARCH 1 THRU 31 _ TT *B=1155 SSET =a it figs C Aor | ae : Coy Tes tr 9 Ge) site CNGer STs Vite al best Cowes bt Sed Post (EC ee eal ELS Gitta ised nen Goleest ie 3s GGY (HiGte Jiens ress Cet sje 2€/9 Cette 2) oe Gane GAO LE > an’ Coe) a Gh? (Cones. Se ce: (ante Wants sit fs (Hee Vinee a Ne IVs st S10) ues S Wat COW Sy ae MLAS (ete, ee al ay Costreyyts Bee (Gia SANE Ey Giiicie? Diy oat ie | (O27 sa2IAT I WA) GOKU ea eae GOV cathe ace ee? (hers: Sy Lf CSS: Tice tl eg (GG NG ines Ute: (MS enth: er. a’ CSG este We ists pa) (Sie s: tre wean al re? 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AIT WEeVIS 4 Quy ChE mM ATMA OL ZEAT 79> Jones csv MOLLYN Je al ad WITIOVWMO FG) Ju LOILOMa Ati’ uw rn 9) n pe ee) = at NU e L c FE y ALT VUSVIS WHS se) \) \) % as | oma | im) SS Men PY Nn 4y G Q rSS vss 2 { S " 5 ? MNOMYWUOdANOD NTH at gy ) van | wn SSS 1 | | HGS? HAG iG 7 5 S iss 4s a5 8 6 4} fy / S MOS 8 % a 5 OG eS “G ey AG q ST Jeet 0 Yea Gas CSTR aCe SOPCVANTO ONY CMpwe Ane CLALIT NSS LS eh eS OVE A eI C2 AAA OF a, mer si NOTLVSTUNFL I SSvId AL patewps TART SS SAPOOe AY ese a aid VIO AWS Fey MOMYWuUOdANOD IT B-1302 WSs TWAS RADIAN CORPCRATION APPENDIX A STABILITY WIND ROSE DIAGRAMS Il B-1303 RADIAN CORPORATION APPENDIX A STABILITY WIND ROSE DIAGRAMS According to the data presented in AEC Safety Guide No. 23, the relationships between stability classes and dq are as follows (the values shown are averages for each stability classification...9, is the standard deviation of horizontal wind direction fluctuations)... Average Values Stability Pasquill Gx Classz fication Categories (degYees) Extremely Unstable A 25.0% Moderately Unstable B 20.00 Slightly Unstable g £5.00 Neutral D 10.0, Slightly Stable E Ce Moderately Stable F Pots Stability. winde roses sobtained at the trailers in the monitoring network are displayed in the following tables. Because of the relatively low heights above the surface (9 meters) at which the wind data is taken, the stability distributions are skewed toward the unstable end of the spectrum. That is, the unstable classes (A, B, and C) have a much higher frequency of occurrence than would be obtained with the Pasquill method of stability categorization (or with instruments at higher levels). Tab be 71 Ndepictsisthe efrequency distribution .of Pasquill stability categories based on oe from data collected by M. M. Pendergast and T. V. Crawford at the Savannah River Plant ("Actual Standard Deviations of Vertical and Horizontal Wind Direction Compared to Estimates from Other Measurements", Symposium on Atmospheric Diffusion and Air Pollution, September 9S Ufa innec distinct range patterns of stability class II B-1304 RADIAN CORPORATION distributions were observed: low, mid, and high, according to the height at which the ore measurements were taken. TABLE 1 FREQUENCY DISTRIBUTION OF PASQUILL STABILITY CATEGORIES stability C2 recen(es esce2 cave. ; B C 0 E 3 G are Cc, S22 te ia - — - — ry} = os fee : < - me = 5 ~~ - < S =] ~ > Ps 5 S > ran « o 2 = =t ~ _ a « > Y 269— < a 3 °o a .e) ty iy a . o ry é re] 4 fe) 15 Pe as z5 STANOAROD CEVIATION CF LATE2ZSL WING Dtazctice op ( Del rd meats a | met ae es | “7 aA a pa a | =o : Lid al da cbt {£ 2 LS We G9 96 énq b?S L61 Patm | 9g ft gg Ah TI {7 6 | / 2 eH AM aes (OWLS: : OT 12 Ce ie, 72 tie pi 1¢ Le We et GI rad a] ra G H 5 {1 “1S 6GSh 3 G 02 lg We bt At 1a AY an LY) 5? Ve is) i 1 ? : ! ~ 4 “te 9G so) GI QT et 0? GS L9 {¢ Y 4 VG Gl } 5. l 9 ° e | adie "22 GOES s of l Pd ty q Lh Qt ga SS. \t 4 5 2 : bY = 2 eas C8 : am | ? : te -~ Wi m0) : : he 1%) hegiel Gl QT Sl Gl 91 1} NV? 1? WI Q | pl tr} R / a 9 GdadS xX Ane %-° WiOL MNN MN aAjM OM MGM OMG “SS OS SS 4S 4c4 J Jud 4h ANH OW INE LINT ape Po cee CC LO a NES CLIT VS ZTE. -C ALIN FES Ca ial WAIT thodeo0e LOA WEA VMs wed WYAOYT JISoOM asta LYE eaves MOILYWuUOdHOD ET ey ACT Oy EP b= 1512 (% 65°@ 29 ~ JAOQGY CALNHTHISTO SwIVd an aaeene WEG NPR er re eernein ipr aleve yeue¥ erie tie Siecaie: ole © @ 0 ayn (ue bo g8' oye, pastors oreHee 6-6 06) (0.60. 0/8101'6 @4a8,/0:9N8 78 (0.99810 8S Sots ee "oot eee | = ot ve °2 yA Sia Fe he ae ON eh de 9 ee) * 1 oi) at) n s ae Ke i fe 2cl oh 0} 9 ¢ I pt Zeb Gat “Tit. Git -2e G2 g 1 5 5 ¢ q : Wil S6e. ihe = 70 9 b 6 l % 4 Gt gt G2 Ge Wt of 5 + \ g 5 5 11 *6E ble 3 hh 5. 2 " 9 q¢ iS wa 2g ug im 3 { ; l = § =e 605 = t I te We RS. On t1 ° an ll celal ean : if 7 G qt 1 : om - Pl *9 2 8 ed - Wi 149 g $ tr? ee) bb edi 9 Ll S i] b Lt Gf Gt yt $1 h 0 { i t 7 AVIS wel Geyer % WIiOL \MNN MN Mpipe A MGA OS MSS OS wS OAS 4ysa4 309 YN VIM of MOLLDINTA ANT fs CCU Tey vals CLETASEL® Cl LEAN, FE, NOON Ae TIAA Lah =o te L9afnd WO VWHS HeD UVMOVED ISO ae ges APE VD AWES (. ae ° RAWAM TA \@ CORO RHOHRHE KEHOE ROH EOREEOHHRHEHOH KL OKHYD 001 x GRO hott 8012 2eul neg] OLV} R69 Wiodl M <= ce ce ec ce cc ye) Bi 5 f MATA) ¥ 9 m re ~© rs 6 om | mH mM IS! 9 a ALOE VEY US a ow it aga % Wied - AlidVihwys 2 40 ANH 4d np aANeS, - ALIVISVIS 4 Bow pee pay 7 hemes arb wo A Ny ES J 4M 4A9NvVIN ANI, % 99° Ud. = KLTV sys S$ 4 Vey d ey Ape deg ZA O° Sl. = LL Vays VY AN FOV Nae CK “bl 2S LLC @ FJAQAV GALANT MES Te Sew do aque cIWwood @seeeeveeosese se eGo eoedevuseeseBevnsveevevaoeeoseveivusevovevoevnedevouveteunseseoeuseses maa (0) oC ofits area | Ai sal (af 2G ®t AG: v2 ban a | ore Ne 8 Jr 4dooudd lh9 Se9 flo 6h 2F0OT bb9f C26) 6Gth pHs nee HOY iv iy Gey $40 : Vit HOt ct G6 9 bY wy? /6 OW LL gS tS ¢§ wh 4S. 79 : $ Lt nee-= SSe “FE Gb 4G t el2 Wy J te Gel Gt oY og b2 TS oma) : 1 = 5 96 | be I ett ia) WE it WO2 GLI 9/1 pn th \ WY 62 ey Wh : lan | = { 9 66 got Livy $52 ROW 2H nl 1S G? é & Vy ye i : Wf « <¢t G2 iat Qf ha n92 O9F ctl Wy I it EAN M i? ~ Wl W 6 h ni An | 762 dpi 2 ny 3 i es bhlA cf S% id Ge H¢ ( LS ge | St ht vf $1 Ge We AVdas ye deus MA} MAM M MOM MS MOS S ISS 4S 4g 3 4 Any an Jib y ‘OTJIDAM LO hy WoL = SS¥YTVW ALTVEOUVES CEEAVG ZS OD LECI SE JVOOT ea AAV) [PMUd4eNO? LIAO VIN AWS Hey VYMOVUTU Sa Guyer ALI VWINVIS NOLLWHOdHOD OT RCA an RADIAN CORPORATION PERCENTAGE OF OCCURRENCE OF WIND O[RECTION FOR 200 F607 LEVEL Pt B-isi4 THIS PAGE LEFT BLANK INTENTIONALLY Il B-13i4a cA : Q >> a (See ey 149 | ” GDRPORATION DCN 77-100-152-03 AIR MONITORING REPORT FOR C=b, SHALE. OLL PROJECT APREEALI77 REPORT NO ~ 32 (% 1 July 1977 Presented to: C-b Shate Ori .Project United Bank Tower Denver, Colorado 0202 Prepared by: Radian Staff PLB aS 8500 Shoal Creek Bivd./P.O. Box 9948/Austin, Texas 78766 /(512)454-4797 LEP RADIAN CORPORATION fea iL . ae TABLE .OF CONTENES GENERAL DESCRIPTION OF AIR MONITORING PROGRAM DESCRIPTION OF INSTRUMENT SYSTEMS ------------ A. Air Quality Instrumentation--------------------- Calibration Procedures -------------------------- G. Data Acquisition (Sys Gets en Meteorological Instrumentation------------------ MICROMETEOROLOGICAL AND TERRAIN FEATURES ------------ OPERATING TIME ANALYSIS FOR EACH SITE------~--------- MONTHLY METEOROLOGICAL SUMMARY ---------------------- A. Summary of the Meteorological Conditions North America during April 1977----------------- B. Summary of the Meteorological Conditions Northwestern and West Central Colorado du Keri 1977 -sSes 23-25 See oe eee C. Summary of the Meteorological Conditions the Oil Shale Tract C-b Region during pet PE OT Tanne a ee ee DATA PRESENTATION AND SUMMARY===-— 92-22 —- = 5e-oe=e ee TE B=1Si6 eo ee eee ae we Over sgl ring aba Page , & Mn, RADIAN CORPORATION TABLE I TABLE Uf TABLE LEE LIST OF TABLES DOWNTIME HOURS FOR C-b SHALE OIL PROJECT AVERAGES FOR APRIL 1 THRU 30 NieEorenyOnedes (NO) loassencsescaasse>>>>>>>= Nat bile £O cin OM CONO) oo ee ee ea Se sce Mie rocenpitoxude £(NO> Voc-s==4-7ssssaacssssest Sul sus paoxmde{(s07 ) once Pat ssscssaseaSsc sere EvasanOmet Giese Soe mS se lIaas asa seca dea c tse Hy GrOcen Poult udes a= SoS eae tats este hovallaltyCrOCanDONSc > 2>——s2—ssacaes asses ces tess Non-Methane----~----------------- rrr rr rrr Carbon Monoxide- ------------------------------ Barometric Pressure--------------- err TOtrat we recip Leacten——— oe = =e Se Particulate-------------~---------- 5-3 Wind Speed==—-—-+=—---<-=—<=4 -—sseer ihe o aaa = Wind Direction-------------------------------- Relative Humidity----------------------------- Temperature----------------------------------- Be Bi S07 Page rN RADIAN CORPORATION LES? 3OF TABLES, €comed) Page TABLE LV DAILY AVERAGES FOR APREL 1 THRU 30 TABLE V Nitrogen Oxides: (NO ee ee II B-1363 Nitric Oxide (NOQ)-----------~------------------ -1363 Nitrogen Dioxide (NQ,)------------------------ -1363 Sulfur Dioxide (S0O,)-------------------------- -1364 Pyranometer----------------------------------- ~1364 Hydrogen Sulfide------------------------------ -1364 Total Hydrocarbons---------------------------- =b3G5 Methane----------~------------+---~------------- =1505 Non-Methane Hydrocarbons---------------------- -1365 Carbon Monoxide~----~+-------------------------- -1366 Ozone-- ----+-------------------- ---- -- -- - ------ =1366 Barometric Pressure--------------------------- -1366 Total Precipitation--------------------------- =1367 Particulate------~---~-----------~--------------- =1367 Wind Speed------------------------------------ -1368 Wind Direction--~------------------------------- -1369 Relative Humidity----------------------------- =1370 Temperature----------------------------------- =LS71 MAXIMUM FIVE-MINUTE AVERAGES AND TIME OF OCCURRENCE FOR APRIL 1 THRU 30 Nitrogen Oxides (NO. ) we eee ee ee ee ee “ES/5 Nitric Oxide (NO)----------------------------- -1374 Nitrogen Dioxide (NO,)------------------------ = 1375 Sulfur Dioxide (S0O,)-------------------------- -1376 Pyranometer---------------------- 2-52 -1377 Hydrogen Sulfide------------------------------ 51ST Total Hydrocarbons---------------------------- =1379 Methane---------------------+------------------ -1380 Non-Methane Hydrocarbons---------------------- =1581 Carbon Monoxide-----~-------------------------- sl BS 02 {i B-13518 om (i, = RADIAN CORPORATION ListeOn ABLES. (Contd) Page TABLE V MAXIMUM FIVE-MINUTE AVERAGES AND TIME OF TABLE TABLE Vi Veet OCCURRENCE FOR APRIL 1 THRU 30 Barometric, Pressure------<<---<-<--<----------- II B-1384 Total Precipitation---~------------------------- -1385 Wind Speed-Wind Direction-~-------------------- -1386 Relative Humidity----------------------------- 1507 Temperature-- ---------- == <9 ee -1388 THE FIVE MAXIMUM INDEPENDENT SLIDING: AVERAGES POR APRIL. a THRU 30 Nitrogen Oxides------------------------------- -1390 Nitric Oxide---------------------------------- -1390 Nitrogen Dioxide------------------------------ 1390 Sulfur Dioxide-------------------------------- =L5o) Sulfur Dioxide - 24-hour---------------------- sal Soul Hydrogen Sulfide------------------------------ -1392 Total Hydrocarbons ---------------------------- = 1592 Methane-- ------------------------ - ee -- =1593 Non-Methane Hydrocarbons---------------------- =11394 Carbon Monoxide - l-hour---------------------- -1395 Carbon Monoxide - 8-hour---------------------- -1396 Ozone-- --------------------------------------- = 1397 Particulate---~------------------------------=-- -1398 FUNCTIONAL DEPENDENCE OF RECORDED PARAMETERS UPON WIND DIRECTION NvGine sen Oxides WNW) =n -- > 26a aaa a SSeS -1400 Nitric Oxide (NO) --------------------- ‘-------- -1401 Nitrogen Dioxide (NO.,)------------------------ -1402 Sulfur Dioxide (SO,)-------------------------- -1403 Hydrogen Sulfide (H2S)------------------------ -1404 Total Hydrocarbons ---------------------------- -1405 LE IBALSI9 ie, RADIAN CORPORATION EES’ OF TABLES -Geontd) Page TABLE, VIL FUNCTIONAL DEPENDENCE OF RECORDED PARAMETERS TABLE VIII UPON WIND DIRECTION Methame=- ~~ 2 = - 3 2 Il B-1406 Non-Methane Hydrocarbons ---------------------- -1407 Carbon Monoxide------------------------------- -1408 Ozone-- ~-------------------------------------- -1409 DIURNAL VARIATION OF VARIOUS RECORDED PARAMETERS Nitrogen Oxides-------------------~------------ -1411 Nitric Oxide-----------------------+---------- -1412 Nitrogen Dioxide-------------~----------------- =14L5 Sulfur Dioxide------------------------- ------- ~1414 Hydrogen Sulfide---------------~--------------- =A Total Hydrocarbons--~--~------------------------ -1416 Methane-----------~-------------~---~------------ =1417 Non-Methane Hydrocarbons---------------------- -1418 Carbon Monoxide--------------+-------=---------- -1419 Ozone- - --- -- -- -- - 2 2 ee rr ere re -1420 Hourly Total Precipitation-------------------- = "=1421 Wind Speed 8 feet------~----------=----------+----+---- -1422 30 feet--------------~----------- iaieieieieietaieten -1423 100 feet----------------------------------- -1424 200 feet------~--------~+---~--------+--------- -1425 Wind Direction 8 feet----------------------------------- -1426 30 feet-------~---------------------------- -1427 100 feet-----------------------------~------ 1428 200 feet------------~----~---------~--------- -1429 ‘bP (BIL520 fy RADIAN CORPORATION EESE OF TABLES Ccontd) | Page TABLE VEEL DIURNAL VARIATION OF VARIOUS RECORDED PARAMETERS Wind Direction Standard Deviation 8 feet-------------------------------- II B-1430 30 feet-------------------------- =14 31 100 feet-------------------------------- -1432 300 feet-------------------------------- -1433 Horizontal Wind Direction Standard Deviation 200 feet-------------------------------- -1434 Relative Humidity 8 feet-------------------------------- -11455 30 feet-------------------------------- -1436 100 feet-------------------------------- -1437 200 feet-------------------------------- -1438 Temperature 8 feet-------------------------------- -1439 30 feet----------------------- +--+ -1440 100 feet-------------------------------- -1441 200 feet-------------------------------- -1442 Houwly. Total Solar Radiacion=—-==---===-+-- -1443 Temperature Change’ from S0}4to.100"-------- -1444 Temperature” Change fremi304 "to 200 °-------- -1445 Barometric” Pressure==—==Ss -==—----=-=-=--=-- -1446 Bi-Vane Wind Speed 200 feet--==----=+--=-=--------------------- -1447 Horizontal Bi-Vane Wind Direction 200 feet-------------------------------- -1448 Vertical Bi-Vane Wind Direction 200 feet----------~---------------------- -1449 Neeacocen Oxides=——— == — er = S- —= = -— = -1450 Nitric Oxide------------------------------- STAG BEB 1521 RADIAN CORPORATION LEST.OF TABLES €contd) Page TABLE. VITT DIURNAL VARIATION OF VARIOUS RECORDED PARAMETERS Nitrogen Dioxide-----------~---------------- II B-1452 Sulfur Dioxide----------~------------------- -1453 Hydrogen Sulfide--------------------------- pe 144 Total Hydrocarbons ------------------------- _ 71455 Methane - --------------------==+------------- -1456 Non-Methane Hydrocarbons --~----------------- = 21457 Carbon Monoxide----------------+------------ -1458 OZ0MG='=5=5 Se 52-2225 5-5-- ae oes Se -1459 Hourly Total Precipitation----------------- -1460 Wind Speed 8 feet-------+-~----------+---------------- -1461 30 feet--------------------+------------ -1462 100 feet--------------------------~------ -1463 200 feet-------~------------------------- -1464 Wind Direction 8 feet-------------------------------- -1465 30 feet-------------------------------- -1466 100 feet-------~------------------------- -1467 200 feet--------~----~----------+-------- -1468 Relative Humidity 8 fetuses es6 6 26 ae Se ee ea ee ea -1469 30 feet------------------------ +H ---- -1470 100 feet------~--------------+------------ ~1471 200 feet-------------------------------- =147/ Temperature 8 feet-------------------------------- ~1473 30 feet-------------------------------- -1474 100 feet-------------------------------- -1475 200 feet-------------------------------- -1476 Barometric Pressure--------~--------------- =1477 DT B=ES22 RADIAN CORPORATION LEST OF “TABLES “Ceonted) Page TABLE, VLEL DIURNAL VARIATION OF VARIOUS RECORDED PARAMETERS Solar Radiation---------------------------- ff- B-1478 Bi-Vane Wind Speed 200 feet-------------------------------- -1479 Horizontal Bi-Vane Wind Direction 200 feet-------------------------------- -1480 Stability Class Determination Using Pyranometer Recording-------<--------------- -1481 Stability Class Determination Using DT/DZ (Level 1)---------------------------- -1482 Stability Class Determination Using DT/DZ (Level 2)---------------------------- -1495 APPENDIX A - STABILITY WIND ROSE DIAGRAMS ---------------- -1508 8-foot level - Stability Class A--------- =50Z Class B--------- =15i13 Class C--------- =1514 Class D--------- 1515 Class E--------- =1516 Class Total----- =iSi7 30-foot level - Stability Class A--------- =i518 Class B--------- -1519 Class C~--------- =1520 Class D--------- Brgy Weal | Class E--------- S22 Class Total----- =i 25 100-foot level - Stability Class A--------- =1524 Class B--------- -US25 Class C--------- =1'526 Class D--------- 27 Class E--------- -1528 Class Total----- =1529 Ti B= 1525 LID, RADIAN CORPORATION Best OF FABLES Ceomtd) Page APPENDIX A - STABILITY WIND ROSE DIAGRAMS 200-foot level ~- Stability Class A--------- IT B-1530 Class B--------- =1551 Class C--------- A552 Class D--------- =1555 Class E--------- -1534 Class Total----- =1555 Percentage of Occurrence of Wind Direction FOr 8-foot level----------------------------- -1536 30-foot level--~--------~-~------------------ -1537 100-foot level----------------------------- -1538 200-foot level------------~----~---------+---- = 1539 It B-1324 RADIAN CORPORATION Te GENERAL DESCRIPTION OF AIR MONITORING PROGRAM RadiamiComperation, uider contrace to the C-b Oil Shale Project, is performing the data compilation and reporting of air quality and meteorological data at one monitoring site in Northwest Colorado. The site measures and records concen- trations, Of particulates, sultur dioxide, joxides of nitrogen, hydrogen sulfide, total hydrocarbons, methane, and carbon monoxide. A 200-foot meteorological tower provides wind direction, wind speed, temperature, and relative humidity data at four levels (8, 30, 100, and 200 feet). Other meteorological variables measured at the tower site are insolation, barometric pressure, and precipitation. Figure I shows the configuration of the monitoring station. The station provides a sturdy and protective covering for the monitoring equipment. he B=1525 NOILVLS ONTYOLINOW AO NOILVANOLANOO 1 ddnola SOVVIES AUAILEV ——— ee eae Ce ee AIVAS WON } wosssudko3 ‘ 7 | Vauv INSANULSHNT | a/v : i viineKoo| tove Soa v | 1 i \ ee “ j ie eee lp oes SJ = o—s f aovas won fy “ya I -p'9 Ca ee ae ee cc ee APROL (es ‘i 