U.S. DEPARTMENT OF THE INTERIOR PROTOTYPE OIL SHALE LEASING PROGRAM TRACT C-b QUARTERLY REPORT #2 (Through February 28, 1975) Submitted to: Mr. Peter A. Rutledge Area Oil Shale Supervisor Conservation District U. S. Geological Survey Grand Junction, Colorado By: Ashland 0i1, Inc. Atlantic Richfield Company, Operator Shell 0i1 Company The Oil Shale Corporation APRIL 14, 1975 QUARTERLY REPORT #2 TABLE OF CONTENTS BY VOLUME NUMBER Volume Number Table of Contents I I. PRE-EXPLORATION FA sea RECONNAISSANCE SURVEYS A. Biological B. Archaeological II. ENVIRONMENTAL BASELINE MONITORING PROGRAMS A. Surface Water 1. Streams 2. Springs and Seeps B. Core Drilling and Associated Ground Water 1. Well Survey Plats 2. Completion Data 3. Drilling Water Production 4. Water Quality - Drilling 5. Water Quality - Baseline 6. Water Quality - Pump Tests 7. Aquifer Data - Jetting Tests II 8. Aquifer Data - Drill Stem §& Multipacker Tests III § IV a. Drei Stem Tests -"SG-17 V b. MPP Series 1 - SG-17 Cc. MBE Series 2 = SG-L7 VI d= MEP Series 3°- SG-17 é:. Driil Stem Tests -°SG=20 é f. Drill Stem Tests - SG-21 9. Aquifer Data - Pumping Tests VII & VIII 10. Lithologic Logs 11. Geophysical Logs 12. Assays 13. Trace Element Analysis 14. Rock Mechanics 15. Gas Samples IX C. Air Quality 1. Air Quality and Surface Meteorology 2. Low Altitude Meteorology 3. Upper Air Studies 4. Visibility 5. Atmospheric Diffusion Studies XXL Gk 6. Radian AQ Data ‘iT? D. aaret Terrestrial Wildlife Studies Aquatic Studies Terrestrial Vegetation Studies Dendrochronology and Dendroclimatology Soil Survey and Productivity Assessment i oe tS III. OTHER STUDIES oe A. Fish and Wildlife Management Plan B. Revegetation Program C. Microenvironmental Program D. Aerial Photographic Study E. Archaeological Studies I Scenic Values Program Ree OO IANS SSE rs Sy SE =X iad fd > gas Ne ma oS bea LS a hte fed bed wns et RC#100-056 QUARTERLY REPORT AIR MONITORING FOR C-b SHALE OIL PROJECT - SEPTEMBER 1974 - NOVEMBER 1974 24. January 2975 Presented to: C-b Shale: Oil Project Suite 555, Iwo Park Central 1515 Arapahoe Street Denver, Colorado 80202 Attn: Mr. Max Legatski Prepared by: Radian Staff II C-688 8500 Shoal Creek Bivd. P.O. Box 939458/Austin, Texas 78765 /(512 FRABDIAN corrorarion E. LE. iL Ee. VI. TABLE OF CONTENTS Page GENERAL DESCRIPTION OF AIR MONITORING PROGRAM...... II C-696 DESCRIPT LON; OF *"ENSTRUMENT SYSTEMS ios Oo otlhe cn nwrewie II C-698 A. Air Quality. Instrumenfation....... cei secicecees II C-698 B Calibration Preoeedrn Gp... ws. \lieiere desuate nk oo Win, bots II C-700 Gi “Data ‘Acquis it Lome S yet oil... dio eens donee raetes » ace, eons II C-702 DD.) Meteorological’ Instrumentation. wi sma’ saps sag oa wie II C-704 MICROMETEOROLOGICAL AND TERRAIN FEATURES........... II C-713 OPERATING ‘TIME VANALYSI Seis iets. + a\s0cx tap tes a So eo II C-719 METEOROLOG@GAL "SUMMARY. stints severe a eth dias ee ates wep ereiee LI: C-725 September Summary. «<2 t.<, ehesanie: ob ae Malo aun gee Sie ara sweeten II C-727 Oetober Summary %....02.g Pe cen sip a ee oe eee ow oes oe IisG-739 November . Summary &. oc, sicathss c,h! ae tees aw Pees eae iB 9 she DATA PRESENTATION AND: SUMMARY 3... sts.0 ad olen ce bos ae LE Ga777 Quarter lye Swear Wir ok wiinedtor« ace he pies ee Dae + wl Ce II C-786 Particulate’ Concentration), Distributnom..... ...5 Sane II C-791 Daily Averace Concentrations. 7c a7... fete. «so eee II C-792 Concentration Versus Wind Direction Cofrel at Leng. vidi tye. eS o's a ae ee cs oe Soe II C-804 otabilityawind Bose Das eames)... seuaeeeeee ccd. . ane Ii G-sst Temporal Varlation.of Reeorded Parameters. ys) 2. II C-891 II. G-6659 ESS OS OES i a a 3 EC ey ems E2ADIEN conroration INDEX TO DATA PRESENTATION TABLES QUARTERLY STATISTICS Site 020 Site 021 Site 022 Site 023 Site 024 DAILY AVERAGES Nitrogen ee ee a me) ee a ee er me | ee ee ee | oer eee ee eee een ete eer seerenne ees eeseeseer ec seeaseeevn ee see ee oN chs sg ain ee ES ata a a eee re ee i ee els ow SE os en Se ee oe Nitrogen Bu IRS pe 2 oe ger ge eo Oe Cie OE Ue eh |r ea . Bitar Daye eas Ge se Ee, ee tis ww Shay: aiarie eoecee eee eee eee eeeneeeseeeeeeeens see e ec ene ee ee Nom-Metharie Hydrocarbons .