37H ——— WIV OU3Z II B-1326 RADIAN CORPORATION Ede DESCRIPTION OF INSTRUMENT SYSTEMS A. Air Quality Instrumentation Nitrogen oxides are measured with a Meloy Model NA520 analyzer. This dual-channel analyzer is based on the chemilu- minescent principle and continuously monitors both NO, and NO. A subtraction circuit in the instrument provides a continuous NO, output, but is not used in Radian's system. NO, is cal- culated once a second by the computer by subtracting the NO value from the NO, value, thus avoiding any drift which. might occur in the NO, output of the instrument. This instrument has a minimum detectable sensitivity of 5 ppb (parts per billion) andway Linearity, oc. 2 1/.. Both sulfur dioxide and hydrogen sulfide are measured with Meloy Model SA185 sulfur analyzers. The hydrogen sulfide analyzer uses a Meloy Model NO,-1 sulfur dioxide scrubber and the sulfur dioxide analyzer uses a Meloy Model H.2S-l hydrogen sulfide scrubber. The Model SA185 is a continuous analyzer and utilizes the flame photometric principle of operation. The minimum detectable sensitivity is 5 ppb and the linearity is +1%. Ozone is measured with a Meloy Model OA350 analyzer. This instrument, based on the chemiluminescent principle, pro- vides continuous measurement of ozone. The minimum detectable Sensltivityiis, 0 .S ppbyand, the linearity is +17. Total hydrocarbons, methane, and carbon monoxide are monitored with a Bendix Model 8200 gas chromatograph analyzer. This instrument, which uses a plume ionization detector, has a minimum detectable sensitivity of 5 ppb for all three components. The Model 8200 works on a five-minute cycle, i.e., one air sample is analyzed every five minutes, and the results are dis- played for five minutes via a sample and hold circuit. iT B-1327 RADIAN CORPORATION The air sample is drawn in through a glass cane and manifold supplied by the Ace Glass Company. The system has a 25mm diameter, through which a constant air flow is provided by an air pump rated at 60 cfm at 0" head pressure. The manifold has sampling ports to which 1/4" teflon lines to the instrument are connected. All joints in the sampling system are secured by O-ring compression fittings. The manifold is contained in a heated (100°F) chamber to prevent condensation of moisture. The teflon lines from the manifold to the instruments are insulated with 1/8'' wall thickness rubber tubing. The trailer has four heavy duty high volume particu- late samplers (Hi-Vols). Fiberglass filter paper is used for the collection of particulate samples, after which each filter is brought to a controlled humidity before weighing. Each Hi- Vol has a flow recorded to permit correction for changes in air flow as the filter becomes loaded with particulates. Each Hi- e Vol runs for a 24-hour period (midnight to midnight) and is turned on and off by the computer. The Hi-Vols, which were manufactured by Radian, were designed following guidelines re- commended by the Environmental Protection Agency. In addition to the normal Hi-Vol particulate samples, a duplicate Hi-Vol sample is collected every sixth day on special filter paper for trace element analysis. Once each quarter these samples are composited and analyzed for gross radioactivity and trace element content. B. Calibration Procedures The trailer contains a Meloy Model RAD-1 calibration unit. This instrument provides a zero air supply, SO, span gas rom an SO, permeation tube, and NO span gas obtained by precisely II B-1328 RADIAN CORPORATION diluting bottled NO span gas. The computer-controlled calibration of all instruments is automatically performed once a day ma bachminstrumentems (firs switched)to:zero;. the. computer monitors the output of each channel and takes a new zero reading after a stable zero signal has been reached. This zero reading is compared by the computer to the zero reading obtained 24 hours before: 6 ands ifjavderftoinmexcessiofsi0 ppb, hasnoccurred;» an excess zero drift light for the channel in question is turned on on the System Status Panel. Next, span gas is supplied to each channel and the computer decides when a stable span value has been reached. This value is recorded and compared to the previous day's valueisy Am excess) span idmitt! Light on the, System Status, Panel is turned on if a drift exceeding 10 ppb occurs. The instruments are then returned to the monitor mode and after two minutes the com- puter resumes data taking. The bottled NO gas used at each site was obtained from Precision Gas Products. Pre-purified grade hydrogen is used in the SO, analyzers. The SO, permeation tubes were manufactured by Metronics Association, Inc. Their output has been verified by comparison to the output of National Bureau of Standards tube 10-42. Both SA185 analyzers in each trailer are calibrated with the SO, from the permeation tube. This instrument responds to the number of sulfur atoms per molecule; thus, SO, can be used to calibrate both: the. H, Sand SO>- monitors. The Model OA350 ozone analyzer has its own calibration system which provides a zero check and a span check. The ozone calibration system is verified by comparison to a calibrated ozone generator maintained in Radian's laboratory in Rifle. iE B-1329 RADIAN CORPORATION The Model 8200 total hydrocarbon, methane, and carbon monoxide analyzer is calibrated with undiluted span gas obtained from AirCo's Rare and Specialty Gas Division. This span gas con- tains methane and carbon monoxide in air, the methane being used to calibrate both the total hydrocarbon channel and the methane channel. The Model 8200 is zeroes with air from a Bendix Model 8834 zero air unit. In addition, the instrument is electronically re-zeroed at the start of every five-minute cycle. The Hi-Vol particulate samplers were calibrated using a Calibration Kit from General Metal Works. Ge Data Acquisition System The basis of the data acquisition system is a Data General NOVA 1200 minicomputer. The NOVA, which has a basic cycle time of 1.2 psec, is equipped with automatic program load € and power fail/automatic restart features. The computer utilizes 16K 16-bit words of core memory. Analog-to-digital conversion is accomplished via an ADC built by Radian Corporation. «|The input/output unit for the system is Texas Instrument's KSR 733 keyboard/printer. This model teletype provides keyboard entry and hardcopy printed output. The data are also recorded on a cassette magnetic tape unit with three drives. The cassette unit is utilized for program storage and loading as well as for recording. To reduce wear on mechanical parts, the power to the teletype and cassette units is turned on only when the unit(s) is (are) to be used. Several important functions in the instruments as well as in the computer and the trailer are monitored by means of lights on a System Status Panel. These data lights are written onto cassette tape to monitor the complete status of the system every five minutes. The Data Acquisition System also monitors the presence of 100V power from the power lines. In its absence, the computer, which is powered by batteries, switches all trailer EE B-1530 RADIAN CORPORATION systems to battery-provided power. If the line voltage is restored before the batteries are discharged to a specified level, the trailer system is switched back to line power. De Meteorological Instrumentation 200-Foot Meteorological Tower The tower has instrumentation at four levels: 8 feet, 30 feet, 100 feet, and 200 feet. At all four levels, there are: wind speed, wind direction, and temperature and relative humidity sensors in a power-aspirated radiation shield. Temperature difference thermistors (also in power-aspirated radiation shields) and their associated circuitry take lapse rate measure- ments for the 30-foot to 100-foot Layer and the 30-foot to 200-foot layer. In addition, this site has a Precision Spectral Pyranometer, a barometer, and a tipping bucket rain/snow gage. The wind direction and speed apparatus used at each measurement level of the tower is the Model 1074-2 wind sensor by Meteorological Research, Inc. (MRI). This sensor has a 540° potentiometer for wind direction and a light chopper for wind speed. This sensor is rugged, with an all-weather coaxial cup and damped vane assembly. The prototype model has been in operation for years under the most demanding weather conditions, performing continuously with the utmost reliability. The wind sensors on the tower have been specially treated with a black paint which will promote warming of the exposed surfaces of the sensor and thereby reduce ice and snow accumulations on the moving parts of the apparatus. The specifications on the Model 1074-2 are as follows: ELSBz1551 RADIAN CORPORATION Wind Speed Starting Threshold} *0-. 75 mptr. Response Distance: 18 feet (63% recovery). Flow Coefficient 7 -9 fect /Revolutioni. Accuracy: +0.4 mph or 1% (whichever is greatest) Wind Direction Starting Thresholds" 0.75 mph. Delay Distance: 4 feet (50% recovery). Damping ‘Ratio 51025: £o) OG" Accuracy (540° system): +1%. Range: 0° to 540°. The relative humidity and temperature sensors are mounted within a power-aspirated radiation shield at each tower € level. All aspirators and sensors are of the Model 840 Series by MRI. The aspirated shielded housing is designed to provide maximum radiation protection to the sensor. Ambient air is drawn into the shield and across the sensors at approximately 15 feet per second. This intake air is essentially sampled from a hemispherical space which is approximately 3-inch radius from the tube opening. Speed of the incoming air at the perhiphery of this hemisphere is approximately 1 mph. The temperature sensor is comprised of a dual thermistor and resistor network. ‘This circuit provides’ a linear resistance change with an air temperature change. The relative humidity sensor is placed alongside the temperature elements inside the shield where it is exposed to a constant sflowtot*aire= Circulation to both sides of the sensing element produces accurate monitoring with a good response time. The specifications on the sensing ele- é ments are as follows: PI°B=15352 RADIAN CORPORATION Temperature Accuracy: +0.25°C. Range: -50°C to +50°C. Humidity Accuracy: £3207" RH. Range: 0% to 100% Relative Humidity. Measurements of temperature difference are taken for two Layers, the 30-foot to 100-foot and the 30-foot to 200-foot layer. The thermistors and circuitry used for these measurements are separate from the thermistors measuring air temperature. The use of separate thermistors and circuitry to measure AT allows for much greater accuracy and resolution in the measurements, which is necessary for stability assessments. Two AT thermistors are at the 30-foot level, one is at the 100-foot level, and one is at the 200-foot level. All of these AT thermistors are mounted within power-aspirated radiation shields. The specifications on the AT instrumentation are as follows: Accuracy: +0.1°C. Range of AT Circuit (Lower Level-Upper Level): +9F° to -9F°. All instrumentation, except at the ground level, is mounted at the end of 12-foot retractable booms. These booms are 3-inch~ box beams which “are “on “rollers “and “can be retracted to the instrument platforms for instrument maintenance. The meteorological tower itself is a 200-foot Rohn Model 80 Guyed Tower, designed for 40 pounds per square foot wind load with %" of radial ice per EIA Standard RS-222-B, to Tl. (B=1553 RADIAN CORPORATION support four levels of meteorological equipment. The material @ consists of tower sections with a tapered base, three retractable booms 12-feet long, three outside work platforms, an inside ladder for climbing, two base ground kits and one anchor ground kit. The cable-type Safety Climbing Device consists of a cable and attachment mechanisms with a locking sleeve and safety belt. The tower is lighted and painted according to FAA specifications. The signals from the tower instrumentation are fed from multiple signal cables into transmitters mounted at the base of the tower. After signals have been converted to analog signals, they are fed into a junction box, also at the tower base, where they are assimilated into one coaxial cable. The signals -are, then run underground within 3” PVC conduit _to the A-to-D assembly, where they are processed. The transmitters are shielded and insulated from the elements. The signal cable is run underground in PVC conduit in order to minimize damage from © the weather or from various rodents in the region. The auxiliary equipment at the tower site consists of a heated tipping bucket rain/snow gage, an analog barometer, and a Precision Spectral Pyranometer. The rain/snow gage is the Model P511-E unit by Weather Measure. In the case of this gage, the durability and reliability of a tipping bucket gage are combined with heavy-duty electric heaters to make this an all- purpose precipitation sensor. This gage may be used to measure both snowfall and rainfall. An insulating.cover of poly-vinyl chloride and a thermostatic control insure the proper gage temperature. The, thermostatic .controel-is ,.adjustable.from.0-te 357 Ca.. Snow falling into the inlet funnel is melted. The resulting water (from rain or snow) drains into a precision tipping bucket mechanism which activates a mercury switch each time the bucket Fills and. tips.-~-The. gage is ecenstructed) of durable. corrosion- resistant materials to provide many years of service. The q II B-1334 RADIAN CORPORATION specifications for this gage are as follows: Gri tices (6. inches: Galabration: | 0 01 neh: Recuvacy: O25. (Caliprated at 0.5 in/hr).. Sensor: Chrome-plated tipping buckets. Switch: Mercury, 0.1l-second closure. Heat Control: Thermostat adjustment, 0 to 3oGe The barometer is the B242 Analog Output Barometer by Weather Measure. This barometer provides an output voltage that is linearly proportional to pressure. The specifications on this instrument, which is mounted inside the monitoring trailer at the site, are as follows: Range: Specially designed for the 100 millibar interval from 725 millibars to 825 millibars. Resolution: Infinite. Linearity: 2+0.5 millibar, over the 100 millibar interval. The pyranometer at the site is the Eppley Precision Spectral Pyranometer. This instrument is used for the measure- ment of sun and sky radiation totally or in defined wavelength bands. The pyranometer is levelled and mounted atop a wooden stand 4% feet from the ground surface. Care has been taken to eliminate the effects from all outside influences, such as reflection or shadows, on the pyranometer. The instrument characteristics are as follows: Sensitivity: 5 mv. per cal/cm°/min. Independence: 300 ohms. Temperature dependence: Sensitivity constant to within +l percent over the ambient temperature range from -20 to +40°C. PE B=1555 RADIAN CORPORATION Linearity: Response linear up to intensities of 4 cal/em+/min. Response time: 1 second (i/e signal). All instrumentation is factory-calibrated and is field- calibrated at various intervals. Sling psychrometers are used to calibrate the humidity sensors; known temperatures and/or resis- tances are used to calibrate the thermistors; and an rpm cali- brating unit is used to calibrate the anemometers. The wind direction instrumentation is aligned to true north (reference direction) by means of a surveyor's transit. TT .B-1356 RADIAN CORPORATION EEE. MICROMETEOROLOGICAL AND TERRAIN FEATURES The Piceance Creek Valley and C-b Shale Oil Tract are situated such that many microscale meteorological phenomena affect the region where the ambient air monitoring unit is located. Trailer 023 and its associated 200-foot meteorological tower are located atop a plateau to the south of the valley, high enough to be affected mostly by gradient flow conditions. The elevation at the meteorological tower site (Trailer 023) is 6940 feet above sea level. The largest gradients in eleva- Elon jin. this area, of course, .occur at the Piceance Creeki Valley walls. However, the northern valley walls are slightly steeper than those at the southern boundary of the valley, which then slopes upward gradually toward the C-b Tract. The Piceance Creek Valley decreases in elevation from east to west in this area, so that nighttime katabatic cold-air drainage flows advect from east EO: wes E;. Site 023 is approximately 2.5 miles south of the Piceance Creek Valley. This location is relatively high com- pared to its surroundings, with the nearest point having an eleva- tion greater than 7000 feet being .5 miles to the south of the tower. The tower itself is on the top of a small knoll located between Scandard and Sorghum Gulches. Because of its location and the irregularities of the surrounding terrain, meteorological patterns are varied here. Wind instrumentation is mounted at four levels of the meteorological tower: 8 feet, 30 feet, 100 feet, and 200 feet. The top level of the tower generally remains in gradient wind flow. That is, the winds at that level are normally generated i B-A557, RADIAN CORPORATION by synoptic-scale features and are usually separated from terrain os features and micrometeorological circulations. Occasionally, a weak anabatic flow influence is experienced. However, such is not the case with the three lowest measurement levels. To varying degrees, these levels are influenced by both the katabatic and anabatic circulation cells. However, when strong pressure gradient forces exist in the region and the synoptic~scale wind flow is strong, all four tower levels will reflect a gradient wind flow as the winds increase in strength and height. The terrain atop the plateau is generally barren and fairly rugged, with a few scattered small trees. The topsoil dries rapidly and is very fine, resulting in blowing dust when dry, windy conditions exist. In the Piceance Creek Valley, the terrain is fairly grassy and flat, with steep valley walls on either side. Surface winds are normally rather light in this valley unless channeling effects occur. e During clear nights with rather light pressure gradient- induced winds, rapid radiational cooling will occur in the region because of the barren nature of the terrain and the generally dry character ofthe air in this portion of the country.