< sil. a.65) cha ets oie so wpaeoat Pa Ca Ae cs bie ab cia Slalle Oiwi Seen ee Fe on oie eee ee ee QUARTERLY CONCENTRATION DISTRIBUTIONS Nitrogen Site 020 Site 023 Oxides | xide Nitric 0: Site 020 Site 023 oS 8. 6 6°22 \8'S, 6 60-609 BO. 9 6 8 CTO OC A CS OC 4 BOTS Bae a a eer eT, YR II C-690 II II id II II iI II it Et a ‘ge II 1 | i II II {I II II IJ ia C752 C-793 C-794 C-795 C-796 C=797 C-798 G-7o9 C-800 C-801 C-802 C-803 C-804 C-805 C-806 S2 (MOU cornporarion QUARTERLY CONCENTRATION DISTRIBUTIONS (Cont.) Nitrogen Dioxide Site: O20... oh sce ce olan at ee ee etc ames Sie Ss te02 3. ook ee Dee be A Sa Sei are ee ee Sulfur Dioxide SEES 020... ods Ao ns ae ce Sa es Site 021. (7.2.02 dr SRN eek) ot ck, COU Oe) ee Site O22 66. 258 acct ee eee eee awe Calera Pera a es Site: 023... i ee ee eee oe oe er Site v024. ues AOL ME POR ae. Tok ot Hydrogen Sulfide Sie O20 |. tit ow een nape oe age cet « ueipe tle Stee mm RPS Ste OZ os dks ace oe a mw here senees @ e's ea Gotekalaie ees reyes Si £6 022 oso ow Bieta wad ale eee osu, alo ele aio ae es More Site 023%. So hae cere a es Sie see nciene = emai Site: O24. 5 13 ns Secale cei es ie ee re as rhe Total Hydrocarbons Site O20... ih gao ss demo ae ease eeu oles Shee ai Site D Sieg a aes Oe ohn Aa tied es Hee eet ao) exer Methane Si fe O20... er ea ate 6: Sak eee seal elena ns) wun eaten ST te O23 o w.6 See Keokerd a ohare AI CL Re cereus ee aoa ete ater enere Non-Methane Hydrocarbons Sime: O20. ko settee les Coneee teks ae eke rte aaa castes 6 re aertata Si fey. O23 ooo kcal noe Sa Ce Reda 1 ara rate camer Carbon Monoxide Sipe ODO oo ee ns Se ee a pe ee ee. aes Sete O8F0 ta os ele eee es ey, le eee Ozone Site, OZ OS eck... ox ce eee eae alo ree. a atant ae oe Site O23. « 35. cee ae in ee a ces bers arenes II C-691 Page Il II II i II II II II II Il II II II II II II II iG: II II II II C-807 C-808 C-809 C-810 C-8it C-812 C-8135 C-814 C-815 C-816 C-817 C-818 C-871S C-820 C-821 C-822 C-823 C-824 C2325 C-826 C-&27 C-&28 Be OIS22) eorrorarion WIND DISTRIBUTION BY STABILITY CLASS September October.. oeee eee ee eeseeeseeseee ere er eee eereewaeeeeee ee eeeerereereereeeteeseeeseee eevee eeee tt tetse®eeeeeeeee ore er ee eeeseeereeeeeereeeeeeeereeeseseseeeeeeeee eoeeervreeeeereeeeeee ee eee ee eevee wee eeeeee ee II C-692 Page II C-834 II C-848 II C-862 II C-876 RADIAN corporariom DIURNAL VARIATION OF RECORDED PARAMETERS September Nitrogen .Osides soe a sien oe Rintde, bastonoie Nitric Oxide... :. pete. mess PO ee ar eee Nitrogen: Deoxr1de Fe .2 «= soins os dale eeatarele Sulfur Diozsde: .. ae. oe Dieta eM Yeo Hydrogén Sultide.3 2s 2 Ue a oats oe sites total. Hydroearbons 2.3 => + suai = + aeale ss Methane v7 2 Pacis «Seis Saye Se ae, Se or a Non-Methane Hydrocarbons.” .0..cu sens « Carbon Monomide: .'. cise uote ashe aetna als, ose Wind. Speed. 2.2. . é..5taee ese ates Sag Ree cies Wind Direchvons . s win ae ar olene aah ee ate SOPar -RAGEAELOM. «, ...\cls ce ene a wigs stata S46 che ache tel alaes's BL C-695 | eure | ee: | “2 ERAADIFAN corPorarion 2 i GENERAL DESCRIPTION OF AIR MONITORING PROGRAM Radian Corporation is under contract to C-b Shale Oil Project to provide ambient air quality monitoring.* Each site measures and records the concentration of particulates, sulfur dioxide, and hydrogen sulfide. In addition, two of the sites record the amounts of nitrogen oxides, total hydrocarbon, methane, ozone, and carbon monoxide. Selected meteorological parameters such as wind speed, wind direction, temperature, and rainfall are monitored at each station. A 200-foot meteorological tower at one of the sites provides meteorological information as a function of. height. Meteorological instrumentation is planned at the 8, 30, 100 and 200-foot levels. Figure I shows a typical configuration of each monitoring station. The station enclosure provides a sturdy and protective covering for the monitoring equipment. *Five monitoring sites are located in Northwest Colorado in the Piceance Creek Basin on or near the Federal Oil Shale Tract-C-D: II C-696 wOSSaudkod o/V. GovdS WHOM ie |_/ Vauv INSNNULSNI yananoo |< ar | ’ 1 Sa CRS) IP SS » EE; GT 5 YOVYL AIXVI HONG Poa aterm | SOVYOLS AYTZLLIVE ee nara | | | KOOU FLL | a | SAOUV O aan gala YIV OVSZ e — ee eee eee ST ShGRe. alll | BIV OYSZ co ee | ee IT C=697 ERA ISIAAN corrorarion ti. 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 chemilumi- nescent principle, and continuously monitors both NO, and NO. A subtraction circuit in the instrument provides a continuous NO2 output, but is not used in Radian's system. NO»2 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), and 2a linearity of I7. Both sulfur dioxide and hydrogen sulfide are measured with Meloy Model SA185 sulfur analyzers. The hydrogen sulfide analyzer uses a Meloy Model SO,-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 detect- able sensitivity is 5 ppb, and the linearity is, +17: Ozone is measured with a Meloy Model 0OA350 analyzer. This instrument provides continuous measurement of ozone, and is based on the chemiluminescent principle. The minimum detectable sensitivity is. 0.5. ppb and the. linearity, ys 17. Total hydrocarbons, methane, and carbon monoxide are monitored with a Bendix Model 8200 gas chromatograph analyzer. This instrument uses a flame ionization detector and 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 result is displayed for five minutes via a sample and hold circuit. IT C-698 F2ZAADISAM corporarion The air sample is drawn in through a glass cane and manifold supplied by the Ace Glass Company. The system has a 25mm diameter, and a constant air flow through the system is provided by an air pump rated at 60 cfm at 0" head pressure. The manifold has sampling ports to which %"' teflon lines to the instruments are connected. All joints in the sampling system are secured by O-ring (Viton-A) compression fittings. The manifold is contianed 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 particulate samplers (Hi-Vols). Fiberglass filter paper is used for collec- tion of particulate samples, and each filter is brought to a controlled humidity before weighing. Each Hi-Vol has a flow recorder 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 were designed following guidelines recommended by the Environmental Protection Agency and were manufactured by Radian. 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. Tf (G-699 ERED IAIN corporatior B. Calibration Procedures Each trailer contains a Meloy Model RAD-1 calibration unit. This instrument provides a zero air supply, SO2 span gas from an SO2 permeation tube, and NO span gas obtained by pre- cisely diluting bottled NO span gas. The calibration of all in- struments is automatically performed once a day, and is controlled by the computer. Each instrument is first switched to zero, and 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, and if a drift in excess of l10ppb has occurred, an excess zero drift light for the channel in question is turned on on the System Status Panel. Next, the 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 turned on if a drift exceeding l10ppb occurs. The instruments are then returned to the monitor mode, and after two minutes the computer resumes data taking. If an excess drift light is turned on, the operator will note this after entering the trailer, and obtain the calibration data from the computer via the printer. The operator decides whether the drift is severe enough to warrant discarding the previous data, and he then performs a manual calibration to determine if the instrument requires servicing. If so, the instrument is repaired. 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 SO. from the permeation tube. This instrument responds to the number of sulfur atoms per molecule, thus SO2 can be used to calibrate both the H2S and SO2 monitors. The zero air is obtained by passing ambient IT C-700 RASIANM corporar4rion air through an activated charcoal column. These columns are replaced every three months. The Model 0A350 ozone analyzer has its own calibration system which provides a zero check and a span check. The zero air is obtained by passing ambient air through an activated charcoal column (replaced every three months). The span gas is obtained by passing zero air through a calibrated UV source. The ozone calibration system is verified by comparison to a calibrated ozone generator maintained in Radian's laboratory in Rifle. 