~ Ase a result, the diurnal range of temperatures will be extremely large. Because of the katabatic flow in the valley, nighttime temperatures will generally be lower in the valley than on the plateau. During the winter, especially, temperatures in the valley may be 20F° lower than they are on the plateau during the early morning hours. [11 B=1339 RADIAN CORPORATION Tes OPERATING TIME ANALYSIS FOR EACH SITE This section presents the operating statistics for each of the major subsystems contained in the monitoring station. Table I shows the specific number of hours that each of these subsystems were inoperative for the month. The colum labeled "DIGITIZING SYSTEM" indicates the entire data acquisition system; therefore, downtime hours appearing in this column means total loss of data. These instances include, in addition to computer downtime, power failures, no power available, and self-~automated shutdown periods such as during air conditioner malfunctions. Calibration time is not considered to be downtime and is, therefore, not included in the downtime figures. The amount of time used in calibrating the instruments is given at the bottom of the downtime analysis table and is reported as total calibration hours for each channel for the entire month. As is evident in the calibration figures, channels can be calibrated independently of one another. No calibration time is given for particulate monitoring since Hi-Vol calibration occurs infre- quently and only during the off-duty cycle for each Hi-Vol while another Hi-Vol is taking data. TL B-1339 S&S st ty of 04 e | 0 Vite ere oe: Vel BS Sete SO eit = +0 °0 °0 *Q val i | OL ha Ge 5) QWwIl W9 *0 °0 Ge" * "10 eA) =0 “0 Bt) 0 °0 ae) °0 “0 “0 *0 *0 0Of/t 0 °0 “Tem "0 “0 *0 (0 0 *0 20 *6 °0 20 0 °0 “0 62/h 20 0 com. "0 °0 ae) *0 i) *0 °0 °0 20 °0 °0 °0 °0 Q2/h “0 ‘0 Aes «0 “0 10 *() =0 = “0 °0 a) °0 =0 “0 rig Lesh a0 =0 “een, 10 °0 °0 “0 “0 0) "0 a4) “0 =O *0) 0 “0 92/h *4 *9 *o2 0 °0 *0 “0 °9 *0 *O *O *y *9 *y a) eT G2/h *O *g ~0 *9 *0) °9 °0 °9 *0 *Q9 °9 *9 "6 *4 “OY *9O n2/h *0 0) *0 a0 oO “0 “0 6d rel oy | | “0 *0 *0 = S2/h °0 °0 Shem "0 *0 ei) “0 °0 “0 *0 *() °C ‘0 °b °6 “0 ' 22/h *9 = 0 *O *y ai "9 0 *9 =O "nn °9 ba () *Q “0 *@ wired {est “0 *0 *0 ig *2 “0 = *0 *0 at) *0 °0 *0 0 “0 mA O2/h °0 =) mat oat “1 “0 “0 mit) *0: °0 0 °0 i) mG “0 °0 6t/h *0 0) ma *0 °0 *0 "0 “6 *0 "0 0 °0 °0 ©. “0 ‘0 QI/h *O =0 ay 0) a *0 *0 =O *0 *0 °0 *0 °0 “0 =q °0 EV H 0 *0 <0 a) =0 *0 *0 “0 °0 a) oa) °0 °0 "0 ‘0 “0 91/h *9 =O =a) ban) °o *0 *@ *O *Q *Oo °¢0 *4 a) *O “6 °9 Si/h =0) *0 1 *0 *0 °0 mi a) *0 *0 0 °0 *0 °0 °0 “0 at/h *9 "0 “0 *0 *0 *0 *0 °9 *6 *9 *6 *9 °0 *0 *0 *y et/h °6 0 A) Salinas ow °0 0 *0 *0 °0 *0 mt) *0 *0 *0 *0 Z21/h aU =0 ee | 0 0 °0 °0 0 "6 *() °0 *0 ‘0 =) *0 tt/h “0 40 Haat. “0 *0 °0 *0 *0 20 =O “0 °0 *0 *0 *0 *0 Ol/h 20 °0 mies 40 “0 “6 =0 “0 ‘0 ~0 ‘0 “a nt) °0 “0 if) b&b /h *o 7) *t2 *9 *o ey) *0 26 *H °0 *o ‘oO =<(} *°O “0 10 q in °0 *0 “tex =O *0 “0 *0 ‘0 * 0 °0 *0 *0 °0 °0 oO *0 L/h *o *9 ont “2 oe "0 *0 *9 "9 “9 26 *0 *o *o *6 *0 9 /t *6 °0 “Oy=) “sf ee *6 “0 *0 °0 ma) *o *0 °0 °0 *0 i. GS /h *0 =O aie. L ve) *0 °0 °0 =0 *0 *0 °0 70 °0 *0 =46 n /h *0 "0 “he a | o *9 *0o *0 *0 #6 *9 *9 *0 *0 *o *0 € / 0 . 0 » 0 ° fy a 0 6 0 e 0) @ 0 6 “0 (l/h 0 ° 0 ‘ 0 e 0 ° 0 e 0 ° 0 e 0 e 0 0 210 0 6 0 ‘ 0 8 0 ° 0 8 0 6 0 e 0 8 0 l/h tia 0 e 0 r) 0 ° 0 8 0 ® 0 e 0 ° 0 6 dwWl 0 e 0 ° 0 ° 0 e 0 @ 0 ° 0 8 * 1 /h fhHy 0 é 0 e 0 6 0 ° 0 ry 0 @ 0 Q aM 0 a 0 e 0 ‘ 0 e 0 @ Uy) ‘ *0 /o HSM ¢ 0 e 0 ° 0 e 0 e 0 r) 0 l dwWl 0 @ 0 8 0 e 0 ® 0 e *0 /h SHY 0 e 0 e 0 a 0 e 0 9 ¢am 5 0 e 0 e 0 e 0 ® °G / "SM 2 0 e 0 e 0 e 0 ‘ G - Wi Z2HY *y A *9 ‘ Th) 0 /h 20M 2 0 9 0 9 *9 n /h Sm tT e @ g TOM 1 “0 2 /h Jlvo Se0 Sins y 193ro Yd 10 J1VHS 4 I 31 €=-9 Y04d MOU ITO ce | rei & fred GOs baie ei vs *0 *9 0 °0 o4 dl ~N 0 ® *h2 ® °9 P) es ry 0 ® he ® 0 ° oH 0 e 2 ® fhe ° 0 ® 1 e 0 ® id ° fe ry 0 e a4 0 é id ° hed ® 0 0 0] ry a 0 e he 9 he a 0 ° 0 ° ate 0 é 2?¢ e te @ 0 a 0 6 0 a eS, ® 0 ‘ ee. he ° 0 ‘ 0 ° 0 ° 0 @ pied e e2 F) 0 8 0 ° 0 6 0 . ® 0 . 2 e ee 6 0 e () e 0 e 0 F +] e &2 ® tre e 0 ° 0 © 0 e he *b 0 s ‘ 0 s Go # Hid. ea 0 ° 0 a 0 ° ra 0 ; 0 ry ne ° G2 ® 0 * 0 e 0 © te e 2 oy 0 IW vad Masia mene the ue eee ee ers eee ee ne tne the qWIL 19 e 0 624 ok "i tte. * 0 ° ° Pe ; a *h fe ‘HD : of ow =) ve ad wie Ce: mn 6 a “i0) aU ‘0 mas 22 ‘ 2 te Oe te oe OS/hb 0 e Peited r) ad e 0 ° 0 e 0 e v2 ot ce] “2 ra ‘he re *9 0 ‘¢2 22d %22 ve 66 0 “6 - °o ice ; 2 *t2 . rf ‘og P CG °ha 62/h Py =O Pr) Lh yee ¢=5 2d ° 0 e 0) @ 0 eo, §2 Os he "ho ce 2 g2/t 0 6 2 ‘ ¢2 ® 0 ° 0 ° 0 . 2 ° 2 *¢ 2 “b 2 9 0 ‘He he ‘he re 9 o 9 ae 0 _° '¢2 Ue *h2 wife ‘so 2 “ne Lesh ay “0 oe "hz bHe 2 "9 0 *4 av “9 .0 “he te *¢2 ie ‘ho pec °c 92/h . “9 veg "ho ae ®h2 *9 "0 “0 a 69 0 ‘ot le ha te "So we ‘h2 G2/n 45 “0 vas er ‘ho *9 *9 #9 ‘gas 9 ‘oo 6 haga ee "he the “Se font n2/h “0 a a ve We ie 0 COR eet se ae 172 0 ha “2 “cl. ¢e ‘te. wale £2/h *0 mi ge he (fie “he 0 Ug 0 a Oe he he "fe fe nee ee ee/n eas, 169 Whee 0 ‘he 0 sg) syd? og ee “0 ‘pe fhe hg "he ree ube bes 69 “0 ses “he “ns “hz *0 tye 4H er ‘go *h "he ‘He ‘be he "he tne 02/h ° yer: coe ‘ha ¢ “oO ogee oo te n2 ¢t ne oh l/h 0 6 He ry ne ) 0 e 0 ° 0) e 0 e nd 6 12 “2 2 0 e he e he ® 0 a 0 ® 0 e, ne r) he %h ¢ *o aIl/h 2 ® ne 6 0 ° 0 r 0 ® 0 6 ne e red *b 2 n2 r) he e 0 v 0 e 0) ry 2 ry 2 6 ; rd *h LI/h fie. 0 e 0 ° 0 ‘ 0 e fe 5° fe “2 2 he e 0 r) 0 ® 0 e te e te e 2 ib ON/h 0 r) 0 ° 0 ® 0 r) te ° h2 e 2 0 P 0 é 0 ° H2 “ne fe s° h2 ‘ GIi/f 0 6 0 ° 0 @ 2 ° V2 ‘ n2 0 6 i) ‘ he. * Heo he ° hi/h 0 ) 0 8 ne 6 2 e i n2 0 e ne ® 2d e We ®%,75 Fish 0 ’ te e he e tid te 6 H2 6 he e Z2/h h2 r) Hh? ) re nd *h2 We *h2 Ttsh lamer / tr) /t /h e 0 Ps *0 e mie ° e 0 r) 2 r 0 r) he tne ne ° ‘ t ‘ fe ° he °* 0 e fe fic eae 0 ° P hones ho ° 0 ° °0 my) he r he 0 0 6 0 e 0 pull “he oe *he Aue *0 Ue 0 a “0 ‘ *9 ve *h2 0s 42 id 9 9 9 ae 9 9 s: a “He he ° “fe © °0 ‘ 0 ® e ‘ e° 8 c y *he ns *h2 Bue “he a “wt a st) i °0 2 Ss h2 °h oon eC Sees *te ee *he ee id ona *nt o °0 : °He Ate "ye ee he He A 2asH 1asA he seis ete et en pe Gee hag te ate : 4 hOSM how? ha ° : ° aa. Sua Sir * , gaw oer San ate a ca i “He ee a a Hi Te ean anes eae Oe aa We oghe |i hi -SMG @OGM he ees he *h 12 Fay Sau yet ape am gy MH 26MH 1 ‘ha ° a GMA (IM ne p H TSMq 1 /h diva 193f0 ud 110 av *T eo 4O4 SYNOH 3 WY LNMOG 5 SA) ete _ MOTE oer res a PuodaNOD ea ae | mor 4 4 | -_, RADIAN CORPORATION V. MONTHLY METEOROLOGICAL SUMMARY aroN A. Summary Of Ehe Meteorological Conditions over North America during April 1977 April 1977 was warmer than normal for all but the most southerm part of the United States. The Southeast and Southwest experienced near normal temperatures. Variable monthly precipi- tation totals characterized most sections of the country. The polar front jet stream weakened and was oriented much further north than during the winter months preceding April. The mean long-wave circulatory pattern for April was nearly zonal. This differs from the ridge-trough patterns during the preceding winter months. The long-wave circulation was zonal on the lst, from the 5th through the 9th, and from the 27th through the 29th. splie flow occurredson the 13th; the 5th through l/th, and from the 2lst through the 23rd. Meridional flow occurred from the 2nd through the 4th,. from the L0th through the 12th, on the 14th, from the 18th through the 20th, from the 24th through the 26th, and on the 30th. The frequency of extratropical low pressure systems was normal during April. These low pressure systems mostly affected the region from the Rockies eastward through New England. The dates and locations of these low pressure systems were as follows: Psiter Rockies 2nd: Rockies, Great Plains, Great Lakes 3rd: Great Plains, New England 4th: Great Plains, Great Lakes Sen: Great Lakes, Atlantic Seaboard, New England (en: Great Lakes 8th: Great Lakes, New England, Pacific Northwest West Coast Pio ES4s RADIAN CORPORATION Sen: Perr: wth Le: Léth-: iSen: 20th: Z2nG: ZI0e 24th: 25th: 26th: 24 ths Zeeis Great Lakes, New England, Pacific Northwest West Coast Rockies Rockies Great Plains Rockies Rockies Great Plains Southeast, Great Lakes, Atlantic Great Lakes Seaboard Great Lakes, Atlantic Seaboard, New England New England New England Great Lakes Great Lakes, New England, Great Plains On a sectional basis, the following temperature and precipitation anomalies occurred during April: Section Northeast Atlantic Seaboard North Central Central Southeast Southwest Rockies West and Pacific Northwest Temperature Slightly above normal Above normal Much above normal Above normal Near normal Near normal Much above normal Above normal II B-1344 Precipitation Slightly above normal Near normal. Variable; mostly below normal Slightly below normal Variable Much Below normal above normal Very much below normal RADIAN CORPORATION B. Summary of the Meteorological Gonditions in Northwestern and West Central Colorado during Aa ho 77 Grand Junction, Colorado, sixty miles to the south- southwest of the Tract C-b, received a total of 0.54 inch of precipitation during April, which is 0.25 inch below the monthly normal of 0.79 inch. Grand Junction received 1.7 inches of snow during April. Measurable precipitation occurred on the lst, 2nd, MMWen. “hth sch 20th Stand the’ 2Sth. “the region received 77 percent of the possible monthly sunshine. Sky cover by cloudiness averaged 5.1 out of a possible 10 during the daylight hours and 4.4 outsofeaspossiblel10!duringothépentire,month. .01 inch) was recorded at the meteorological twoer on the 2nd, Lich, i2th. 13th. 15th fiGen= and. the 27th. The ipreecipitation. on. the,lleh.and 27th.was.in the Eerm of rain. All other precipitation occurrences were in the form of snow. The monthly average station pressure during April was 789.3 millibars at: the meteorological, tower. ~Thissreading is 5.4 millibars higher than the March average station pressure of 783.9 millibars. The highest daily average station pressure occurred on the 6th, 7th, 23rd, and the 24th. The lowest daily average station pressures occurred on the lst and 2nd. Cloudiness decreased slightly in the Tract C-b region during April, compared to the March cloud cover and insolation statistics.:o The regiom received an,.insolation total of 12,864.5 langleys, which is equivalent to a daily average insolation total of 429 langleys/day. This average is below the normal for April of 540 langleys/day in the Tract C-b region. On a diurnal basis, the greatest solar radiation rates occurred between 1200 and 1300 hours. The greatest daily radiation totals were re- ceived on the 8th;. 9th, L0th,. 14th, 22nd) 23rd. .246h. and) the 30th. The lowest daily solar radiation totals were received on the 2nd, 12th, 15th, 19th, and the 27chs. the gredeest five-minute © Il B-1348 RADIAN CORPORATION radiation total received during April was 7.85 langleys (a Edtemor lo5/ laneleys/minute), whieh occurred om the 13th. The largest hourly insolation total received during April was 81 langleys, which occurred on the 14th between 1200 and 1300 hours and on the 30th between 1100 and 1200 hours. Because of the progressively increasing solar elevations and the increasingly longer periods of daylight that prevailed during April, the total possible solar radiation which could be received during a day increased monetonically throughout the monenh . The slight decrease in cloudiness which affected the Tract C-b during April caused the "very unstable" and "slightly unstable'' stability classes to become more common than they had been in March. Using the Pasquill method of stability deter- mination, "D'' stability (neutral stability) was the most common Stability, oceusring during 156 daytime hours, or 40.2 percent @£ the time. Im decreasing order of frequency, “C" (slightly unstable) Stability oceurred during 146 hours, or 37.6 pereent of the time, and "'B" (very unstable) stability occurred during 85 hours, or 21.9 percent of the time. "A" (extremely unstable) stability occurred during only one daytime hour. Using the lapse rate method of stability determination (D. ene “very unstable 2's). amd neutral “("D"): “stability classes were the most prevalent during April. In general, stable and/or neutral conditions prevailed during the nighttime hours and unstable and/or neutral conditions prevailed during the day. The following table is a diurnal breakdown of the various stability classes. As one proceeds from "A'' to "F", the stability class ranges from extremely unstable to extremely stable. The columm labeled "number of occurrences" indicates the number of times a particular stability class occurred during bh B-1549 RADIAN CORPORATION Precipitation totals in the Tract C-b Monitoring Network during April were generally below normal. The total number of precipitation occurrences were the same during April as during March. Only 0.50 inch of precipitation was recorded at the meteorological tower during April. The largest daily precipi- tation total recorded in the network during April was 0.13 inch on April 15th. The greatest five-minute precipitation total recorded during the month was 0.02 inch (a precipitation rate of 0.24 inch/hour) ; recorded. om,the llth and the 13th. Measurable precipitation (>.01 inch) was recorded at the meteorological twoer om the 2nd, llth. 2th, .3eh, . Sth 19tns andytne 27 cn. Theprécipltation,on.the,lilth.and 27/th.was.in the form of rain. All other precipitation occurrences were in the form of snow. The monthly average station pressure during April was 789.3 millibars at the meteorological tower. This reading is . 5.4 millibars higher than the March average station pressure of 783.9 millibars. The highest daily average station pressure eccurred om the 6th;s 7thie 23rd/.and whe-24th. The lowest daidy average station pressures occurred on the lst and 2nd. Cloudiness decreased slightly in the Tract C-b region during April, compared to the March cloud cover and insolation statistics. The region received an insolation total of 12,864.5 langleys, which is equivalent to a daily average insolation total of 429 langleys/day. This average is below the normal for April 'of:.540 ijlangleys/ day, an,.the, Tract. /C-b. region.) One a diurnal basis, the greatest solar radiation rates occurred between 1200 and 1300 hours. The greatest daily radiation totals were re- ceived on the 8th, 9th, 10th,. 14th, 22nd.) 23rd. 424eh) and. the 30th. The lowest daily solar radiation totals were received on the 2nd, 12th, 15th, 19th, and the 27th... The eresatest five-minute. © II B-1348 RADIAN CORPORATION radiation total received during April was 7.85 langleys (a rate of 1.57 langleys/minute), which occurred on the 13th. The largest hourly insolation total received during April was 81 langleys, which occurred on the 14th between 1200 and 1300 hours and on the 30th between 1100 and 1200 hours. Because of the progressively increasing solar elevations and the increasingly longer periods of daylight that prevailed during April, the total possible solar radiation which could be received during a day increased monotonically throughout the month. The slight decrease in cloudiness which affected the Tract C-b during April caused the "very unstable” and "slightly unstable" stability classes to become more common than they had been in March. Using the Pasquill method of stability deter- mination, "D" stability (neutral stability) was the most common Stabiluey, occucring during 156 daytime hours, or 40:2 percent Gf the tame. | Inedecrneasrme, onder Gf frequency, “C" (slightly unstable) Stabriatye occumred during 146 hours, or 37.6 percent of the time, and "B" (very unstable) stability occurred during 85 hours, or 21.9 percent of the time. "A'' (extremely unstable) stability occurred during only one daytime hour. Using the lapse rate method of stability determination (D): che “every uns cable! 6B '):, and neutral (€'D") stability classes were the most prevalent during April. In general, stable and/or neutral conditions prevailed during the nighttime hours and unstable and/or neutral conditions prevailed during the day. The following table is a diurnal breakdown of the various stability classes. As one proceeds from "A" to "F", the stability class ranges from extremely unstable to extremely stable. The columm labeled "number of occurrences" indicates the number of times a particular stability class occurred during pt B-S49 RADIAN CORPORATION a yn i} ob) 9) 1S) & i=} OQ | CO, tA IN| ea SS in eC COM ise Conmsst Cet fet fe Ce Lo CN ter NS enh fat QA em 2 =o) oO) Oo #8 N ea rs CO N + es =| a » Ce | Oo UV 0 U PAKS) ZO So eet et oS eS SF NAN OB DO SO N - N oa) =a reat tie ONS oa) “Woy te) Ua Woe Ss N - N fl Qi GaN Nt ei erst Oe ett SO (ONE N — N ra al OQ Qa r— NigS es ne) +r Ww N oxo NN al aye) eee) Gah “at Not le Qo Ae OSS SS N cd N od Qi aA ere St OO an nana oc oe a al re rt et co ©:
    ) => 7 (o) Cal a 2) ent ee rm) SC iN col Gal ila > >, eee IN rs = i OO p=) Cal foal )) 7 cet 1 <8] fo) o oO a wd tA ions On So wy Gal) PA Ua) Gy OS Le —~ a a as al jo) Gia oat 2G rN Say Oso Siesta or ® om) al N es N Pras “— SON et SS Oo SIN we iO Oe eS at oO Oo HIN re ea FS 2 eet oot of ao) ww ~ OO) (Al te set IN OO oO ANH AN OO CO a As et ee et et e aad oO Oo nwet wa oO OO nN on est fF OC OC — a oe el] a oe ea) is} > QO 9 et GN OF co EN yO ese EO 6. (Ol Om ete A ( fx a f=] as | =| me ee ON eat ee SS 0 Eee Re re) Se esd es ur EN SCN Oars a Al IN AN “Hy Or o8 on ee Cal tA eet ON (Sih 5) ENS nw NN SS et ao oo eA et >t ose eke Se ON BO ep) ON CO) a Gli CN rs (ob lo a+ OW an ee GaP alin oO «4 uv an An Fs NM @ cd te —a 8 cane ec C35 et rst N eee Gal ee WG! nor wna N Gay ini Te) Key Ch al een oO et Aan re et A On Ae ENO ke) Se Se ret CON eet) tS Oat ec ~ H ~ re aa A ma et eodgcnra Vv bas = fee i eS ju S Oo <2 ea ve i co) bt DN OD WY OD fo) jae} Wea On an a “ord Va w — eorouwnen v o 4 a HIMOARE ° 100>, \and"200~-foot levels were similar. The 8-foot level of the tower exhibited higher percentages of the unstable classes because of excessive mechanical turbulence. The bivane at the 200-foot level of the meteorological tower indicated a pattern of upward vertical motion (negative vertical directions) during April. Upward vertical motion was more pronounced during the daytime hours at the 200-foot level. Upward motions were less pronounced at the 200-foot tower level during the early morning hours. The bivanes at the 30- and 100- foot levels were removed in late March due to instrumentation problems. The ore value obtained at the 200-foot level using the bivane compared favorably with the oe value obtained at that level using the standard wind instrumentation. iy B= 1S oe RADIAN CORPORATION VE. DATA PRESENTATION AND SUMMARY S This section includes summaries for various recorded data at the monitoring sites. The data presentations indicate the variability of pollutant concentrations and meteorological parameters with location and time. In addition, the presenta- tions indicate. the,functional. dependence.of: pollutant jconcentra- tion with wind direction. All data except suspended particulates (24-hour samples) are sampled once each second, but recorded as five-minute arithmetic averages of the one-second samples. This averaging technique tends to smooth instantaneous maximum values, and is especially evident when comparing wind gusts to local weather bureau data. Inherent to any data acquisition system is random noise both from the recording instruments and quantization in the ana- log-to-digital conversion. The lower threshold for all analytical @ instruments is twice the maximum noise level generated by the instruments. This lower threshold is 5 ppb for all instruments, except: fory the ezone analyzer, forrwhich, itis 0.5,0pb. . There- fore, any values appearing in the data presentations that are less than 5 ppb indicate only a trace of pollutant in question and should not be construed to be. absolute levels. In addition, the recorded quantity is simply random noise and averages tend toward zero. Thus, when concentrations are below the lower threshold of the analytical instruments they may appear as a zero entry in the data presentation which does not indicate absolute zero concentration. All pollutant data (except. for“particulate data) is taken at the monitoring site in integer parts per billion (ppb) but is presented here in micrograms per cubic meter (yg/m’*) ED B=1g5Z RADIAN CORPORATION assuming standard temperature and pressure of 25 C eard 2760 mmHg (O13 2 miliibars),-respectively: “The~scale factors: required to convert pug/m* at standard conditions back to ppb for the various pollutants are given in the following table. TO CONVERT ug/m? AT 25°C AND 760 mmHg TO ppb MULTIPLY BY POLLUTANT The units of the meteorological parameters are given in the table. It should be noted here that inside temperature is monitored and recorded as a functional part of the system but is not presented inthis’ report! Table III displays the monthly statistics for each MON LECTIN ess EateLomulor). the: monthy. (jlo; imsure, statistical sig- Hiticance’,, and ito reduce ithe sossibility .of introducing. a bias in the presentation, averages are computed only when at least 50 percent of the samples are present, except for relative humidity and temperature, in which case 75 percent of the samples are required. If less than the required samples are present for a particular parameter, that entry will be blank. The number of ET eB=13535 RADIAN CORPORATION samples present for a particular channel is defined as the total possible number of five-minute samples for the averaging time less the computer downtime less the channel downtime less the channel cakibrationytimes the averages in’ Table £ik@are arien— metic averages with the following exceptions: e Wind speed and wind direction are computed using a vector averaging technique where the wind speed is treated as the vector magnitude. - Particulate averages are computed as the geometric mean. Table IV displays the daily averages. Again, 50 percent of the five-minute samples are required in order to compute an average except for the cases of relative humidity and temperature which require 75 percent. A blank entry indicates an insufficien# number of five-minute samples present for that day. Wind speed, wind direction, and particulate averages are computed the same way as described in Table III. Table V presents the maximum daily five-minute average retained in the data base as well as the time of occurrence. A five-minute maximum average is printed if any samples are present for that day. Therefore, the maximum five-minute average for a channel which experienced considerable downtime or calibration time during the day in question may be misrepresentative of the maximum expected for that channel on that day. Table VI indicates the five, largest averages for various averaging times. The table shows the period of time covered by the average. Maxima are chosen so that time segments IT B-1354 RADIAN CORPORATION are independent. The maximum averages reported are found using a 'sliding average’ technique with the exception of the 24-hour particulate average, which is computed from midnight to midnight. For averaging times less than or equal to three hours, the slid- ing average is stepped one five-minute sample at a time. For longer averaging times the step size is twelve samples or one hour. For averaging times less than or equal to one hour 100 percent of the five-minute samples must be present to compute an average. Averaging times greater than one hour require 90 percent. Whether or not a sliding average is computed is solely determined by the number of samples present in that averaging time and is independent of daily and monthly averaging criteria. To demonstrate the functional dependence of recorded parameters upon wind direction, Table VII shows pollutant con- centration displayed in a bi-variate distribution with wind direction. The tables display the total number of five-minute samples occurring in each concentration and wind speed class. The mean concentration for all samples occurring in each wind class are also shown. This distribution demonstrates the dependence of high pollutant concentrations upon wind direction. Appendix A shows the stability wind rose diagrams. The wind speed classifications used in Appendix A are based on the Beaufort wind scale classification system. This is a system of estimating and reporting wind speeds, invented in the early nineteenth century by Admiral Beaufort of the British Navy. It was originally based on the effects of various wind speeds on the amount of canvas that a full-rigged frigate of the period could carry, but has since been modified and modernized. In its present form for international meteorological use it equates: (a) Beaufort force (or Beaufort number); (b) wind speed; HEB=1555 RADIAN CORPORATION (c) descriptive terms; and (d) visible effects upon land objects é or the sea surface. One land adaptation is the NRM wind scale. The six basic wind speed classifications used in the report are: -l-3 knets,, 4-6. knots... /-10 knots, Ll-L6"-knots, 17-21 knots, and winds of greater than 21 knots. The following table is a complete description of the Beaufort Wind Scale, taken from Physical Climatology, by Helmut Landsberg, 1969. EE EE > PERL BEAUFORT WIND SCALE FOR CBSERVATIONS AT LAND STATIONS ! a, \ Corresponding Limits of Wind Speed ‘ Force | ExXp> ilacery Specification for Use ue at 10 meters ab.grd. fees? VAs Knots | Ka/hr! M/sec. ! Fr/sec. ! O | Calamity sscee os fal Smoke etses wramctca Diy... sas oats a's | <1 3 cle 4 <1 0.3 1 | 1 | Light aki. 2:0 ece ; Direction of wind shown by smoke drift, i H ; | | Gpbucmnoty Uy windivanes., fo. 72 S508 cea pepe eal aS eel 5 2 OR Sa 55 1-5 2 | Ligne breeze...../Wind Felt on face:leaves rustle:ordinery | | | | | Whe YMtalcis argue ch Wb yn cetera cha ote: aye th on ajaite, da eev singe p= Teil eG ome 6=— le ell 6 = 35.3 6-11 | 3 | Gentle dreeze..)..} Leaves and small twigs in constant mo- ; i : } | | |, (tLongwimd extendselienec flat... o1.cheepeusrcrehe : 8-12 ! 7-10 | 12-19 | 3.4=5.4 | V2=% 4 Moderate breeze.. | Raises dust and loose paper:small bran- | \ | NG chee dare moved .prrs J. gett ters se atihore nice iy toe) thy BING. | ya0=28 15.5 5=7.9% || 19226 5 Fresh dreeze..... ‘Small trees in leaf begin to sway:wave- i H | | lees-formed) onvinlandcwaters...< .\. ss «aeaels |; 19-24 | 17-21 | 29:=38 sl 820=10 275 .27=—35 6 Strong breeze....iLarge branches in motion:whisctling heard | H i im telegraon wires:umbrellas used with |! | | | | GU EER OWL GY cticic, clecinisreis aera oio'e.e:ausre, evens, 5 ciaceters 25=3L | 22527 39-49 | 10.8-13.8 |] 36-45 7 | High wind........iWnole trees in motion:inconvenience felt | | | when walking against wind.............0 32-38 | 28-33 | 50-61 | 13.9-17.1! 46-56 8 | Fresh gaie.......:Breaks twigs off trees:generally impedes , \ | | | We OROeresSis ox anise teem aca en eee oe | 39-46 | 34-40 ; 62-74 | 17.2-20.7| 57-68 v] Strong gale......:Slight structural damage occurs (chimney | pots.and: slates removed)... cece ce neue s 47=54 41-47 75-88 | 20.8=24.4| 69-80 10 Wnole gale....... ‘Seldom experienced inland:trees uprooted: considerable structural damage occurs... 55-63 48=55 89-102 | 24.5-28.4 81-93 LL | SEO LM aii cieie wvererenenoe 'Very rarely experiences:accompanied by | | | \, -Widespread) Gamage i. ss acerocse as sec ee «6 j 64-72 , 56-63 | 103-117] 28.5-32.6| 94-106 12 HUPELCANS cs ose ac ihie ew « chord 0 31s oe ene mw Bite ates lo ee/eere eteyane elAa omer aan s 73-82 |; 64=71 leiigenas 32.7-36.9 | 167-121 LS) py lsated ish ctncle Be Cerccc stout tae ace oo 83-92 | 72-89 | 134203 37.0-41.4 | 122-136 | Bed sere mise tine rugs ee Joc eee cece een cece nee ee ences eee e erence ees 93-102| 81-89 | 150-166 41.5-46.1 | 137-151 ae oe eerie eS ds tic ee re Sri ee oe 1104-114 | 90-99 | 167-183] 46.2-50.9 | 152-166 | 16. Visas awainc an adsn we tain nae CL ae See oe ten « Aare a ee | 115-125 | 100-108 | 184-201 ! 51.0-56.0 | 167-183 | Lar \eieieghiate ese) aenavetwbapene Laatecuiaicte Brogan seal Nias de Merce eit se arte one Seater re 26-136 | 109-118 | 202-220; 56.1-61.2 | 184-201 { ! i Source: Table 36 (p.119) in R.J. List (1951) :Smithsonian Meteorological Tadles:Smithsonian Miscell.Coll.Vol. 114. II B-1356 RADIAN CORPORATION Table VIII demonstrates the diurmal variation of various recorded parameters. Hourly averages are determined by arithmeticallv averaging five-minute samples, except for wind direction averages which are computed vectorially assuming unit vector magnitudes. Totals in the diurmal wind direction tables are vector averages of the columms and rows. For all parameters, a blank entry in the diurnal variation table indicates that less than half (i.e., less than 6) of the five-minute samples for that hour are present. All times given in the data presentation are Mountain Standard, Time. To facilitate comparison of recorded concentrations to ambient air quality standards, the following regulations are presented. EES B=2557 RADIAN CORPORATION TABLE. ET FEDERAL AND COLORADO STANDARDS Non-Designated Designated Area Primary Secondary Area 1973 1976 1980 Particulate Annual G. M. 75 ug/m°> 60 g/m? 45 ug/m? 70 ug/m? 55 ug/m> 45 ug/m* 24 Hr. Max. * 240 150 150 200 180 150 Sulfur Oxides Annual 80(.03ppm) -< 60(.02ppm) 25(.009ppm) 10(.004p.m) 24 Hr. Max. * 365(. 14ppm) 15(.005ppm) 300(. lppm) 150(.05ppm) 55(.02ppm) 3 Hr. Max.* == 1300(. Sppm) -- ~< -- -- 1 Hr. Max. ** -- -- == 800(.28ppm) 300(. lppm) == Oxidant l He. Maxe* 160(.08ppm) 160 8° Hr. Max* -- -- Annual es == Hydrocarbons 6 3 Hr. Max.* 160(.24ppm) 160 6-9 a.m. Carbon Monoxide Max. 8 Hrs.* 10000 (9ppm) 10000 Max. Hic. * 40000 35ppm) 40000 Nitrogen Dioxide Annual 100(.05ppm) 100 Units are micrograms per cubic meter and ppm in parenthests. *Not to be exceeded more than once per year. k*NOt to be exceeded more than once per month. [f-B=1358 RADIAN CORPORATION TABEESLIL AVERAGES FOR APRIL 1 THRU 30 II B-1359 Tf B-d3560 RACERS RSKRASEUD RASH RMA MEROKDH MR Re Daa MSNAAASUHAASHAASHAS AAMAS ASTRA EK EDA K Antennae 0°g 0Ss° £20 ¢20 aLIs ALVINITLYVd NOLIVLTdI93Ud WLOl g°6R@l 9°08 £20 ¢20 £20 SLU JHNSSANd ILYLIWONVG JNOZO0 JGIXONOW NOGYVI ¢°262 0°16 S°eoet £20 £20 $20) ALIS SNOGYVIOUGAH ANVHLSW-NON JNVHLAW SNOGYVIONGAH WiOl eo S*poget Ge ¢20 C20 ¢20 airs JGISINS N3XONGAH HYILIWONVHAd (ZosjyaaqIxora ansiwns tot Sia | G*2 ¢20 ¢20 ¢20 3111S (ZON) A0IXOIO NADXOYMLIN (ON) 3JG1XO JILIN (XON)SIGIXO NIDNONLIN (SIHINTONOTLVITdII9Nd LSUVALIITWSNNSSANd FSAATINV) WILOL*Y3SLIWONVYAd {HIYON JHL OL 193dS3N HLIM SASYDAGH@NOILI3INIG GNIM SLISHNANHV4 $39u9I90+9NNL VU AdW3L {YNOH Y3d SAIWW8dI3adS GNIM fYSLIW IJTANI 3d SWVYDONDJIN@=SNOLLVYLNAINOIISLINN) O€ NYHL I Udv YOd SINVHFAV “ITT Javi NOMYWHOAIOD RTO 7 eo if B-1361 GS & ow be Ot Ob Oe 08 GS GD we Ob & BF OD ae oe OS OS OH OP Oy Om OD GD BD OS GD OD OO OD OD OD GD & & ae & Ud GD @® O8 Ut Ok co OD GE OD GS Ow OD OS at ap Ae OS G0 OO te MS OD ab OD OP im GD Ge ae OP OD ay WS oe OD GS od GO ay Go OD OD Oe OS om Oe wD Os oe Oe GO me Ge Oe Ge oe ow Ge a GD oe OY hy OS ¢°2h 0°Ch n° oh 0°2n (i4-002) (i4-001) (lL4-0f ) (ide) €¢20 3LIS JUNLVHadWSd 7°99 n°@9 L°99 2e°L9 (id-002) (l4-003) (l4-0f ) (l4a-8 J) ¢20 3118 ALIOIWNH JATILV1398 C0 On Oe oe oe ew OF O&O @ & os ie we om 88 ee me em & Oe Ft ED Oe & Oe Oe Ob OS Ge ow 8 ted ee om ae 8 68 om we Us Om 60 Ge on ot OD OD OR om He Ob om US om & om 88 OR oe) ay om by Oe 60 He om Oe Ge OF OO GP ey Ge OO Gr ow OS Ge me Gn By om be Gh OH om GD OD OD oe OD tthe S*t¢2 i’ ite bh Vinie (14=002) (14-001) Ciae0t ) (isa) Se0 Sas NOTLIASHIG GNIM Tee ve 0°2 S°t (14-002) (lj-001) (ij=-0f ) (La-8 ) t20 42's QA3dS (NIM (SJHINI=NOTLVLTdI99Ud (SHVAIDVIIW3NNESIdd CSAFIONVT WILOL*NYASLAWONVYAd {HLYON JHL OL LIAdSAY HLIM SAZNNIVGeNOTLIANIAC GNIM SLISHNSYHVS SAFINIAISIUNIVYSdWAL !YNOH Y3d SIWWdI9dS GNIM CYILIW JIANI Y3d SWVYNONITWSNOTIVYINSINOISSLINA) oo O€ NYHL I UdV e SSOVYHSAY “IIT 378v1L NOMWNOAHOD = a Aen Cas ar RADIAN CORPORATION TABLE IV DAILY AVERAGES FOR APRIL 1 THRU 30 II B-1362 tl B-1563 0° 0° 0° O¢/h h° Q*y 2*e be/h ved 9°) 0°6 R2/n 0°2 ne hoe Le/h G*et 0° G*2t 92/n 9° L*e g°¢ Se/h 6° One 6° hesh a | On £1 ge/t 2° ft 0° hate ed/n LH s° 0°S Ve/t PY orrTrrerrirerprrteeyeirrerrreelreTt le he eee ee teen ee en ean ae | 9° te 02/n tt e*t 6°2 6t/n Git bt 9°2 “Ot 70 ‘agg 0°t L° LV/0 Cs ¢°9 6° 9I/h 1° G°sS 9°S Gl/n 0° Be vr nish es c° S° ¢I/h 1° Het 9°41 2t/t ~ et e*'t List 0° 0° 0° OT/h 0° 0° (oad 6 /0 0° 9° 9° g /b 0° 9° 9° 17h g°2 al g°2 9 /h g°t 1° n° Get 0° t hy h /v 1° \ bed 1e £ /h Tg 2° Q° 2 /t Tas 0° ce Sev Aly jJiva £20 &20 ¢20 311S (20N) 30IXOIO NISOULIN (ON) 3GIXO JIYLIN (XON)SFJAIXO NIDOMLIN (SIHINI@NOTIVITdID9Nd {SUVAIVIINeSYNSSINd (SAF TONY] WILOL*YILIWONVHAd {HLHON JHL OL 1939d89Y HLIM SAFNDIO@NOTLIINIG GNIM FLISHNINHVAS SAAMIIGSINNLVAIdwW Il {YNOH M3d GSATVIW=03939dS GNIM {HFLIW IIANI Y3d SWVYDONIIW=SNOTLVYLNAINOIESLINN) 0€ NYHI F udVv YOd Sa aNy AlIvd °AI 3798V) NOLLYHOSNOS gy 2 oo TTA ET 4 4311S 0 6 g l 9 S hn + 2 J 0 6 Q E 9 S i] g. 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FC a RADIAN CORPORATION TABLE VIII DIURNAL VARIATION OF VARIOUS RECORDED PARAMETERS IIT B-1410 Lae rosy 1 fry a CORPORATION r h £ uty aNd dt ' | DIURNAL VARIATION OF NITROGEN OXIDESCUG/M«x*3) 4/30/77) PERIOD( 4/ 1/777 TO 25 TRAILER NO, HOUR 24 MEAN 23 3 14 AS We ky ie le 12 10 DAY oo a3 i o * 3 * 8 —NuNO bale | ait | 10 ait) «8 ® 10 * Laie * 4 13 14 15 16 17 18 19 ce 10 xy 10 10 Wt MW re? 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JL IC (HSW) 1334 8 LY 0330S ONIM JO NO} LYUIYUA TYNYNIC oe 1 St, 88 OL Sh Oh fl Sin Cte iL (HdW)Q033dS ON] O'Sst II B-1461 RADIAN CORPORATION bc = 3S (HdW) 1334 O& LY d33dS ONIM 3O NOJLYIYNA IWNYNIG YNOH Re bec Aa ode “Bh Bl tl Sh St ht CE et 14 Ol 6 , 8 € 3 S ch © -@ ot | {| ‘| : H h j po Set OCS (HdW)033dS ONIM EE Be 1462 CORPORATION RADIAN he ae 2% ~ JLIS (HdW) 1334 OOl “id G33dS UONIM JO NOJLYIYYA TWNUNIC YNOH i 02 6U Bt AL SE St At = ct \t Ol G @ &£ &§ © h € 2 0°02 (HdW) 033dS ON] II B-1463 RADIAN CORPORATION = ahs (HdW) 1334 002 ike G33dS ONJM JO NOILYJYBA WWNYNIG pele he t% 2 1% O% Gt al LI 9 ne el at wool 6 @ 6 9 S he 2} o aol (HdW)G33dS ONIM 0°02 II B-1464 CORPORATION RADIAN Seas 1333 8 LU NO} LOIN CNIM JO NOJLUJYYA TWNYNIC uNOH ne GEE 220 12 HOE S61 181 CL 39 Sot HY fst iv 0°08 | NO] LI3ZYIC ONI]s O°OSE TE B-1465 CORPORATION RADIAN = 31)S hoes (OG by NOILIIUIO ONIM JO NOJLBIYYA TWNYNIC YNOH eee ree i BE SE er ol We ee Sh eet O°O8T NOTLOIS¥10 ONIM DOSE II B-1466 RADIAN CORPORATION = aS 33a OO Le NOI LOauIO QNIM JO NOILYIYBA TWNYNIO YNOH he €2 2% 12 02 G1 Ql Cl gt St hl El ct Wool & O°ost NOILIS¥I0 ONIM O°OSE II B-1467 CORPORATION RADIAN = 3LIS 1332 (00c 8 NOILO3UIC ONIM JO NOILYIYBA TENYNIC YNOH commas See oat VRl GCE sL ISU Ont Chae tI al ob Bob of gS a ob oe 1 Oo o-ost NOI LOSYIC ONIM O°OSE II B-1468 RADIAN “92115 IEEE rato ed bc LLIGIWNH JAJLUI3Y 30 NOILYIYBA TWNYNIC HINDH Rowec RZ Nic poe ght gel cel ga Vet) [| et 01 8 0°OS (IZ) ALIJOIWNH 3A} LY13Y hi O*OOot CORPORATION II B-1469 RADIAN CORPORATION CC == ILS 13343 Of LY ALIGIWNH JAI LUI3Y JO NOJLYIYUA TWNYNIC YNOH te €c cc le Oe Gl Bt Et ST St Rl Gt cl Wt ol. & @ € Ss S&S WE Ct Mf f A § ’ ‘ ; 4 HW A q \ i f i A 4 \\ | A ti ) So 0°OS (YJ ALIOIWNH 3A] LY 13y 0°O0l II B-1470 RADIAN CORPORATION = ais 334 ODWalg LLOIWNH JA LEZ JO NOILYIYYA TWNYNIC YNOH Le a ese Racha al eh 0 Riis I ALIGIWAH 3A) 1Lb13Y l O°oot ED Ba147t RADIAN CORPORATION We GG. cc = JL)S L333 O02 Lb Losin SAI LU13Y JO NOLIVEWA THNYNIG YNOH We OC GUcet Ci rSt St. mA oc: zt ut ae eS O°OOL (SJ ALIOIWNH SAI LU ay IT B-1472 tc. —2LIS (4 930) 1334 8 LY 3YNLYUYSdWIL JDO NOJLUIYUA IWNYNIG YNDH he G2 UZ 1 Oe BL al Lt 91 SI cL tt ou a3 ™ aS = ma 20) 28) al tah G& hed yas 0 or mM eas} ™ q) “Ty — oO S ren) Pie 1475 RADIAN CG et ALIS (4 930) L334 Of LU 3YNLUYSIWIL 40 NOJLY)YWA TWNYNIC UNOH NaGocae tects 8) Ll Ot Ci ht Cl cH 1h f i 4 A | ' Ml q j i ) 4 4 i q i i : ( { i 4 i 1 if ay Mm aT “yy mM 3) D wna vcAr Ae 2 20 eo FN &) mM Q) 14 | =) a oO CORPORATION TI B-1474 - 31)S (J 930) 1334" O01 LU JUNLYYSIWIL JD NOJLYIYWA TWNYNIC le he €2 U2 i o% GI BI Li 9 ol Vt ol ey o So (4 930) SYNLYY3dW3L 0°Oot II B-1475 CORPORATION RADIAN . e = 3)s (4 930) 1334" 002 LU 3YNLYYSdWIL 40 NOJLYIYWA TWNEHNIG UNOH he €2 2 WZ. 02 Gi Bl Li gt St EL tt ov Gos {3 030) SYNLBYS SNSL O“OUt II B-1476 RADIAN CORPORATION ~ 3LIS junsSaud JIYLSWOWNS JO NOILUIYUA IBNYNIC bNOH he ee eh, a Se ee ee O°osL O*06d 0°C08 SYYSTTIIW EL Bol477 RADIAN CORPORATION Eu > seas CAJTONYT)INOILUICUY YWIOS TWLOL ATUNOH YNOH GUCCORUCORICMOCR TE MUON ALY Stes Vethi CN CY NOL 6 Ge bag Ss ho ee A i 1 i " f { : t i 0°OSh 0°006 NOJ LO] OY II B-1478 ne €¢ tc 1G 0CG6! Bl Ol Si Sich! EL ch Ti9vl gs © Pf SoS hh f € RADIAN CORPORATION Roy as 1334 00@ LY O33dS ONIM JNUA-]8 JO NOI LYUIYYA TENYNIG YNDH a ~ —+— rea) got O02-d3adS GNIM SNvA-Ig 0°02 Pr B= 1479 CORPORATION RADIAN = 3 1JS 1344 00¢€ LB NOI LO3ZYIO aNIM JNUA-18 VWLNOZIYOH JO NOI LYIYYA TIENYNIC YNOH Lo ORE ieee ea Ne ae ae Oi ee “Z1YQH O*ost 00¢2- NOI LIS¥IG 0°O9£ II B-1480. Rca Fh CORPORATION > { 4 ty. 4 yy fit iri ew rer ws «=| CeB SHALE OIL PROJECT METEOROLOGICAL TOWER SITE STABILITY CLASS DETERMINATION USING PYRANOMETER RECORDING 4/30/17 i) . w) PERIOD( 4/ 1/77 TO HOUR 23 24 ee ail 19 H7 16 v2 oO aa aUMO WoOouAdanc YVYOonuUNU0 eaarvad avoon aaqo0aunsn fan a om Be 0 ce) ovo ta & ooTonad oOo OaAvUvVUU gounmov 4/ 4} 4/ 2 4/ 3 4/ 4 4/ 5 auaaca gooa qgaaqgagangouanad VUQUIag aaononanuaaga Oepmpaananaganaa eaeoeadcakdsonana BomM0aaocroads mampoaacoadaas namaoaoawmdvuuad eaeaaoaanaaovuaond Booackgaa0oas OpDbpeodao0ucu usmYUGCVUUNU OA ad WwOoaa & (o) 4/ 6 4“/ 7 4/ 8 4/9 4/10 N/14 4/i1e 4/13 U/\4 on © | Qo a a ©) Oo a qa aa a Go fon) oO au (an) fam) Qa ao 4/15 QO =) Oo =) 4/16 4/17 QaAuankunsa «} QO tt Y 4/18 4/19 4/20 4/2 4/22 4/23 4/24 4/25 4/26 4/27 4/28 ou D 4/29 4/30 * NON#ZERO PYRANOMETER READING BUT STABILITY CLASS UNCERTAIN SINCE NIGHTTIME NET RADIATION INDEX IS REQUIREC II B-1481 20- 2h -2e2 “25. 