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 contains methane and carbon monoxide in air, the methane being used to calibrate both the total hydrocarbon channel and the methane channel. This span gas-is checked against a bottle of span gas which was calibrated at the National Bureau of Standards. The Model 8200 is zeroed with air from a Bencix Model 8834 zero air unit (a molecular sieve dryer plus catalytic oxidizer). In addition, the instrument is electronically re- zeroed at the start of every five-minute cycle. Bottled NO span gas is used for calibration of the nitrogen oxide analyzers. Bottles from three different manu- facturers are used, and these agree with each other within 3% (Precision Gas Company, Linde Specialty Gas, AirCo Specialty Gas). The zero air is obtained by passing ambient air through an ozone generator (to convert NO to NO.) and then passing it through two charcoal filters (replaced every three months). Bottled NO span gas has recently become available from the National Bureau of Standards and a bottle has been ordered. Hrec-70r E2AAIDSAALDS eorPoRATION The Hi-Vol particulate samplers were calibrated using a Calibration Kit from General Metal Works. IL Ce7Qz RADIAN corperarion C. 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 hard copy printed out- put. 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 recording. The power to the tele- type and cassette units is turned on only when the unit(s) is to - be used to reduce wear on mechanical parts. 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 110V power from the power lines. In its absence, the computer, which is powered by batteries, switches all trailer 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. IT C-703 FRAEIAR corrorRaArTIon D. Meteorological Instrumentation 1. Ambient Air Monitoring Trailers - Four of the ambient air monitoring trailers are equipped with the following meteorological instrumentation: (1) dry bulb temperature (outside), (2) relative humidity, (3) wind direction, (4) wind speed, and (5) a tipping bucket, heated rain/snow gage. The temperature probe and relative humidity sensor are mounted in- side a motor aspirated radiation shield, the Model 186 Aspirated Radiation Shield by Weather Measure, which gives an aspiration of approximately 100 cfm. The wind instrumentation and temperature and relative humidity apparatus (in the aspirated radiation shield) are all mounted atop a 30-foot crank-up meteorological tower (the WM-33, by Weather Measure) at each of the four trailer sites. The wind instrumentation at the monitoring trailers consists of the Model W103/3L Lightweight Cup Anemometer by Weather Measure and the Model W104-2 Lightweight Vane by Weather Measure. The anemometer is a high response, low threshold wind system which offers the optimum in versatility and economy. For low threshold applications, a unique frictionless tachometer employing a high frequency oscillator and receiver is used to measure precisely wind speed. The oscillator, transmitter, and receiver are encapsulated in a small cube of epoxy for total protection against the environment. The high frequency tachometer embodies several distinct advantages over the commonly used light chopper systems. There are no light bulbs or photocells to burn out; power consumption is low; and the system is insensitive to moisture condensation or dust deposition. The solid state tachomete! is essentially free from maintenance with a life of well over five years when operated continuously. The specifications of the W103 Cup Anemometer are as follows: Il C-704 BE2LAIPIZAAM corPoRaArTion Accuracy: + 1% or .15 mph, whichever is greater. Bearings: Sealed and shielded precision stainless steel. Threshold: 0.6 miles per hour Distance Constant: 5 feet The wind vane, the W104-2, is equipped with a 1000 ohn low torque potentiometer and two wipers for o” to 540° operations. The response characteristics of this vane are: Dead Band: 0 degrees Damping Ratio: 0.4 Distance Constant: 325 feet DAresnold=e0. 75 ees per hour Potentiometer Linearity: 0.5% The thermistor probe used in the motor aspirated radia- tion shields is the Model T621-TP18X Air Temperature Premium Thermistor Probe by Weather Measure. This probe has a range of -50°C to +50°C and an interchangeability of + 0.055°C. The out- put signal accuracy is + 0.3°F. The relative humidity sensor is the Model 2013 Remote Reading Relative Humidity System by Texas Electronics. The sensor assembly contains a newly-developed hygroscopic inorganic sensing i Ur RASTAN corpornr:on element. Its expansion and contraction positions the suspended core of a linear variable differential transformer (LVDT). The absence of friction inducing linkages and wiping contacts minimizes hysteresis and improves accuracy. The. LVDT output signal, when processed, is directly prcportional to relative humidity. The. specifications of this instrument are as follows: « (“Rangevot Indication: “GZ (to 1007 RH * Response: The sensor response time to a step change of 10% in relative humidity is less than 2 minutes with the sensor exposed to moving air. Pe ) Aecunacwe Sg bon RH; 2, 92-8 ie Plots 95% Riot 277 Re 95% -100% RH; + 3% RH *— Solera... Output: Analog signal of -150 mv. £0: 4150 mv. with electrical zero at 50% RH Tse standare. Each of the four monitoring trailers is equipped with a Model P511-E Remote Recording Heated Snow Gage 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 snowfall and rainfall. An insulating cover of poly-vinyl chloride and a thermostatic control insure the proper gage temperature. The thermostatic control is adjus- table 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 Il C-706 E2RZADIAN corporarion @ of durable corrosion-resistant materials to provide many years of service. The specifications of this gage are as follows: ¢ Orifice: 8 inches : Callibeat ions 0.01 inch - Accuracy: 0.5% (Calibrated at 0.5 in/hr). - Sensor: Chrome plated tipping buckets - Switch Mercury, “0.1 second closure - Heat Control: Thermostat adjustment, Oto 35°C. @ 2. 200-Foot Meteorological Tower The tower has instrumentation at four levels: feet, 30 feet, 100 feet, and +200 feetz VAtrall four levels, there ace: wind speed, wind direction, and temperature and relative humidity sensors in a power aspirated radiation shield. Temperature dif- ference thermistors (also in power aspirated radiation shields) and their associated circuitry take lapse rate measurements for the 35-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 II C-707 EPFL fild corPcRATIONn damped vane assembly. The prototype model has been in operation for years under the most demanding weather conditions, performing continuously with the utmost reliability. All of 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: Wind Speed + Starting Threshold: 0.75 mph - Response Distance: 18 feet (63% recovery) - Flow Coefficient: 7.9 feet/Revolution ¢ Accuracy: + 0.4 mph or 1% (whichever is greater) * Range: 0-100 mph Wind Direction Startane Threshotd; 0.73 mph Delay Distance: 4 feet (50% cu nee Damping Ratio: 0.5 to 0.6 Accuracy (540° system): + 17% Range: 0° to 540° II C-708 FeAIDIANS CORPORATION 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 periphery 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: Temperature - Accuracy: + 0.25°C - Range: -50°C to +50°C Humidity -, Accuracy: 7253707. Ru * Range: 0% to 100% Relative Humidity Measurements of temperature difference are taken for two layers,.the: 30-Loeet to 100-fcot dayer and’ the 30-foot, te 200=teot ii C=708 E2PABDIAR corpcrarion = 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: = “mecuracy> + 0:1¢ - Range of AT Circuit (Lower Level-Upper Level): +4°F to -8°F 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 4"" of radial ice per EIA Standard RS-222-B, to 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 attach- ment 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 Lr C-720 RADII CORPORATION 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 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, with characteristics and specifi- cations as described in Section 1. 