24 19 Mi OWKWURLOWODBLLOKXLOVULEREELEKR We QOwWWUuUeWeuowWwhwW Te OOSWDLWH ei lid bi AQAvasnwuie bw YwaewWewoDna Dov RkReWk ened dokb wm QMUWOWRAYWU Re WODWWOWWaA WOW e ws O Ui GQoadwrekbw we uwowuotovwoowwaeqoowoaaderdtw oOmsnamaeawoaoovadtmopmntouanqovdoarttrnoasdaga 4/30/77) HOUR 15a 26 14 12 ox D aaonaaa oBavovaunacea aaim Oagaxta anagavaductc ace DO aauvunuoe waumavmvao0avuona ata aonxa ea manrovuaorda aa S t MSS 383 2 £ 38 2 38s ass } L MS 2 MN MN MN o 20 0 MSS MoM = MNN MNN t S$ t 9 & MSM NOMWNoOAdNoOD ?P "a ‘ uy II B-1492 Ss Mss S 2 ot ft 383 ¢ oom 5 M M 2 S M MN q 2 § ¢ as 38 368 y 2 -& 38 38 383 h S as 36s 0 S § D h2 €2 22 $ MSM MSS 9 $ 38s S MSS MSS h 6 ass . S MSM fe Od 6t MS L 3643 3S h 3s JS u] t 3S JN é I 3$ @ Gis 21 91 St ft Et eh St] OF 6G 8 L 9 YNOH SSV19 ALITIavis 4 NOTLISNIG GNV ONIM ATYNOH (LL/0G/H OL LL/T /b JOOTYHISd 3S 4388 4s 3S MS MM MS S 2 t $ a>... 39 L . 4as3 S 3ss § AN S$ @ i} 0 ¢ S$ 3NN N a5 263 2 2 e @ aM $ qS.. 494 2 h % t (1 T3A57) 20/10 SNISN NOTLYNIWY3SL390 SSV19 ALIIIEVIsS JLIS YSMOL WITIOTONOALIW LISDLOYNd TIO JWHS Aad NOlLWROAdNOD ENTRAR 3s MS MSU MO TT B=1495 3ss ass wy lJ mus ow ut wa uJ wn {uJ ut wm a we SKU VUWN OPS vs a ty a 4: 2%. dae 4 MNM 2 MSM MNM é 2 383 AN MNM MM M i 1 2 ¢ ¢ MSM MS MS MSM t 2 2 9 MNN 9 3ss 3ss ass 9 6 OT MNM ¢ NOMWUAOduOD PRTG cel mz MNM MNM un Jb Jn II B-1502, MS TT MSS MSS MSS Lt 91 3NN 386 MNM 91 St MSS S$ MS nt ht MSS S 3N 8 JNN N 8 0% INN L MNN MNN M MS MS Qt 63 9% gt 9 3N SSV1D ALIVIGVIS ¢ NOTLIAYTIO GNV GNIM ATYNOH CEL/0271 OL LL/71 7G O01 ad OS Us oz MNM MNM MNM 3 h e 2 0 (2 VW3A51) 70/10 ONTISN NOTLYNIWYSLIO SSVID ALITIAVISs JLIS MSMOL WITSIOTONOSLIW LISFOUd WO JIHS G=9 NOMWHNOdNOD oz Q EL *B-1503 O£/h 6e/h Be/h Le/h 92/h Se/h nest £e/n 2e/h le/b Oe/h 6T/h 8t/h LI/b 3Sss My We “ae MNM mE os Ze 3NN = ass 38s Lengo MNN 9 MSS 8 as 6 St at ETS 9 as ass nS 3a «as dail | Cl LE. Ot. (Sh “Pi GSi-wdt LE 0F -6 g L 9 YNOH SSV1D ALIVIGVIs 3 NOLTLIAYIG ONV GNIM ATYNOH (L4L/0¢/b OL LL/T /b JOOTYAd (2 13A31) 20/10 ONTSN NOTILYNIWNS1LIO SSV19 ALTIIGVIs JLIS MY3MOL WOITSOIOYOFLIW LIZLONd TIO 3IVHS 99 » ISS § 9 4 M 2 N 1 $ 4aSS § 48S 4386 6 L S @ @8 ass 3S asa 3S 1 9 6 OT MNN MNN es: MSM 2 MNN i M M Loe NOMUUodNgGS II B-1504 383 MNN 3$4 ss ~ = Mi 3N ot MSS MS MSS tT 3S 3839 4SS MSS i] g g +7 : 3N3 MS S 3S$S JN 4a S 3 1] 2 2 0 J h 3S§ N MNN 3S 2 0 J \ 3N3 MSS 2 Q S S re ty A 3 MS 2 0 1 M MSM N MS 3N3 N 0 1 i 0 J 0 MNM t 363 ass ¢ 0 MNN MSM if 1 MSM MNM MNM MNM MN ON 1 I 2 S ¢ L aN M MNM 0 0 if SSV19 ALTVIAVIS 43 NOILIZYIO GNVY GNIM ATVYNOH (LL/OG/h OL LEAT sh )OOTUAd (2 V9A391) 20/10 ONISN NOTLYNIWY3L39O0 SSV1D ALTIIAVLS JLIS YAMOL WVITIONINOALIW LI3LONd W110 FIVHS AW) 4 NOMWHOdHOD NINA 8 TT *B=1505 O£/h 62/h 8e/h Le/h 92/h Se7 i he/sh Le/n ee/h Te/h 02e/h 61/h 8t/h LI/h MS§ 2 as x 3S 43S S h as 0 He. ee Ze te ~= 02 6} Tz @ 3ss 3ss 3S 9 h Q Y MSM N S i MSS 25 366 JSS aS¢ Hse a66°6 ass S h 2 0 1 2 2 46-488 MS: 38 2MS¢ 1 t 2 2 2 3SS 3S 3S3 MN ¢ E ¢ 1 Glo ti St Gi. Pie Sho et Ab 0b 6 8 ra 9 S uy] 3 2 J YNOH Ssv190 ALIVWavis 4 NOITLI3AYTIQ GNVY GNIM ATYNOH (LL/0&/0 OL List /h JOOTHAd (2 IHA31) 20/10 ONISN NOTIVNIWYSL3G SSvV1D ALIVIAVIS JLIS Y3MOL WITSOTONOSLIW LIALOYNd WO JTIVHS 99 NOIMWUOdNOD a eae A fi B-1506 MSS MG MS 3ss 38S 3S§ Li 0h Ot 8 8 f 3ss s 3s - 8 9 z MSM 3S S 2 AN JN3 MNN MS t 2 2 g M M&S ass s 38 mss § iL Vt £ 2 t 2 2 3S 3N “S MS 3$3 363 3SS MNM MSS £ t 5 LE 2 ¢ 0 0 1 MNN ro M 3S a N as 3S3 t t ' 0 4 t 363 MNN MSS MSS S 4s 0 t Z 2 I ie MS MSM MSM 3S 4384 ass t 0 0 d g 0 P| N MNM 3 N 0 t t 2 0 SSv12 ALIVNEVIS J NOTLIZYIO GNV GNIM ATYNOH CLU/OS/i “OL £2L7\ 7h DOOTdad (2 T3AZ1) 20/710 ONISN NOILVNIWHNSLIG SSv19 ALTIIGVLS JLIS YaAMOL WITSNOWYOILIW LIZFOYNd VIO 3TVHS d=9 4 6 ~— NOLLWHOAUOD ry ss@ Ve Mitre ae, Bae a 4 t i - TT B= 507 RADIAM CORPORATION APPENDIX A STABLLITY WIND ROSE DIAGRAMS II B-1508) RADIAN CORPORATION APPENDIX A STABILITY WIND ROSE DIAGRAMS According to the data presented in AEC Safety Guide No. 23, the relationships between stability classes and Jo are as follows (the values shown are averages for each stability classification...a, is the standard deviation of horizontal wind direction fluctuations). Average Values Stability | Pasquill Tg Classificatzvon Categories (degrees) Extremely Unstable A 7s Og Moderately Unstable B 20.0° Slightly Unstable C 15210 Neutral D 100" Slightly Stable E 5a0 Moderately Stable F i a Stability wind roses obtained at the trailers in the monitoring network are displayed in the following tables. Because of the relatively low heights above the surface (9 meters) at which the wind data is taken, the stability distributions are skewed toward the unstable end of the spectrum. That is, the unstable classes (A, B, and C) have a much higher frequency of occurrence than would be obtained with the Pasquill method of stability categorization (or with instruments at higher levels). table, L depicts the frequency distribution of-Pasquill 0 from data collected by M. M. Pendergast and T. V. Crawford at the Savannah River Plant stability categories based on o ("Actual Standard Deviations of Vertical and Horizontal Wind Direction Compared to Estimates from Other Measurements", Symposium on Atmospheric Diffusion and Air Pollution, September 9-13, 1974). Three distinct range patterns of stability class IIT B-1509 RADIAN CORPORATION wv distributions were observed-— tow mid, and high, according to x the height at which the Og Measurements were taken. TABLE 1 FREQUENCY DISTRIBUTION OF PASQUILL STABILITY CATEGORIES Stability Cetescries based sac SE I TO LECCE ae A 8 C 0 E Bi G = ae Gy 523. 12 £55 <23 l3 ve, <]2 8. <<, SOY Ney S55 S07 2S 8h 2h zs 6¢ Sh gh gl : Aviol see Gle 8 S Gt &t gt nt St Qt St iy 22 L2 62 nt 12 vt St 2 e Te See ueoh veo won -G0. = 22 -be os Ge » OF 6b. ee Ge Ht vote = 0S 6 bt . 9% 8 : = ¢ Pee top oe oat OC OF kG oe 1 Se. OF. € t S ¢ ¢t 92 re em | “rt Olt £ 2 9 S i] ef SG =o ey US 2 I : gt = ef “ttn = 2 l L : he. 2 ON *0 ; : ve. 19 HdW 93 9} nt ¢3 ii Lt 02 02 nt Ot g 9 tt at tt 2t G34d8 XVW dNOUd % ‘WiOl MNN MN MNM MM MSM MS MSS § 366 4& 383 3 3N3 JN 3NN N NOTLOSHTA QNIM Q = SSV193 ALIVIGVIS (ZL70¢/b OL LL/t /h YOOTH3d 1334 8 =& 13A5) L9afOUd WO 3IWHS dd WYYOVIG 3S0¥ ONIM ALIVNIGVIS NOMwUOAaNOD Ravn ad ‘oot Tene pEe AOL TIES ‘ot 6Sh Som fee ote atic *0 *S eat £1 bh 9S 91 Me B= 585 (% 99°S LEI = JAOGY AZLNAIYLSIG SW1V¥9 3O Y3EWNN AvVLOL ee@eseeaeetCoeececesneseseeeecseeseseaeseseeee eee e ce CGoeeeeveeeeseseeeseseoeoe soso Co eKCRECHRHEBHEHO HOOKS KHHEKEHOHOKHEKCHKEHHOHKHHHKEECH4E *Q Hy) *h *9 rie He Sloe ee'6 or °g °s 45) aS *2 Sie ay) : IN3943d 002 98 96 Gt “HOno = tes tte TET “Set sot! 2nte 29 0S 8S 698 : wilol 22 he 1¢ 0S ¢STt 6 6S 6S Ll 29 £9 ¢¢ bt 6} te t ¢ tal C6 OSa6 ci 16S Ont OF 166) 908" tl One Ge 2ecme et Ve Goo et l » § gs g 12 92 is 9S £S he Lg 2 t Ll St Lt 92 $ Zz} = 1 92 h 2 9 Sh ¢@ re 2 t 2 t 9 3 Qt = 2] 1 S ¢ 6 9 : he « Qf t he 19 HdW ST Ht nt 02 12 02 bt 9} Os Q g ct ct Zt ht Ga3adS XVW dNOYd MN MNM M MSM MS MSS § ass 3s 3s3 3 JN3 3N INN ON Ae IW EOL MNN NOTLIZYIA ONIN gd @ SSV¥19 ALIVIGVIS CLL/0E/h OL LL/t /t JaQOTYHAd 1334 8 = W5A31 LI3SLONd VO JIWHS Ged WYYOVIG JSOYN GNIM ALINGVIS @ pi Slee Rance] @ II B-1516 (% S8°6 )092 = JAOAY GSLNAIYLSIQ SWIVD 40 43BWON W1OL COOH HEHHHREHHEHHHHEHEHHH HEHEHE HESHERHAHE HHH THHOHETHHHKHEHHHHHEHEHHEHEHEHEHH OHHH HHHOHKRHAHO HHH OE HOES "001 ae! *Q i ay °9 mae: =O) = "9 *g ay! ‘9 Pall “< *s a °b $ IN39u43d On9d £ GLE hte Lot t8 66% ¢£hS 92 B02 29t 981 O9ht Ttt £9 G2 cs Stitt 8 Wlol “th O9TT & Ch Sh 8S ES el bSe- Set $9 98 S6 oot L9 ¢h Gt ve 6% i & a “Si S2tt.$ SO.- 60t 9h Sf S0t LS$2 sot 18 69 28 9h. th 22 6 9 fh 3 l a § ‘Ol 952 $1.29 OF 4 S Ol tk, ON or 6 Z 1 ¢ 62 3 eto | ‘“¢ fA 1! 6 Oe = Gc h 9 By Gk. I ¢ : et «= 2t ; 0 Ste 3 1 h k 1 : h2 = OT LO), t 3 1 : He rls HdW Gosh fr ht "oy oe.“ pe Phat eis tty ry Sh G Cy 4 et gt Qa3dS xYW dNOUD % WwlOl MNN MN MNM MM MSM KS MSS § 38s 43s 3gsa 3 JNJ SN JNN N NOILISYIG GNIM 3 = SSv10 ALTIavLs (LL/0%/h OL 22/3 /b YGOTYSd 1334 89 = VW5A37 133F0Ud WO Z31VHS 89 WVNOVIG JSON GNIM ALIVWGVIS NOMWUOAdNOSA LT B-1517 % ce SE @ ALI VIGYIS 3 30 39VINAINAd % of°2o @ ALTIIAVIS 0 JO 39VLNSIN39d x t9°9T @ ALTVIGVIS 9 JO 39VINAIN3d move 79 = ALTUIIGVIS g JO J9VINIINAd % 8t°6 © ALTIVIGVIS vy JO 39VINSIN|Ad Chow k yess BAOAY GILNATYLSIG SWIVI dO YSSWAN WIlOl CEO DEK EHH REDO REHE HHO EHEEHAEHEH HOE ORAEEHHEEEHTAEHHSHRHHHHHEH OH OHEHH CHEECH HEED H HOHE SEE REED SS "oot % 2 *6 "Gh. sibs) Os a *9 ‘9 °S *h "¢ =e *S; *s : IN39Y3d Ob 1 HOS €L9 S9E SOE H8h Fatt t2e ehS fh 99h Bes LIE Bre FBI Tee Oh § vL01 Soe fie fe 2) eft Ott 2St ‘efh 652 GT b61 @¢2 6fe S61 @et 68. 20 Ich % ¢ 17 ‘th €605 t 602 29E E6t Het 2t2 99h Hee het Sot hot Htt oO2et fe 89 O0T FAT $ L ~ £ Com eia ty hot 2et 6dr Sh SO Ss tht Het Ssh 06 § 2 9t 22 eh 6 & rf a 2 hs tos tie s5 tt) Of; te G21 991 95 § ee ee eo ee a cet te ft 1 S h 02 02 J : ne» Bt mow ' i he a . Hd Near ft te Oe’ te. Se ie Sh Te Tel ah ee aot aa3dS X¥w dnoU9 % WilOlL MNN- MN MNM M MSM MS MSS §& ass 34S asa 3 3N3 JN JNN N | NOTLIBNIG ONIM aylol « sSv1) ALIMIAVIS (LL/0¢/b OL LL/3 /h YGOTYSd 1334 8 2 13A31 Loar0dd WO AIWHS Bed WYYOVIG 3SOUN GNIM ALITIGVIS * . e nena | 6! 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RADIAN CORPORATION iN ga 7 : Pee eee se ae S i mad ce my aoe . — ; — *S f Pea ae ae \ J \ i ¢ 4 j F E 1 ‘ f , i i % ! i ; § ; \ i‘ \ é \ 7 re J \ \ \ : : “ , \ . “ ‘ \ eo eee \ is a a Zs co 7 AE es ~ ee \ An = >< ee = — PEACENTACE OF CCCURRENCE CF WIND O[AECTICN FCA 200 FecT LEVEL BieB- 1559. | ™~. RADIAN CORPORATION 7S. PERCENTAGE GF GCCURRENCE CF WIND OLRECTICN FOR 100 FCCT LEVEL IT B-1538 | RADIAN CORPORATION i - 50 e NS ¢ ; tas p ; \ : j FS, \ i \ i \ i ( ; } ‘ j { HW Es ~ | { \ \ f j 9 \ \ / J \ \ fi \ ‘ oN a \ : - ‘ ‘ as ed a Ne / . os -" x an we ne te Tee ae je es - ~ aA PEACENTACE OF CCCURRENCE CF WIND O[RECTICN FCA 200 FOOT LEVEL TT B-1539 “Ye THIS PAGE LEFT BLANK INTENTIONALLY ) II B-1540, | DCN 77-100-152-04 AIR MONITORING REPORT FOR G-b. SHALE. OLL; PROJECT MAY 1977 Report No. 33 22 July 1977 Presented to: G=b ‘Shale Oils Project United Bank Tower Denver, Colorado 80202 Prepared by: Radian Staff LE B=1541 RADIAN CORPORATION TABLE OF CONTENTS I. GENERAL DESCRIPTION OF AIR MONITORING PROGRAM------ II. DESCRIPTION OF INSTRUMENT SYSTEMS------------------ A. Air Quality Instrumentation-------------------- B. Calibration Procedures------------------------- C. Data Acquisition System------------------------ D. Meteorological Instrumentation----------------- III. MICROMETEOROLOGICAL AND TERRAIN FEATURES----------- IV. OPERATING TIME ANALYSIS FOR EACH SITE-------------- V. MONTHLY METEOROLOGICAL SUMMARY- ------------- ase A. Summary of the Meteorological Conditions over North America during May 1977------------------ B. Summary of the Meteorological Conditions in Northwestern and West Central Colorado during May 1977--------------------------------------- C. Summary of the Meteorological Conditions in the Oil Shale Tract C-b Region during May 1977--------------------------------------- VI. DATA PRESENTATION AND SUMMARY---------------------- IIT B-154? Page zi B-2550 = 1570 RADIAN CORPORATION TABLE E TABLE If TABLE LT LIST OF TABLES DOWNTIME HOURS FOR C-b SHALE OIL PROJECT Site 023------------------------------------ Site 023------------------------------------ Site 023------------------------------------ FEDERAL AND COLORADO STANDARDS -------------- AVERAGES FOR MAY 1 THRU 31 Nitrogen Oxides (NO) - Ss ee ins lp pe eee Nitric Oxide (NO) --------------------------- Nitrogen Dioxide (NO,)---------------------- Sulfur Dioxide (S0.2)------------------------ Pyranometer--------------------------------- Sulfur Dioxide (SO,)------------------------ Total Hydrocarbons-------------------------- Methane-------------------~--~----~----.----- Non-Methane Hydrocarbons-------------------- Carbon, Monose Ges ——+- === —- = aoe ee cone cee Barometric Pressure------------------------- Total Precipitation------------------------- PD ears te oa ee ae Wind Speed---------------------------------- Wind, DimecELon === ————2—— ae ee ee Relative Humidity--------------------------- Temperature--------------------------------- i B54 3 Page RADIAN CORPORATION LIST OF TABLES (conmed) Page TABLE IV DAILY AVERAGES FOR MAY 1 THRU 31 Nitrogen Oxides (NO) 2 --- = --- eG II B-1588 Nitric Oxide (NO) --------------------------- -1588 Nitrogen Dioxide (NO2)---------------------- -1588 Sulfur Dioxide (S0,)------------------------ AalS89 Pyranometer----- aad ad alla alata a a .~1589 Sulfus Di oxtaew (sO, jee se==— 2-2" — = eee -1589 Total Hydrocarbons-------------------------- -1590 Methane---------------------~---------------- -1590 Non-Methane Hydrocarbons -------------------- -1590 Carbon Monoxide----------+------------------- = 15911 Ozone ~ <= = +n ee ee He He He ee ee =1591 Barometric Pressure-~---+---------------------- “1591 Total Precipitation------------------------- -1592 Particulate--------------------------------- -1592 Wind Speed-~------ wn ee nnn -1593 Wind Direction------------------------------ ~1594 Temp erature----~+--<+------------------------- -1595 TABLE V MAXIMUM FIVE-MINUTE AVERAGES AND TIME OF OCCURRENCE FOR MAY 1 THRU 31 Nitvogen Oxides: (NO ja—sa-orsesa sees -1597 Nitric Oxide (NO) --------------------------- =1598 Nitrogen Dioxide (NO; )---------<------------- =1599 Sulfur Dioxide (S0,)------------------------ - 1600 Pyranometer--------------------------------- -1601 Sulfur Dioxide (S0O,)--+----------------------- -1602 Total Hydrocarbons-~--~----------------------- -1603 Methane- ------------------------------------ -1604 Non-Methane Hydrocarbons-------------------- -1605 Carbon Monoxide----------------------------- - 1606 OZONE ~ ~~ - ee we en nn ee en eee -1607@ Barometric Pressure----------------------~--- -1608 PT B-1544 ’ RADIAN CORPORATION EEST OF TABLES. Ceontd) Page TABLE V (contd) TABLE* VI TABLE VEL Total Precipitation------------------------- II B-1609 Wind Speed - Wind Direction----------------- -1610 Temperature- ------------- - eo ee ee rn eee -1611 THE FIVE MAXIMUM INDEPENDENT SLIDING AVERAGES EOR MAY-i- THRU" 31 Nitrogen Oxides----------------------------- -1613 Nitric Oxide-------------------------------- -1613 Nitrogen Dioxide---------------------------- -1613 Sulfur Dioxide------------------------------ -1614 Total Hydrocarbons -------------------------- -1615 Methane------------------------------------- -1616 Non-Methane Hydrocarbons-------------------- Sao Ly Carbon Monoxide----------------------------- =1618 Carbon Monoxide- 8-hour-------------------- = -1619 Ozone--------------------------------------- -1620 Particulate--------------------------------- -1621 FUNCTIONAL DEPENDENCE OF RECORDED PARAMETERS UPON WIND DIRECTION Nitrogen Oxides (NO,)--==------------------- - 1623 Nitric Oxide----~---------------------------- -1624 Nitrogen Dioxide (NO,)---------------------- -1625 Sulfur Dioxide (S0O,)------------------------ - 1626 Sulfur Dioxide (S0O.,)------------------------ -1627 Total Hydrocarbons -------------------------- -1628 Methane-- ------------------~---------------- -1629 Non-Methane Hydrocarbons-------------------- -1630 Caron Monoxide------------------------------ -1631 Ozone- -------------------------------------- -1632 ie B>rSa5 RADIAN CORPORATION ErEsTt OF TABLES €contd) Page TABLE VELL DIURNAL VARIATION OF VARIOUS RECORDED PARAMETERS Nitrogen Oxides----------+-------------------- II B-1634 Nitric Oxide-------------------------------- -~1635 Nitrogen Dioxide---------------------------- - 1636 Sulfur Dioxide-~----------------------------- -1637 Total Hydrocarbons-~-------------------+----- - 1639 Methane-------- ee eee ee ee eee ee + -1640 Non-Methane Hydrocarbons - --~------------+------ -1641 Carbon Monoxide-------------+------+--------- -1642 Ozone=- ~--~------ + -- ee ee ee ee =e - 1643 Precipitation--------------------+---------- ~1644 Wind Speed 8 feet---~--------------------------- -1645 30 feet----------~-------------------- ~1646 100 feet-~---------------~-------------- ~1647 200 feet------------------~-------------- -~1648 Wind Direction 8 feet-------+--~----------------~--- -1649 30 feet-~-~~--~~-~----------<----+------ -1650 100 feet---------------+-- 24 -- 2 eee ee -1651 200 feet~~---~----~---------------~-~-+-+-- -1652 Wind Direction Standard Deviation 8 feet------+--------~--~----+-------+-- -1653 30 feet----------~-- wee ee ee ee ee eee . 1654 100 feet--------------------~---------- -1655 200 feet----~-----------------~--~----- -1656 Horizontal Wind Direction Standard Deviation at 200 feet------------~----------- -1657 Temperature 8 feet---------------------~---------- -1658 30 feet--~-----~------------~---------- ~1659 100 feet-------~------------------------ -1660 200 feet------------------------+------- -1661 Il B-1546 RADIAN CORPORATION LIST OF TABLES jCeont¢) Solar Radiation---------------------------- Temperature Change from 30' to 100'-------- Temperature Change from 30° to 200°-------- Barometric Pressure------------------------ Horizontal Bi-Vane Wind Direction at Vertical Bi-Vane Wind Direction at 200 feet----------------------------------- Nttnecen. Oxides =—--= s- == — ee ean ss Nitric Oxide------------------ 9-9-9 Nitrogen Dioxida=<<=<<<--=<--s5-==--2--===5- Sulfur Dioxide----------------------------- Non-Methane Hydrocarbons------------------- Carbon Monoxide-- -------------------------- Wind Direction at 8 feet------------------- 30 foette os 242-e5-—4—-=---- Temperature at 8 feet------ Saelwesee =e =a 210). Geshe 100° feet===-——-=-=-—---.—-=-----< 200° feet=—o<= ee e= ee = === === Barometric Pressure------------------------ it B-1547 Page RADIAN CORPORATION LiSt OF TABLES Ceontd) Page Solar Radiation----------------------------- i (B1692 Horizontal Bi-Vane Wind Direction at 200-feet--------------------------------- =1693 Stability Class Determination Using Pyranometer Recording--------~-------------- -1694 Stability Class Determination Using DT/DZ (Level 1)----------------------------- -1695 Stability Class Determination Using DT/DZ (Level 2)----------------------------- -1708 APPENDIX A - STABILITY WIND ROSE DIAGRAMS ---------------- -1721 8-foot level - Stability Class A------------ ~1725 Class B------------ -1726 Class C------------ =e) Class D------------ -1728 Class E------------ 729 Total-------------- -1730 30-foot level - Stability Class A----------- =1/ 5" Class B------------ -1732 Class C------------ 1753 Class D------------ -1734 Class E---~--------- 1735 . Total------ ~------- 1736 1l00-foot level - Stability Class A---------- -1737 Class B------------ “1/33 Class C------------ -1739 Class D------------ -1740 Class E------------ -1741 Total-------------- -1742 200-foot level - Stability Class A---------- -1743 Class B------------ -1744 Class C------------ -1745 Class D---~-------- -1746 Class E------------ SAT II B-1548 Total-------------- -1748 € RADIAN CORPORATION LIST OF TABLES (contd) Percentage for 8-foot 30-foot 100-foot 200-foot Page of Occurrence of Wind Direction disyeiehoee -eteeeneets nest -- II B-1749 | QVGl- 225- = S== SS e ar -1750 heweNl Jaa oe Foe Se =1751 lidvel- 322=- =4=-=- there are: wind speed, wind direction, and temperature and relative humidity sensors in a power-aspirated radiation shield. Temperature difference thermistors (also in power-aspirated radiation shields) and their associated circuitry take lapse rate measure- ments for the 30-foot to 100-foot layer and the 30-foot to 200-foot layer>itIn addition, this):site ihas: alRrectsion sSpectral Pyranometer, a barometer, and a tipping bucket rain/snow gage. The wind direction and speed apparatus used at each measurement level of the tower is the Model 1074-2 wind sensor by Meteorological Research, Inc. (MRI). This sensor has a 540° potentiometer for wind direction and a light chopper for wind speed. This sensor is rugged, with an all-weather coaxial cup and damped vane assembly. The prototype model has been in operation for years under the most demanding weather conditions, performing continuously with the utmost reliability. The wind sensors on the tower have been specially treated with a black paint which will promote warming of the exposed surfaces of the sensor and thereby reduce ice and snow accumulations on the moving parts of the apparatus. The specifications on the Model 1074-2 are as follows: hipb=1556 RADIAN CORPORATION Wind Speed Starting “Threshold: Response Distance: Flow Coefficient: Accuracy: Wind Direction Starting Threshold: Delay Distance: Damping Katio: ~ 0.5 Accuracy (540° system) : Range: O° to 540°. O27 > mph. NS "feet (637 recovery). 7.9 feet/Revolution. +0.4 mph or 1% (whichever is greatest) 0.75 mph. 4 feet (50% recovery). to 0.6. = The relative humidity and temperature sensors are mounted within a power-aspirated radiation shield at each tower level. by. MRI. maximum radiation protection to the sensor. dtawn imtoo the shreld and across This imeake from a hemispherical space which 15 feet per second. from the tube opening. Speed of perhiphery of this hemisphere is The temperature sensor and resistor network. change with an air temperature change. All aspirators and sensors are of the Model 840 Series The aspirated shielded housing is designed to provide Ambient air is the sensors at approximately air is essentially sampled is approximately 3-inch radius the incoming air at the approximately 1 mph. is comprised of a dual thermistor This circuit provides a linear resistance The relative humidity sensor is placed alongside the temperature elements inside the Shiela where Me is exposed to a constant flow'of air. Circulation to both sides of the sensing element produces accurate monitoring with a good response time. ments are as £L£ollows.: The specifications on the sensing ele- Li Beaso/ RADIAN CORPORATION Temperature Aecuracy:. £0 .25°'C. Range: -50°C to +50°C. Humidity Accuracy: =23.0%— RH. Range: 0% to 100% Relative Humidity. Measurements of temperature difference are taken for two layers, the 30-foot to 100-foot and the 30-foot to 200-foot layer. The thermistors and circuitry used for these measurements are separate from the thermistors measuring air temperature. The use of separate thermistors and circuitry to measure AT allows for much greater accuracy and resolution in the measurements, which is necessary for stability assessments. ' Two AT thermistors are at the 30-foot level, one is at the 100-foot level, and one is at the 200-foot level. All of these AT thermistors are mounted within power-aspirated radiation shields. The specifications on the AT instrumentation are as. follows: Accuracy: £0: AC. Range of AT Circuit (Lower Level-Upper Level): +9F° to -9F°. All instrumentation, except at the ground level, is mounted at the end of 12-foot retractable booms. These booms are 3-inch box beams which are on rollers: and can be retracted to the instrument platforms for instrument maintenance. The meteorological tower itself is a 200-foot Rohn Model 80 Guyed Tower, designed for 40 pounds per square foot wind load with %"' of radial ice per EIA Standard RS-222-B, to Tl B-1558 RADIAN CORPORATION support four levels of meteorological equipment. The material consists of tower sections with a tapered base, three retractable booms 12-feet long, three outside work platforms, an inside ladder for climbing, two base ground kits and one anchor ground kit. The cable-type Safety Climbing Device consists of a cable and attachment mechanisms with a locking sleeve and safety belt. The tower is lighted and painted according to FAA specifications. The signals from the tower instrumentation are fed from multiple signal cables into transmitters mounted at the base of the tower. After signals have been converted to analog Sienals tthe, are “ted aimto a ijunction ‘box; calsio at cthe tower base, where they are assimilated into one coaxial cable. The Signals are then rum underground within 3" -PV@ ‘conduit %to the A-to-D assembly, where they are processed. The transmitters are shielded and insulated from the elements. The signal cable is run underground in PVC conduit in order to minimize damage from the weather or from various rodents in the region. The auxiliary equipment at the tower site consists of a heated tipping bucket rain/snow gage, an analog barometer, and a Precision Spectral Pyranometer. The rain/snow gage is the Model P511-E unit by Weather Measure. In the case of this gage, the durability and reliability of a tipping bucket gage are combined with heavy-duty electric heaters to make this an all- purpose precipitation sensor. This gage may be used to measure both snowtaid rand: rainiail 7 iAntnsulating ccovexr iof ipoly=viny lh ichilorade and a thermostatic control insure the proper gage temperature. The thermostatic control is adjustable from 0 to 25| JG.f s2Snow falling into the inlet tunnel is melted. . The resulting water (from rain or snow) drains into a precision tipping bucket mechanism which activates a mercury switch each time the bucket fi bis Gand teiqs 479 ihe (cage: is fcomstructed ofrdurable corrosion- resistant materials to provide many years of service. The Tt B-1559 RADIAN CORPORATION speciiications for Chis gage ane as follows: Orifice e968) imehes- Calibration. 0 etnies. Accuracy: 0.5/<¢Galtbprated at 70e5. in) ni) Sensor: Chrome-plated tipping buckets. Switch: Mercury, 0.1-second closure. Heat Control: Thermostat adjustment, O to 25 C2 The barometer is the B242 Analog Output Barometer by Weather Measure. This barometer provides an output voltage that is linearly proportional to pressure! >the specifications on) this instrument, which is mounted inside the monitoring trailer at the Site, ‘are as follows: Range: Specially designed for the 100 millibar interval from 725 millibars: to 625 melivbars. Resolution: Infinite. , Linearity. 20.75 milliban. over the: {00 smi llabar interval: The pyranometer at the site is the Eppley Precision Spectral Pyranometer. This instrument is used for the measure- ment of sun and sky radiation totally or in defined wavelength bands. The pyranometer is levelled and mounted atop a wooden stand 4% feet from the ground surface. Care has been taken to eliminate the effects from all outside influences, such as reflection or shadows, on the pyranometer. The instrument characteristics are as follows: SENS sel vast ic 2D TV) Spek cal/cm®/min. Independence: 300 ohms. Temperature dependence: Sensitivity constant to within +l percent over the ambient temperature range from -20 to +40°C. PES B=1560 RADIAN CORPORATION LinearLty = Response linear-up to intensities of°4 call/em* /min- Response time: 1 second (i/e signal). Atlleinstrumentation is™factory-calibrated andjiissfield- Calibrated ae varrous intervals. “Slings psychrometers are sed’ to calibrate the humidity sensors; known temperatures and/or resis- tances are used to calibrate the thermistors; and an rpm cali- brating unit is used to calibrate the anemometers. The wind direction instrumentation is aligned to true north (reference direction) by means of a surveyor's transit. Jie) igiie Rae Xo RADIAM CORPORATION Let: MICROMETEOROLOGICAL AND TERRAIN FEATURES The Pieceance, Creek Valley andjG-=p Shate Oil” Tract are situated such that many microscale meteorological phenomena affect thesregion where,the,ambient.air monitoring. unit is Located. Trailer 023 and its associated 200-foot meteorological tower are located atop a plateau to the south of the valley, high enough to be affected mostly by gradient flow conditions. The elevation at the meteorological tower site (Trailer 023) is 6940 feet above sea level. The largest gradients in eleva- tion in this area, of course, occur at the Piceance Creek Valley walls. However, the northern valley walls are slightly steeper than those at the southern boundary of the valley, which then slopes upward gradually toward the C-b Tract. The Piceance Creek Valley decreases in elevation from east to west in this area, so that nighttime katabatic cold-air drainage flows advect from east CO West. Site 023 is approximately 2.5 miles south of the Piceance Creek Valley. This location is relatively high com- pared to its surroundings, with the nearest point having an eleva- tion greater than 7000 feet being .5 miles to the south of the tower. The tower itself is on the top of a small knoll located between Scandard and Sorghum Gulches. Because of its location and the irregularities of the surrounding terrain, meteorological patterns are varied here. Wind instrumentation is mounted.at four levels of the meteorological tower: 8 feet, 30 feet, 100 feet, and 200 feet. The top level of the tower generally remains in gradient wind flow. That is, the winds at that level are normally generated II B-1562 RADIAN CORPORATION by synoptic-scale features and are usually separated from terrain features: and=mierometeorological circulations.” Occasionally, a weak anabatic flow influence is experienced. However, such is not the case with the three lowest measurement levels. To varying degrees, these levels are influenced by both the katabatic and anabatic circulation cells. However, when strong pressure gradient forces exist in the region and the synoptic-scale wind flow is strong, all four tower levels will reflect a gradient wind flow as the winds increase in strength and height. The terrain atop the plateau is generally barren and fairly rugged, with a few scattered small trees. The topsoil dries rapidly and is very fine, resulting in blowing dust when dry, windy conditions exist. In the Piceance Creek Valley, the terrain is fairly grassy and flat, with steep valley walls on either side. Surface winds are normally rather light in this valley unless channeling effects occur. During clear nights with rather light pressure gradient- induced winds, rapid radiational cooling will occur’in the region because of the barren nature of the terrain and the generally dry ‘character of the air in this portiom of the country... As a result, the diurnal range of temperatures will be extremely large. Because of the katabatic flow in the valley, nighttime temperatures will generally be lower in the valley than on the plateau. During the winter, especially, temperatures in the valley may be 20F° lower than they are on the plateau during the early morning hours. Ely B=563 RADIOS CORPORATION Ns OPERATING TIME ANALYSIS FOR EACH SITE This section presents the operating statistics for each of the major subsystems contained in the monitoring station. Table I shows the specific number of hours that each of these subsystems were inoperative for the month. The colum labeled "DIGITIZING SYSTEM' indicates the entire data acquisition system; therefore, downtime hours appearing in this column means total loss of data. These instances: include, in taddition to computer downtime, power failures, no power available, and self-automated shutdown periods such as during air conditioner malfunctions. Calibration time is not considered to be downtime and is, therefore, not included in the downtime figures. The amount of time used in calibrating the instruments is given at the bottom of the downtime analysis table and is reported as total calibration hours for each channel for the entire month.* As is evident in the calibration figures, channels can be calibrated independently of one another. No calibration time is given for particulate monitoring since Hi-Vol calibration occurs infre- quently and only during the off-duty cycle for each Hi-Vol while another Hi-Vol is taking data. 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"he Os *0 ay nie i, ce ‘ oe *0) °0 ais 0 ne 20 aaee 0 e bd 8 e ® ® : 6 Vf °9 ‘ a) ne =O sh 0 igs au ‘ S, oe “ *9 oF ° 2 4 "0 Sa Hy *6 s *0 s *0 e 0 *h 0 “9 *he ‘ *o é *n2 "6 sa A 27S *0 aU °0 give a) in - aes a *0 "0 *n2 ” iis ew a0) *0 *n2 “he *h2 “te “te ~* te "Oe =." 02 "te + ° te “te * Ire “pe tre LW aareleak was) 1 Pp i te on° iz "Hie She “te w° tid “te. 2 cine * Wie: te ne “the + tre “te “te "We atte “Wie eae “Ne whe "2 aoe oie othe * tie ~~ te “fe he ico aie “j2. “he "ne = "he “te «86 “he tie” “tre “wie tie “G2 “Pie ne We TOMA TQMH NOMWUudd2023 eae ora > RADIAN CORPORATION V. MONTHLY METEOROLOGICAL SUMMARY A. Summary of the Meteorological Conditions over North America during May 1977 May 1977 brought warmer than normal temperatures to most of the continental United States. Precipitation totals were below normal over most of the country except for the Rockies and western sections of the country. The long wave circulatory pattern for May featured a trough in the western United States and a ridge in the eastern United States. The mean long wave trough was responsible for the slightly below normal temperatures and much above normal precipitation totals that occurred in the western United States. The mean long wave ridge accounted for the below normal precipitation totals and generally above normal temperatures which affected the eastern United States during May. The long wave circulation was meridional (north-south) on all days during May except from the 26th through the 29th when -Lt was..split flow, Extratropical low pressure systems were frequent in the United States during May. These low pressure systems usually affected the northern half of the country. The dates and locations of these low pressure systems were as follows: 4th: Northern Great Plains ath: Northern Great Lakes 6th: Great Basin 8th-9th: New England LOths Upper New England l2th-L3th: Southwest L3th: Upper New England Lhe Great Plains hie B- 1568 RADIAN CORPORATION 16th: Great Basin 2isit-22nd.sGreat Plains 23rd: Pacific Northwest 24€h,- Great Basin On a sectional basis, the following temperature and precipitation anomalies existed during May. Section Temperature | Precipitation Northeast Much above normal Below normal Atlantic Seaboard Above normal Below normal North Central Much above normal Below normal Central Above normal Below normal Southeast Near normal Variable Southwest Near normal Variable; mostly below normal Rockies Slightly above Variable normal West and Pacific Slightly below Variable; mostly Northwest normal much above normal lie B= 1569 RADIA CORPORATION B. Summary of the Meteorological Conditions in Northwestern and West Central Colorado during May 1977 Grand Junction, Colorado, sixty miles to the south- southwest of the Tract (C=b, secerved a ftotal.of 0.59; inch of precipitation during May, which is 0.04 inch below the monthly normal of 0.63 inch. Measurable precipitation occurred on the 10th; ‘L3thyJeeh, 15th, and the 26th. (The region ~ceceived 70 percent of the possible monthly sunshine. Sky cover by cloudiness averaged 5.2 out of a possible 10 during the daylight hours and 5.2 out of a possible 10 during the entire month. The region had eleven clear days, eleven partly cloudy days, and nine cloudy days during the month. Air mass changes were frequent during May. Seven frontal passages occurred during the month. These frontal Passages occurred regularly as an upper-level trough dominated the western United States throughout the month. Transport winds over the region as a whole were stronger in May than in April. Maritime polar cold frontal passages occurred on the 4th, 7th, 9th, 14th, 16th, 20th, and the 24th. TE B= 1570 i SA Daa CORPORATION C. Summary of the Meteorological Conditions in the Oil Shale Tract C-b Region during May 1977 An upper-level trough which had a mean position over the western United States was responsible for the relatively frequent passage of cold fronts through the Tract C-b area during Mayen Precipatationvoceurred om the 13th, 14th, 15th, and 26th of May. Temperatures in the Tract C-b region were slightly above normal during May. Seven cold frontal passages occurred during May. Maritime polar cold. frontal passages occurred on the 4th, Jtbes then Lath /othy. 20th, and. the, 24th.. The monthly average temperatures recorded at the meteorological tower during May were 47.8°F at 8 feet; 49.4°F atg0) feet. .401 7k at 100 feet, and 48.2°F at 200 feet. These averages are somewhat misleading since temperature data was obtained only during the first nineteen days of May. No tempera- ture data was available for the last twelve days of the month. These averages are approximately 6F° higher than those recorded in April. The averages would have been higher had the last twelve days of May been included. The warmest days of the month were the 6th through the 9th and the 12th. The coolest days were the 14th and the 18th. The highest temperature recorded at the meteorological tower during May was 73°F at the 8- and 30-foot levels on the 9th. The coldest temperature recorded at the meteorological tower was 25°F at the 8-foot level on the morning ofthe 19th. No relative humidity data was obtained during May since the sensors were removed in early May due to faulty data problems. Wind speeds on the meteorological tower during May were much stronger on the average than the winds that prevailed during April. Resultant wind vectors at the meteorological tower during ie B= 57/1 eA DIA dd CORPORATION May were as follows: 207.4 degrees at 5.2 miles per hour at 8 feet;-200.8 degrees at 629 miles per Hour at 30 feet; 199.2 degrees at 7.9 miles per hour at 100 feet; and 208.5 degrees at 8.7 miles per hour at 200 feet. The scalar average wind speeds associated with these resultant wind vectors were 7, 10,-22>- and 13 miles per hour; respectively. The Ekman spiral and Ekman effect, i.e., a veering in direction and increase in speed as a function of increasing height above the surface, were in evidence during most of May. A reference to the May wind rose for the meteorological tower indicates that the winds at that location were primarily south- southwesterly with a high occurrence of southwesterly and southerly winds in addition. The windiest days of the month at the meteorological tower were the 3rd, Sth;*6th;” Poth? 23rd) and the.24en. 3" The : days having the lightest winds were the 13th, 19th, 20th, 21st, 27th, 30th, and 3lst. The highest five-minute average wind speed recorded at the tower during May was 48 miles per hour at the 200-foot level on the 16th. Precipitation totals in the Tract C-b Monitoring Net- work during May were generally slightly below normal. Precipitation occurrences were less numerous during May than during April. Only 0.36 inch of precipitation was recorded at the meteorological tower during May. The largest daily precipitation total recorded in the network during May was 0.20 inch on May 15th. The greatest five-minute precipitation total recorded during the month was 0.04 inch (a precipitation rate of 0.48 inch/hour), re- corded on the 13th and the 15th. Measurable precipitation (>.01 inch) was recorded at the meteorological tower on the 13th, 14th, I3th, and the -26th.°’’ The precipitation on’ ‘the/morming of the’ 14th Pe Bal SZ RADIAN CORPORATION was im thes form of snow. All other precipitation occurrences were im the Eoum Of Laimtall, The monthly average station pressure during May was 786.1 millibars at the meteorological tower. This reading is 3.2 millibars lower than the April average station pressure of 789.3 millibars. The highest daily average station pressure occurred on the 2nd, -30th,;*and the *3Sist.~ The lowest daily average. Station. pressures, occurred on'*the oth, 6th, and the “16th. Cloudiness increased in the Tract C-b region during May, compared to the April cloud cover and insolation statistics. Tne region received an insolation total of 16,221.1 langleys, which is equivalent to a daily average insolation total of 523 langleys/day. This average is below the normal for May of 580 langleys/day in the Tract C-b region. On a diurnal basis, the greatest solar radiation rates occurred between 1100 and 1200 hours. The greatest daily radiation totals were received on the igen. 29th, 30th, and the Sist. =The“lowest daily“-sollar radiation totals were received on the st, 3rd;"the 13th“through the Ld5th, and the 26th through the 28th. The greatest five-minute radiation total received during May was 8.60 langleys (a rate of 1.72 langleys/minute) , which occurred on the 21st. The largest hourly insolation total received during May was 88 langleys, which occurred on the 29th between 1200 and 1300 hours. Because of the progressively increasing solar elevations and the increasingly longer periods of daylight that prevailed during May, the total possible solar radiation which could be received during a day increased monotonically throughout the month. Therefore, even though cloudiness increased during May compared to April, the actual” amount’ of solar radiation received also increased. LeBow S/S RADIAN CORPORATION The increase in cloudiness which affected the Tract C-b during May caused the “very unstable” ‘stability ‘classes to become much less common than they had been in April. Using the Pasquill method of stability determination, ""D" sitabila ty, (neutral stability) was the most common stability, occurring during 284 daytime hours, or 66.8 percent of the time. In de- creasing order of frequency, "Cn Cslacghtly unstable) «stability occurred during 98 hours, or 23.1 percent of the time, and "B"” (very unstable) stability occurred during 43 hours, or 10.1 percent of the time.-"A” (extremely umstable)2stabality did not occur during May. Using the lapse rate method of stability determination (BS). the neutral ("D"), slightly stable ("E"), and very wnstable ("B'') stability classes were the most prevalent during May. In general, stable and/or neutral conditions prevailed during the nighttime hours and unstable and/or neutral conditions prevailed during the day. The following table is a diurnal breakdown of the various. stability classes. As one proceeds, from 7A’ tol Fk", the stability class ranges from extremely unstable to extremely stable. The column labeled "number of occurrences" indicates the number of times a particular stability class occurred during the month on an hourly basis. Level I presents the temperature change versus height values (D that were considered between 30 feet and 100 feet. Level II indicates the values that were considered between 30 feet and 200 feet. Using the standard deviation of the horizontal wind (o,) method of stability determination, "E"'" stability was the most common stability classification at the 30-, 100-, and 200-foot levels of the meteorological tower due to moderately strong winds at those levels. The "D" stability was the most common stability classification at the 8-foot level due to a higher degree of mechanical turbulence at that level. PY B=1574 RADIAN CORPORATION n 4 @ oO to) c c (oy Y Gi fa Ne} A) Prete Or, CO Wi fy NOP MON ~ ell 2ST) OS) oO A Or en SS) ONO Ow ON OER os G9 Is 3 N =) N . OU 7 U ge) ous ZS ZO ~wt et oti NS eye te ~— rt) rsa COO! et) N N ~~ Seas SE TNO) BA It (a) SP NE Esl, LES hr) N N N SRN, eit NO} NO cr) N ot OOOM™N~ OO N N rd Sic Cet sr Oy < Lan eb IC Le ti NN N oO Ho Onn AN © ee) “uN Con IM N N an Om, NO) eee |S oO Sr ie <7} _ Coal fea) eee CNP Oo) oS oe) re ©) om ss 5 u ei ee J re eo fab) reD) job) ™~ SO NFO Ko Snio© QO =~ SO) NE eS sO Ge 4 rm | ao © Ne} OMe IN 1) WS OS an) ON et wn os Soe Nass EOS “~~ rei Oye CO IN 1 OM IE=) uIU Ww (=) CN ION: Oe rst FO) i) SZ) © QUINT iStaeet 1S ce ci Loma! ri HH KH ei | fon) ON ae On) F Ge FC Cy fon) ON sar Ca 1S) Se) fz} tm J rc > ic iam @ Pe NOS SSS |S - 6 Oo WwW ft !Y © =; A ol ~ ND “Fo mS Oo La. GSN ~ N wv wy Ne} N we GO N © oO ee oe amg ee w ao oOo N CO ES wy oH MO AHN @D J NE oS eS oy if em NS OP ort oy YU re Copy. cet ts) et (Sr ON at COS Q es Y (aa) qn Oo OO BW ec 98 OdUrei y+ am ma N ON aN Oy) 36) KO" NS nN UO ws as N NN FN &™ Geo Ww GS + Gon vot WW ed Oo IN Vet .o- 6G Cos) 0) er QF 0 & eS Aw may Lon ©? oo) aa Verna Vv Ww ESwvauvreée My ss) Ore -eter eG = ° bw Pm OO YW OD bk o joe PMA DH o5] ~ ~x Voi dren ~ Py Ydruardnuon vg Py wW wv aH Hd mew ee ee ee ee ee ee ee ¢e ¢e e6 ce ee oan ee ec ee ee ee HA Ca Ee es =< ROA RIE wd <1 eay Oc ard Qo © 8 0 tJ uw ioe) isp) EP sB= 8575 32 4 3 00-0 0-0 0-0 0 @ 0 0 2 1 L200). 0 De dis A DD RADIAN CORPORATION The bivane at the 200-foot level of the meteorological tower indicated a pattern of upward vertical motion (negative vertical directions) during May. Upward vertical motion was more pronounced during the daytime hours at the 200-foot level. Upward vertical motions were less pronounced at the 200-foot level during the late night and early morning hours. The bivanes at the 30- and 100-foot levels were removed in late March due to instrumentation problems. The Cg value obtained at the 200-foot level using the bivane compared favorably with the Cg value obtained at that level using the standard wind instrumentation. PEVB-1576 RADIAN CORPORATION VES DATA PRESENTATION AND SUMMARY This section includes summaries for various recorded data at the monitoring sites. The data presentations indicate the variability of pollutant concentrations and meteorological parameters with location and time. In addition, the presenta- tions indicate the functional dependence of pollutant concentra- tioni withiwindwdirectionepyAlk data-except suspended particulates (24-hour samples) are sampled once each second, but recorded as five-minute arithmetic averages of the one-second samples. This averaging technique tends to smooth instantaneous maximum values, and is especially evident when comparing wind gusts to local weather bureau data. Inherent to any data acquisition system is random noise both from the recording instruments and quantization in the ana- log-to-digital conversion. The lower threshold for all analytical . instruments is twice the maximum noise level generated by the instruments. , This lower threshold 2s, 5 ppb for all, instruments’, except tor the ozone analyzer, for wiacitatws O25-ppb7-~ There= fore, any values appearing in the data presentations that are less than 5 ppb indicate only a trace of pollutant in question and should not: be construed to be absolute levels. In addition, the recorded quantity is simply random noise and averages tend toward zero. Thus, when concentrations are below the lower threshold of the analytical instruments they may appear as a zero entry in the data presentation which does not indicate absolute zero concentration. All pollutant data “(exceps tor “particulate “data) is taken” at the monitoring site in ‘integer parts per billion (ppb) but is presented here in micrograms per cubic meter (ug/m?) TT B-1577 RADIAN CORPORATION assuming standard temperature and pressure of 25°C and 760 mmHg (1013.2: millibars), respectively. @ Uihevscales Lactose eaiesed to convert ug/m*® at standard conditions back to ppb for the various pollutants: are given invthe following table. TO CONVERT tie/m- AT 25-¢ POLLUTANT AND 760 mmHg TO ppb MULTIPLY BY 934 234 234 384 a2) Ik 3)0 i230 Ole Been by The units of the meteorological parameters are given in the table. It should be noted here that inside temperature is monitored and recorded as a functional part of the system but is not presented in this report. Table III displays the monthly statistics for each monitoring station for the month. Topansure statastical sis- nificance, and to reduce the possibility of introducing a bias in the presentation, averages are computed only when at least 50 percent of the samples are present, except for relative humidity: and temperature, in.which, case. 75 percent of the samples are required. If less than the required samples are present for a particular parameter, that entry will be blank. The number of II B-1578 RADIAN CORPORATICN Samples pmeesent for a particular channel.is defined as the total possible number of five-minute samples for the averaging time less the computer downtime less the channel downtime less the channel calibration time. ~The averaces an TablevbilLsare.agith- metic averages with the following exceptions: - Wind speed and wind direction are computed using a vector averaging technique where the wind speed is treated as the vector magnitude. e Particulate averages are computed as the geometric mean. Table, IV. displays the daily averages:*Again,: 50 percent of the five-minute samples are required in order to compute an average except for the cases of relative humidity and temperature whiecherequire /5 percent. A blank “entry indicates anVinsulincient number of five-minute samples present for that day. Wind speed, wind direction, and particulate averages are computed the same Wavyeesradeseribed im Table Ltr. Table V presents the maximum daily five-minute average retained in the data base as well as the time of occurrence. A five-minute maximum average is printed if any samples are present for that day. Therefore, the maximum five-minute average for a channel which experienced considerable downtime or calibration time during the day in question may be misrepresentative of the maximum. expected for that channel on that day. Table VI indicates the five largest averages for various averaging times. The table shows the period of time covered by the average. Maxima are chosen so that time segments TP B=1579 RADIAT CORPCRATION are independent. The maximum averages reported are found using a "sliding average" technique! with the exception of the 24-hour particulate ‘average, ;which «is: computed from midnight, to midnient. For averaging times less than or equal to three hours, the slid- ing average is stepped one five-minute sample at a time. For longer averaging times the step size is twelve samples or one hour. For averaging times less than or equal to one hour 100 percent of the five-minute samples must be present to compute an average. Averaging times greater than one hour require 90 percent. Whether or not a sliding average is computed is solely determined by the number of samples present in that averaging time and is independent of daily and monthly averaging criteria. To demonstrate the functional dependence of recorded parameters upon wind direction, Table VII shows pollutant con- centration displayed in a bi-variate distribution with wind direction. The tables display the total number of five-minute samples occurring in each concentration and wind speed class. The mean concentration for all samples occurring in each wind class are also shown. This distribution demonstrates the dependence of high pollutant concentrations upon wind direction. Appendix A shows the stability wind rose diagrams. The wind speed classifications used in Appendix A are based on the Beaufort wind scale classification system. This is a system of estimating and reporting wind speeds, invented in the early nineteenth century by Admiral Beaufort of the British Navy. It.was originally based on the effects of various wind speeds on the amount of canvas that a full-rigged frigate of the period could carry, but has since been modified and modernized. In its present form for international meteorological use it equates: (a) Beaufort force (or Beaufort number); (b) wind speed; IZ, B- 1580 | ‘ RADIAN CORPORATION (c) descriptive terms; and (d) visible effects upon land objects or the sea surface. One land adaptation is the NRM wind scale. The six basic wind speed classifications used in the report are: = I=3 knots,.4-6 knots ;*7=10 knots, “11-16 knots’, 17-21 knots, and winds of greater than 21 knots. The following table is a complete description of the Beaufort Wind Scale, taken from Physical Climatology, by Helmut Landsberg, 1969. BEAUFORT WIND SCALE FOR OBSERVATIONS AT LAND STATIONS | PE we hee aoe i. aoe | Corresponding Limits of Wind Speed Force PBXs aCOEY Specification for Use 1 7 at 10 meters ab.grd. Title j | Bayh | oO Rrots' Ka/he! Misec. | Pc/sec | 0 CG aAtltintetonepemenecbsce cuerege [SINGS MESS Vee MI Ga 11 wr epeusieleis ae islet. a) ois) cheiers St oe GD UY MD 6m Os Ow OO ae US OD Gb a ON om SO 2b on Om am OS OD oe GD T’bat £° 126 @°Ssort 20 £20 £20 4311S SNOGYVIONGAH ANVHIAWN@NON INVHI SW SNOUGYVIONGAH Wil OS BS OO ah 8 DD @ 6 & os ed EF 66 oe OS ® ED OE OF OS OS OD Oe oe BS EOS > OP I On SO EO BOSE BSH HH ERS MHS SHREK SHEDS OOM MHD ODS M HME DSM MAHA MMSEKR ADRK EBDEAEHRB AMD Em ne T*t2291 1° F20 §20 gao°* ZL 1S C208) 90GIXOIQ yHn4a1ns YALAWONVAAd (208) 301x010 YNns ans 2 ae oe ot BO & 08 OOF oe me © OD Ot mm Oe 68 OD OR 8 > OD on oe ED OD Mm BD 0) OD SS OD OD OD ww HM OD oe OD Ot OD ED @ @ OF OF OF me OL 8 Om Gs OD OD GS OD a GS Ot ms Se GD OD GS Ge Oe ow Oe Gs OH OS oe of OS Ge oS Oo SR oe mm at ow Gy @) On © oe 88 ob ee i Oe Oe On iS te £20 £20 £20 311 (2ON) 301X010 NIASONLIN (ON) 3ULX0 JINIIN C(XON)SAGTXO NANONLIN (SFHINTSNOTIVITAIO9Nd fSHVHITVIVI We ANNSS3dd LSAFIINVT WLOL*4SLaWONYAAd fHLYON AHL OL LIO9FdSSN HLImM S4ARNDIGRNOTLISNIO ONIM SI) TSHNSMHVA SIZNDFU#INNLVAAdWIL SHNOH H3d SATIWRUF9IdS GNIM $NFLIW JDIAND Had SWVYSONIIW=SNOTLVYLNIINODISLINN) Te NHHI J AVW HOS SADVHFAV “TIT 3718vl aol * MOMWuOANOD isis vegies EV sara eae a j | ' { 4 ~ IT B-1586 2°St L°On f° oh er 20 (14-002) (14-001) (l4"0C ) (L4-98 ) L£¢0° STs VNLVeAdwal oo OP OD GR SP OD OE OH GD GD OD Gm OD OD Om ED Be om OD OS Om Om GD GH AD Om ED OD OO ab DN is Me Ae Si OO G8 OS 5 ED OS Om FD Et OF OD MD OF ot an ED BD Ot Go OS at RO 6D ees ON OD OM bn OE AD UD OS Od GL GD AD Gt GD OD Gm GD OD oe GE OS mo fms @2 OD OD on GO BS bt OD AY OD om uD Oc Gt OS a Do > oe Don Om C(id=00¢) (L4-001) (l4-0¢ ) (id“8 ) $20 311S ALITGIWAH FATLV14948 S*802 2°66T g°002 . 1° L402 (L14=002) (14-001) (i3-0¢ ) (lLi-8 ) £20 311 NOTLOAYNIA ANIM L°8 6°L 6°9 2°s (14-002) (14-001) (l4=0¢ ) (14-9 ) $20 311s d343dS (NIM (SSHINT@NOTLVITdI 994d IEHVATTIIN|@INNSSANd {SAFIONVI WLOl@4alAWONVYAd f{HLYON SHL OL LIAdS3M HLIM SISNDAG@NOTLOINIO UNIM ¢LIZHN3MHY4 SABNNIG“3NNLVYIdNIAL {YNOH Y3d SAIWW=d349dS GNIM fYALIW DIAND Y3d SWYYDNONIIW=SNOTLVYLNIINOIZSLINN) Te MUHL fF AVW HOS SAOVYFAV “TIT a1svi NOIMVWMNOAdUGI? a ~™ e- ao ia RADIAN CORPORATION TABLE IV DAILY AVERAGES FOR MAY 1 THRU 31 EL B= 1567 0° g° 0° TAS qo? o¢ u° 0£/S Ont OF 0° 62/5 2° vw S° 82/5 O° (a Gr L2KS O° 0° ag 92/5 Oe OF oO G2/S Q° gq? 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(SEte )0°802 0°2¢ (Onse JO*SOT 0°82 (SEib6 0°22 0°¢2 9 /S COTES) OR Te 0°S¢ (O0tET)IO*T02 0°S¢ (00°¢1)0°002 0°0¢ (S2%02)0°002 O*n2 S/S (OME9TIO*ST2 O° TS (Ont9oTt)o*Oot2 0°L2 (Stistjyo°ste 0°¢2 (0S2S1)0°022 O°st » 7S (SS29T)0°H9T OSS (SS29OT)O°LSI O° l {YNOH Y3d SIVWWd9adS GNIM fHYFILAW JINNI Y3d SWVYDNOYDIW=SNOTLVYLNAINOIESLINN) TE NYHL F AVW YO4 JINFYNNIIO 4O JWIL GNVY S3OVHSAV JAINNIW SATA WOWIXYHW PA J1AV4 =. NOUYWNOAROD a ‘ paces oan ae f aes ; Lf 4 ~» 4 RADIAN CORPORATION TABLE. VI THE FIVE MAXIMUM INDEPENDENT SLIDING AVERAGES FOR MAY 1 THRU 31 II B-1612 Ii B-1613 (fno02:0T)8° (S2:6t=Seret)e /S °S (oo2:8t)e°® (SEtSt=Stintye /S (664270). 2° 4 (Shrol=SniestdotssS °F (2028 OT) 2" 1 (O2thT=022Lt)8 /S °2 (2¢¢398 1¢°L COnset\eOnsLI6sS “tT £20 3LIS uNOH=T [OM %3§M) AGIXOIG NADONLIN etss Veo (SIEG =Stth B2e/S °S (LGOEsL Inert (OSiTt=0S:0T 82/5 °r (pESs6 3S°e2 CO2sutHO2tLT)OT/S °% [ Ge Ee oe OF OD > op Om OO GD as US MS OS Gs be 20 OF tt mb Gh Un OY GD om Be Ge ow wD OD We Gr Ut OD om ao ow a Oe GE OS OD KG OB ow ow Gm OH oe On 60s BO Ot GS ae OO oy OH aD Oe oe me $20 3LIS LV S3wIl 61 GIAASIXFI AuvaGnviS AYVONOIIS $20 SLIS L¥ SBWiL 6} Q3ACSAOX3R GYeVaNTLS AYVWIY C9TTSL JG*SSTTTCOO86 #0089 J)JIT/S (ones IG*T2LTCO0%6 =0029 )TZ/S (TE &$S JO°VETTCOO26 =0089 22/95 (S6222 JE°S62e2L(00%6 #0029 JOZ/SS ([9GTSETIC HIST (0086 =00°9 )E2/g (WY6"9) HNOHAS [OM SM) SNOBYHYVIONGAH WLOL £20 d ingeselie Wi (2S¢8S JG°S (Of 3% 18°S [toTbi92)1°9 (ostsi2)t°e dnOH=T (AM $S$4) FJQIXOIA AN4gINS HLYON JHL OL LI3dSAM HLIM S3INDIGH“NOTLIINIGC OQNIM *YNOH Y3d SAIVWRdAAdS CNIMN SUALIW DIANID Yad SWYNOONIIW@SNOTLVYYINIINOD 2SLINn CNOTLIZNIO GNIM (INV OF3dS ANIM OSLVIIOSSY HLIM) CSTETe=Ste02)9T/S (SE20 =GEFT2)IT/SS (SS:2 =GSSts JLI/S COnSLT@“ONnE9TIITSS (GEi9TH=GeiGt)9II/sS 220 [21 AVW YOd SAIVYAAVY INTIQIIS LNJGNSdSONI WNWIXVW BATS SHL SIA 378vL @g NORAWMOANDD a (oN rey OOS re bone Meh oe Me OE ach | 6 ss °h oy me 5 ANTS HLYON JHL OL LIIdSIAY (NOTLOAYIA GNIM Tae} ¢20 3LIS LV S3WIl of $20 SLIS -1V Sawil Gi (WV6"9) YNOHeS (GM SM) JNVHI AW AYW YOd SADVYSAV WOWIXVR HLIM S39au9a0#NOTLIIINIG SYNOH YAd SATIWHGISdS UNIM 2Y9LIW IIBNI HAd SWHVHDONIIWASNUTLVYLINIINOS GNY QaadS ONIM GaLVIDOSSV HLIM) SATS ans OQNIM “TA CLLTibtis®Sd6 (C00t6 “0029 (TOZgs2TI B°L26 (0026 =0089 (6ncit 1°26 (0026 =0089 (9TT8Z JL 5256 (0026 20029 (S6zgi2 JL°186 (0026 #0039 £20 ISLINA 371dvi ~ a a % r t ri MOMWUOANOD II B-1616 aS VATS yie7S YtT/S 1027S Q430349X3 GHVGNVLS AXVONUIFS G30339X3 GHVGNGLS ANVAIUd aS “v7 °s ‘2 aa aLIS Ph Ba Lo27 ) om ob GS OS Om OS GS GD ae a8 OS me GO om OS OS om be OD && 2 68 OD om Ok > MS GD OB i On oD OS Gf 2b EE E> 2D Om OD oe et me oe a SO OS aw at oe ap OS we ee oe ee O8 G8 om OS GE OD OS a 8 a SS om & OF oe ow So & o® Ot OE GF Gs oF on OS Go OD MSS aS 1) Oh OT GD GD OS SI Wh OD aD Ga TH on ScO0rshise Ly. -Sanie sor 20 SLITS LV S3WIL 6t (WV6"9) YNOHHS (OM *SM}SNOHYVYIVHQAH ANVHLAW=NON HLYON SHL OL L99dS94N HLIM S399N9IO=NOITIIDINIO ANIM 2YNOH Y3d SITVWIW#d39dS GNIM SUALIW JIHND Yad SWVYDONIJTW@SNUTILYYLNIINOI (NOILISZYIAQ GNIM ANV O33dS UNIM G3LVIJOSSV HLIM) Te=J AVW YO4 SA9NVYHSZAVY WONWIXVW SAIS AHL SIA ol e (v6 3S J2°Lot Giels es'S: #300 Shale (9978S 11° t¢2 (Sods2 JL * LHe [9ST&8etl9°Sln Q030339X3 Gu¥vVONVIS AYXVONOISS Q9IG3S39X3 GHVONVLIS AYVYWIYd (006 =00°9 )8 /S °S (00%6 =00%9 )2e2/S °r (006 “0039 Je /S °¢ (00*6 =0029 )02/S °e (006 =00:9 )¢ee/S °*T £20 3LIS >SLINN da1qvi la icter Bemba alee sf NOMmwRodNos . . a uae 11 1B- 161s LK SUUM Ae KAKU A AeKHESHKSM HO HHHASKSNAKE RS SHKNSA RRR EKH OHO KEDERSATAAA HAAR AR ARASH ROHS eAeNanee (9623L JE'GLB COTSITHOLESTIET/S °S (TogsLtI2e°T06 (OZtOt=0226 IS /S *H (YGTIOEI B°6S6 (SOSETHSOF2TIII/S *% (VETS JS*OTOFCOSSTIM0S2OTIEI/S °e [ELTIG2I2°GLOT(SSEITHSSS0TIII/S °F £20 3118S HNOH=1 (QM 3SM) JGIXONOW NOUV) HLMYON SHL OL LD9dS3Y HLIM SISNDIGSNOTLIANIO ONIM SHYNOH Yad SATIW=G93dS UNIM SH9L3WN JIGNI Yad SWVYYDUNITWHSNOTLVYLNIINOI PSLINN (NOITLI3YIO GNIM ONV G33dS ONIM G3LVIIOSSY HLIM) Teet AVW YO4 SAOVYABAY INIGIIVS LNAGNAdZONI WAWIXWW BATA 3H1 TIA 3 evi MOLY MOAMOD f TT B=1619 (OLTEL 12°9S9 (SG8E #GStet)St/S °S (OZZ29TIL°269 (SSiec=GGihT)ni/s oh (LUIS 2ie snd (SGREl SSG 0917 Seas (T3226 Jt°R@Ld (SSFBTHSSFOTIST/S °e (60£28 IS°S6L (GSILTHSS%6 JET/S *1 £20 aLIS YNOH=8 (QM *SM) 30IXONOW NOHHVI HLYON JHL OL LO3dS9N HLIM $39N9N90SNOTLISZNIO GNIM 2YNOH Yad SAWW§d39dS GNIM FY3L9W DIBNI Y4d SWVHIONIIWeSNOTIVYLNAINOI FSLINN (NOTLIAYIG GNIM GNV G34dS GNIM GZLVIIOSSV HLIM) beef AVW YOd SANVYSAV ONIGIIS LNSGN3dSONI WNWIXVWW BATA JHL °IA 31HvL MOMTUdodMora ¢ 4 SN Up at ee Tare 4 : ¢ II B-1620 creo ens er DOA MMAR DAMA AMR SAR SANAAOANHHAR DAN SS NDARRANSAHAOHANRRATAAHNABRANNAHHAAHARUNRHB EK KaAanannmnasBnawmnwanuaansan (VolsOZ2IL neat (To2e:otlo°net (letsoeia*set PELE t (no02202)9°L2I (SO:9T#SO02ST)E2/S COSS9t=0SISTILISS (SEtGtSGeentjIT/S (SttateSteLT)&e2/S (SriSt=SninidLt/s £<0 YNOH@ I (UM %SM) 3anN0Z0 HLYON FHL OL LI3dS3N HLIM $3939N9IG"NOITL99NLG GNIM SHNOH Yad SATIW=G33dS GNIM tualaw JIANI Had SWVYDONIIWHSNOTLVYALNAINOD *SLINA Leet (NOILIZYIG GNIM GNV Q3949dS GNIM Q3LVIIOSSV HLIM) AVW YO4 SBIVYSAV ONIGINS LNAZGNAdSONI WOWIXVW SATS SHL “IA 318vi re perme MNOM’7BEOAUDD -. RS “Ss Za PB 6 0°9n E2/G G O°Lh GS /S t) OOS 9T/S g O*hS n2e/s 2 0°L9 LI/S T §20 3118S YNOH=He Zivot lavd UDLiIW DIGNI YAd SHVYHYIONDIIW=SNOITLYYLNIINOI 2SLINN Tool AYW YO4S SIDVYSAV WONWIXVW JAIAS BHL “SIA 3718Vh ¢ | NOMWUOAHOD Rome oye ened 1 ' ' ; ' a 5 RADIAN CORPORATION TABLE VII FUNCTIONAL DEPENDENCE OF RECORDED PARAMETERS UPON WIND DIRECTION i B-2G22 *9 9 *9 *2 *2 *y ‘9 *y *g *y "y *y &¢ *y a, *y ‘2 *y it B-1o25 ; UE i So bv Obie b 60 0 .Ub.8 40 60:0 40:0.6.656 61) & of Wlejeie lars 6 ofble els clots UZ a}sChCh lores" 0 aieie e ote celal) ole iefoiate a 6 6b 64) 0 (nd se wb 60 Goedel: ctl Sze! tae pece eye GtaY 29et!rIZti cee) seue eze¥ cot’ tet’ sot? ezt’ get’ zpe- 2” wid ($08 t Stl t22 948 22k Bye GIE z9Ch ZtZI LOes wee Ece Zot Tet vOS GLb ved gre 3 Ut i4 Ge 3 ? y rd 1 2 G g i rd 1 $ ve ~ QI J : ") J ") s we = 02 t H " J 3 vb = of ") t ) $ @G - wb J t J | : 09 - 4G : 2 HZ - 09 : : 08 ~ Ol : : 06 ~ 08 t 1 vat = 6 t : wlt -~ vet : 2 uel ea : 2 url = bet ; : 09) ~ vps i : wgt ae geew/ ON NUTLVYLNZINOI VWwilOlL kV mNN MN MNM oh MSh MS MSS § ass 439 3$a 3 3N2 JN 3NN ON NOTLIO3ZuN1O ONIM CLEA VOLS © O04 «LEAT 7S OO LM ad «Oe © = “ON HITE LOSfONd IWIO a1VMS g=9 CXON)SSQLXO NADOSLIN YAA37 GNY NUTLI3ZNYLO GONIM AG SB3IdhVS AZLNNIW SALS SO YAUYWIIN ¢ ) NQLAWROANQD FEN Fp et RN LT ie ae! ' | ¢ ) ’ So Ba SCOR ome Ve Bk oA Mg Re. yt Se pe eee Sg Sg. | My Fg ty sv 9b a SEPAS OS SO 8 CESS GOSS O THEE DEERE OCR SED EC D4SS DE ROM SED CHRED ESE CeDDRETE OOo HOCREC OCDE RCEEORER OC Oe dee OD geue ' 6tt Se ‘tec pee eye 6te eget stat eect dev ‘ede’ yot ‘ter’ Sot ‘edt’ oot ‘epe wid euve Sin Vee 828 cet Bye GSTS COLT PIZT ZEcl vty GZe° PDI tes pai 6ZT Pct Gpe : of Ha ve H J rd ra) rA @ S A t rd i $ 2 = ot 4) 3 ~) : Wwe « @2 r) : g t wp ~ o¢ y) : g $ @G “~ Op J t 1 | 2 0g - 4s : t wd - 99 ’ $ 8 = UZ : 3 U6 =e , ¢ ult = 621 oe $ ach aa OS ' 1 ort - 02} $ 95 - ort : vgs 19 Caan/On NOTLVYLNSINGOD WidkL wWIVO MNN HN MNM OM MSM MS MSS oS 4SS 3S 3$3 3 3N3 3N JINN ON NUTLIOZeHIG CNIM CLLAVESS © OF LLAE 7S JUOhNSd Cd: * em HON CRDTIT VR LO3fO08d IU 31VKS 93 CON) HOIXO JISLIN 4A37 ONY NUTLO3Y1O GNIM AG SA4dhYS JANNIW BALd JC BaeWrIN NOMVUOArMAD ee a ae ~ omer “ f =) S808 LLOS L Wildl ie) N 20 “0 °0 "0 °0 =0 £0 Oo .e. 0 al) a) “0 °0 "0 ~0 0 "0 NV 4W af Pay 6 6 6b 0 O66 6 600.8 06 we On 60 6 UB alalefuje le: je ele of8}s] el ciejeie) €je Sia{sleye 6/0 je Gojelatejalere eiere jagetere ayaye: qe ene)e Sysxerege on8 ee eee Stitt Gi2 Tee" ‘Hee ets ““6TS -2Z90T “WELT 662) SER “6L% 991 THt Got 6LT act Lie : AY Oe fa STT 212 GLE hes Be ESS 290T SLI 66S) "SER Off not tnt Got b&L1 9¢T Lhe - OF sea = 2 T t > Qe = O] 0 ; OF - 02 J > ON - 0¢ : OS @ ()f $ 09 = 0G 2 OL = 09 2 O08 ~ OL =: 06 - 09 > OO0T ~ 06 3 OE ~ (OT : Oct - (OTT > Ont = (Oct : ogt = Ont 5s O9T Ko Geen / ON NOTLYYINIINOI W1¥2 MNN MN MNM OM MSM MS MSS § 3SS 3S 3s3 3 3N4o9N INN ON NOILLIIJYIG ANIA CLE/AISZS SOL! HEAP STD OG0TNAd 882 =" PONMATIVGY EDAILOYd WO-31VHS G=9 (2ZON) 3UIXOIQ N3SDVYALIN JGA97 GNY NOILIAYUIG GNIM AH S3AIdWVYS JLNNIW JATA JO YAWN MOoMyvwHrodroz R * manner read oa} ’ Th. B=1626 0 0 0 °0 0 “eo *0 *0 ie) *0 =O °0 °0 °0 °0 “00 AGO SY AW eevee seve eee eee sees vos ete snes eB H CHOKE GeC HEHEHE T HEH HK HCHO RH OHHEHEHR HEH OHHH HEH HOH HHHEHHO HH HEHEHE HB HEHE HH DHS acing a vale Goe cl, pee 9Se HES GUIt tet Tent 6G V6S “SLI “BT” &£fb "Set tht. GSidy = TW LOL HGhees tet Goce. c0 BES. GSE TWEE S GUELIGHOL PEP UoGhes 16G. SLL orth yiaet. SQL tel 65¢ % Of “ola 2 : 2 > 02 ~ OF 3 > 0¢ - 2 : 2 0 - 0¢ : a $05 - On H 2 09 e 0S ; > OL - 09 Hy : 09 = 02 ; > 06 - 08 : 2 008 ~ 06 H : OTF - 00t ; > O25 - OTT $ 2 04 = Oct ; ; Ont = 0&1 H : Ont 1%) ¥¥W/ II) NOLTLVAINIINOD Wi0Ol WIV MNN- AN MNM ™ MSM MS MSS 3ss 3S 3$4 3 3N3 4N ANN ON NOTLISUT0 GNI CLLESTE/G) «6OL LL/V “SS )Q0TeYad «Fe © 8 ON MATT Val LIATOed 110: 3 VHS #2 (20S) 301XUTd ANIING JAA37 ONY NOTLOZYIO UNIM AW SATdWVYS JLANIW FATA JO AFIANNIN NOUVUCAUO? PN FR TRE Or aca tase pte =e ea ‘ } 14 ’ ' ry ie ; (a I] B-1627 °0 “0 °0 °0 °0 = °0 °0 *0 °0 m0 nH) 49 *0 * °0 “0 20 NV 4W Be i a aay aig ceilu ins wr eree esl Mes BNO eo 47 W6 Ste tee eed e's ee ¥..0) ae Are o¥es pee aNa! aFe, ties area) ale te BnE ene ake bi 26.6 8 0x0\ 0/8)88 [GhQ 2 -Tel -Gbeardune VEG wSes SEE HITT Onel OFht ons 16e. Heli et: e@£t {Sel Wik OSes WiOd tGhe s T2t Soe 20 bs 2Se SCE GIT Onet CLnT ene. bot bet unt” eet SQL til ~eSe =< 04 17 ; 2 Oe - Ot ‘ 2 OF = 02 : 2 Ob = OF : 2 0S = On H 2 09 - US : 2 OL - 09 i > 08 - 02 ; : 06 - 08 t : 001 = 06 3 3 Ort = OOF ; 2 Oct - OTT : t oct - 0d H : ont = OFT : s ont 9) £¥¥W/9N NOTLVYLNIINOOD een Nighy O) MINN: MIN MNM OM MSM MS MSS § ASS 088 = O29 G t v t I j } $ OYVYT = B88 v : ) Q ¢ v t wiet «© gaBt H Q 3 ¢ 0 t @2rt = a¢vet re t ) J I M) : #V9T = Bert 9 i i 2 rd t : gegt = orgt 3] H 0 J i 1 obu2 «© Beet i i 0 t : @@¢2 * eee 2 : t J i wvpe = “eee ! : 9492 = bere f $ 0UB82 = 4292 $ ! @uve = H2B2 ; : weve 19 Pean/9On NOTIVYLNSINOD Wwilod wi¥d MNN) MN MNM MM MSM MS MSS § 3S$ 3S 383 3 3N3 AN 3NN N NOTLOZXIO CNIM CZ22/08/G OL LL4/3 ¢G JUOLYSd fe » PAN BBTV LOarO¥d TIO 3TVHS 29 SNOGYVIOUDAH JNVHLISW=NON 3AZ37 ONY NOTLIAZYIO ONIM AG SBTdhVS BSANNIW 3AITS 4O YBEWIIN MOMYWHUOdNEDD EN Pt ren a NT camel ce a | ec s II B-1631 *zep ‘stp “2ap “aap “ten ‘ecy “pov “cup Seep “top “vee “ocr “Sry “pen *2ev “62p Sdop “Sep Wy ay See oeePGKhasesoegsoosee esa Fosse Fe eRe HFERaHeREAGoOCHHoKReSHeKRGO HO KEE HAMS HHKHOKHH KRHA HEB HEH HG HAH HEE KHEHOHHRBHEOKEKTBHHKCAHOHB OHSS é6pes 1 89 GSt 4ee gue ost ace Ope etet 9p6 SoS ece azet ss eat 6 #89 22t t ‘vaca Bees % Bg SGSt p «19 i Qeaw/9ON NOTLVYINISINOD WiLOl WY MNN MN MNM MSM MS MSS § aSs ‘3S CSTE See, SN304 SN 3NN ON NOTLI394N10 ONIM CL4Z/tbE/G Ol 42/3 7S JUOTead £2 © SON BETTI YUL LIAfOUd IO AIVHS 84) (03) 30IXONOW NOGYVI V3A37 GNVY NOTLOSYIC GNIM AG SANdkhYS ALANIW JAIS 40 Y3SEWNN NOMUYWNOdHOD Has sey Oy NI Aiea inna Ee iis *S6 °9OR *96 *66 "oat 16 hts "96 *66 “96 "68 ft "88 "28 SHeoooRKH HO HSH HHKSH HOH RDHEKEHSHHHEH SHH THEHSHKHHH HD EK HOHKHEHOHKHKHEHHKHO RH KEOHHHHKEECKDKHOKKHOKRHHEKRHBHOKHKE HOKE HOH HOKEC HHO OKO HOE pee G2 pee BITt wbet Vrs dps ‘toe vel ‘ert 6pre t tet S62 cep Wil0lL WIVD MNN- MN H t Q bY Ss Ve a @ Y) @ g ’) } @ Y) oo ese ute Get TZt 92h vet £63 998 y oe MN L93fO¥d 110 VHA37 ONY NOTLOZYIO ONIM AG S3TdhY¥S BLINNIW SAIS 40 Y3EWNN a g ) é a r4 pe 49 26 apy 6eb ett rf 8 M MSM (L22Z/TE/5 aIVKS @=9 i) MS NOTLI3NIG ONIM Ol 24/6 /S JQ0LHSd a “ £&9 69T MSS "7 Q § ¥ 4) a$$ 4 38 g2 Q 383 @ "ON UsTIVYd Y 3 4 & So a al “Gi on Ol kOe 60 NY 3K ‘21. Gl PPS © 2Stugtraaiwnol " “ “ a 2 we 14 ¢ u " 2 tw « 02 g v } y) 1 09 = Ob 66-760 =< Obs €2 iade = 29 69 gH} G9 Git 3: Bet * ¢9 ie vl Gh pit stepet .endat 6 ¢ ¢ 2 Opt = B21 $291 = Opt : 08h * 91 : 90% + o8t 1622 = Oz 1 ypc = B22 : gre 19 ean /ON NOTAVYLNZONOD 3N3. 3N 3NN N } i . \ (£0) 3N020 NOMYWHOdUNOD -=3 = RADIAN CORPORATION TABLE VIII DIURNAL VARIATION OF VARIOUS RECORDED PARAMETERS TE B=1695 ‘ | Dil J } / ‘ be CORPORATION DIURNAL VARIATION OF NITROGEN OXIDES(UG/Max3) 5/31/77) PERIOD( 5/ 1/77 TO 23 TRAILER NO, HOUR 19 el 23 24 MEAN 18 17 13 DAY i) * ay xg *% % Se OT a | ca | x3 Laie x3 xf *% 3 10 11 xt x $ 12 3 14 15 16 17 18 19 20 * 3 ee * 3 *s x3 lat *y x3 «$ x3 xy ei xy 22 * 3 23 it 24 ay * 8 25 *3 x8 26 xg Hl | * 3 x2 29 x3 30 bal Ly 0 MEAN 0. TOTAL NUMBER OF OBSERVATIONS BELOW THE MINIMUM DETECTABLE LIMIT OF THE INSTRUMENT t INDICATES CALIBRATION DURING THE ny” x DENOTES A VALID SAMPLE al B- 1 634 i e aor { fees ware ah ee tle bed Nd Lae ' \ t ha CORPORATION ¥) ee kad a Le ; DIURNAL VARIATION OF NITRIC OXIDE(CUG/Mxx3) O/SUL ET) es PERTOOC SA EAT7T TO TRAILER NO, HOUR 20 et 23 24 MEAN t9 18 14 DAY oo Oo *§ * xf *3 xs “—um«m xs bat xy baat «3 * xy 10 ia li2 13 14 15 16 x8 ball x8 * fg x8 x3 *y *y x $ 17 18 19 20 ae *% xt xt xs «8 24 ee 22 23 xe 24 bal lal x4 25 26 xy «3 «Ky Cal * 8 «3 28 29 xy 30 | 0 MEAN 0. TOTAL NUMBER OF OBSERVATIONS CALIBRATION DURING THE HOUR * DENOTES A VALID SAMPLE BELOW THE MINIMUM DETECTABLE LIMIT OF THE INSTRUMENT INDICATES 1: B=11655 24 MEAN cei 2s 19 21 57317 0%) PERTODG: S72 1.777 - 4.0 HOUR = 23 DIURNAL VARIATION OF NITROGEN DIOXIDECUG/Mx«3) TRAILER NO, ] ; t } ) \ aad dias Nae ead Nudd Bae, ky ? J\ } CORPORATION 4 5 av feed Ne ea ’ a a DAY xy * bale Lat ball _ nM xs ooocoooqccoo7ocoo x3 x8 ky xt x3 ee 10 i le [3 14 15 16 V7, 18 19 20 xs Lal | x3 x} * xy * 3 xy * 2 x3 ee KY ol} Lait wy tal at | xf * 3 * 3 x3 a4 x3 xf et 22 23 24 e5 26 27 28 *3 xy kt 29 30 31 INSTRUMENT 0. Bell. MENT MUM DETECTABLE LIMIT OF THE TOTAL NUMBER OF OBSERVATIONS > INDICATES CALIBRATION DURING THE HOw * DENOTES A VALIO SAMPLE BELOW THE 0 MEAN DIURNAL VARIATION OF SULFUR DIOXIDE (UG/Mex3) Ed yh 4 4 “vl % Nie deed “bk CORPORATION gb ry L. 5/31777) PERTOD (657) 17775710 = 23 TRAILER NO, HOUR 24 MEAN ee Ses 21 20 DAY 03 0: 0% 03 03 0% 0: 03 03 03 03 03 0% () Osoe0 0) 0) Q) 03% () 03 3 10 1} 0% 0% 0) 13 0% 0% () 13 14 15 16 17 18 r9 20 0% ee () 03 0: 03 Ot 03 03 fat) 22 B) 0% 03 03 0 24 03 ee 0% 25 26 03 03 0) 0% eT 0% 0 28 0) se () 29 () () 30 cp 03 0 MEAN Oe TOTAL NUMBER OF OBSERVATIONS DURING THE HOUR INDICATES CALIBRATION ® 6 EB 1657 Wi Lay Ls ake : fogs ut WA. eas ti CORPORATION » irs fb uy DIURNAL VARIATION OF SULFUR DIOXIDE (UG/M*x3) 2/51777) PERTOO( S/ 1777 T0 Ce) TRAILER NO, HOUR 24 MEAN él “22 23 20 i} DAY 0% 03 0% 0% 02 03 03 Od 03 eco 13 33 tat 03 1% 03 0 0 08 10 ley ive 1S 14 15 16 ibd A 18 19 20 ) () 0% 08 0 Q 03 1 0) 03 0) 0) Oy rea 03 22 as 24 () 0) 0% 0 0 0% 03 03 25 vi 26 () 08 () nN () 28 29 13 () 03 30 51 0) MEAN 0. 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ENT Tae ’ ii B-A7 Te/G eg/s 62/G 8c/G 4o/S 9c/G Go/G peor ec/s Zo/G 1o/S Ze0/G 61/S al/s¢ ii/G RADIAN CORPORATION APPENDIX A STABILITY WIND ROSE DIAGRAMS EL B=1721 RADIAN CORPORATION APPENDIX A STABILITY WIND ROSE DIAGRAMS According to the data presented in AEC Safety Guide No. 23, the relationships between stability classes and Jg are as follows (the values shown are averages for each stability classification...o, is the standard deviation of horizontal wind direction fluctuations). Average Values Stability. Pasquill or Classification Categories (degrees) Extremely Unstable A 250" Moderately Unstable B 20 0° Slightly Unstable C 150° Neutral D 104.0 Slightly Stable E 50° Moderately Stable F 5. Stability wind roses obtained at the trailers in the monitoring network are displayed in the following tables. Because of the relatively low heights above the surface (9 meters) at which the wind data is taken, the stability distributions are skewed toward the unstable end of the spectrum. That is, the unstable classes (A, B, and C) have a much higher frequency of occurrence than would be obtained with the Pasquill method of stability categorization (or with instruments at higher levels). Table 1 depicts the frequency distribution of Pasquill stability categories based on o, from data collected by M. M. Pendergast and T. V. Crawford = the Savannah River Plant ("Actual Standard Deviations of Vertical and Horizontal Wind Direction Compared to Estimates from Other Measurements", Symposium on Atmospheric Diffusion and Air Pollution, September 9-13, 1974). Three distinct range patterns of stability class II B-1722 ER ZaPe AN CORPORATION distributions were observed: low, mid, and high, according to the height at which the Og Measurements were taken. TABLE 1 FREQUENCY DISTRIBUTION OF PASQUILL STABILITY CATEGORIES Stability Ceteseries based sae none B C 0 E F G SO a, 223 18 ¢c, <23 13 xc, <18 Bec, <12 4 sc, <8 2<7, <4 c, <2 10 22.5 13-2 21.2 23.9 8.9 0.5 35 35 19.3 11.2 19.4 32.4 15.9 0.7 0.5 LOW RANGE 91 9.5 6c7 7355 1.7 2016 WS.2 2.5 : 137 3.3 Se 13.7 70.8 23.5 Taceee Geg.) eD RANGE 182 7.0 2.9 6.3 Wat 25.9 e568 Rag 263 7k 2.3 9.4 yale 27.6 22.9. 10.4 HIGH RANGE 304 72 37 8.0 17.2 23.7 239° tt3 Also, Figure 1 (from D. H. Slade, Meteorology and Atomic Energy, 1968, p. 52) demonstrates that the line represent- ing very stable conditions (which by their nature are associated with light winds) branches into three separate lines near the ground. The curve at the left represents the smallest values of GO, usually observed. The curve that branches Off“to the VEight reflects the contribution of very low-level wind direction meander to the total standard deviation. These meandering oscillations decrease in amplitude very rapidly with height under stable conditions. The central curve represents typical inversion conditions. Actually, for a given stability condition, values of ore will always be greater when the wind is light than when it is strong. This phenomena is most noticeable in the lowest layers. hh Batis RADIA CORPORATION €09 -— -— of ae qrvasce wwaceene a r) a ed - t s aC e ~ adh} = ae 400—. > = Fe = x} Ee =) = 3 » - < ¢ 2 ? = “A c ? » > S oe Z S Y 209— < m a 3 o a se) ‘ ‘ s . . . (e] 5 sO 13 20 re) 23 STANOARO CEVIATICN CF LATERSL WINS SiascTice FIGURE 1 The vertical variation of the lateral wind- direction standard deviation (0,) for various stability regimes. The curves represent average or typical con- ditions with the exception of the two outer "very stable" lines, which represent extremes. The large surface values of D6 for unstable conditions do not decrease very rapidly with height. As in the case of very stable conditions, the greatest lateral fluctuations during a very unstable thermal structure occur with very light winds. As a general rule, for a given insolation condition, increasing wind speeds are associated with profiles of 86 that tend toward neutral stability. The majority of the trailers in the network recorded very light winds throughout the month. Therefore, the stability distributions had a predominance of high Tg values and, hence, unstable classifications. 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