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 miliibar interval fromig25'imillibars te 825 millibacs . Resolution. Infinite Banéariew. = 0/5 milbiper, overethevres 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 It C=7ia hh nr? FAIS corrornarion eliminate the effects from all outside influences, such as reflection or shadows, on the pyranometer. The instrument characteristics are as follows: - Sensitivity: 5S mv. per) cal/cm* /min - Independence: 300 ohms - Temperature dependence: Sensitivity constant to within + 1 percent over the ambient tem- perature range from -20 to +40°C - Linearity: Response linear up to intensities of 4 cal/cm?/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 resistances are used to calibrate the thermistors, and an rpm calibrating 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. II C-712 RADIAN CORPORATION LEG MICROMETEOROLOGICAL AND TERRAIN FEATURES The Piceance Creek Valley and C-b Oil Shale Tract are situated such that many microscale meteorological pheno- mena affect the region where the ambient air monitoring units are located. In particular, the three units in the Piceance Creek Valley (Trailers 020, 021, and 022) are heavily influenced by a katabatic-anabatic flow regime. 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. Trailer 024, located half- way between the valley and the meteorological tower, is affected by a mixture of the gradient and mountain-valley flow regimes. Elevations in the monitoring network range from about 6200 feet above sea level at Trailer 021, near the Rock Creek Schcoi in the valley at the westernmost end of the monitoring network, to 6940 feet at the meteorological tower site (Trailer 023) atop the plateau within the Tract C-b itself. The largest gradients in elevation in this ares, of cotirse, occtr At joke 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 to west, or from Trailer 022 to Trailer. O20°to Draiser 22. As mentioned at the outset of this discussion, the terrain will have a large influence on the meteorology of this region. Considering fLirst)Trailer 022, .at the eastem end of the monitoring network, a nighttime katabatic (valley or down- slope) flow will exert a tremendous influence on this site. Le Nu Oe RADIA corrorarion Of the three monitoring locations in the Piceance Creek Valley, this site has the steepest valley walls in its vicinity. As a result, the nighttime katabatic flow is strongest here. That is, the downslope winds are constrained or channelled at this point such that the nighttime drainage winds often reach 15 miles per nour.) In addition, the channelling effects of the Piceance Creek Valley walls normally cause surface winds to flow from one of two preferred directions. At night, the downslope winds parallel the valley contours, generally coming from 115° (east- southeast, referenced to true north). During the afternoon, or whenever suitable pressure gradient conditions exist, the winds generally come from the west-northwest because of the boundary conditions and channelling caused by the valley. This monitoring location has an elevation of approximately 6450 feet above sea level and is at the mouth of Oldland Gulch. Trailer 020, midway down the Piceance Creek Valley near the Redd Ranch, at the mouth of Gardenhire Gulch, has an elevation of about 6320 feet above sea level. Once again, the valley walls are steeper to the north of this monitoring loca- tion. The Piceance Creek Valley widens a little from Teailen 022 to Trailer 020, so that channelling effects are not quite as great at this location. Nevertheless, a well-developed katabatic-anabatic flow cycle affects this site, with the “after- noon anabatic flow being fairly well-developed at this location. The channelling effects of the valley walls cause two preferred surface wind directions, southeast and northwest. However, other wind directicns are experienced here, particularly during the transition periods between downslope and upslope flows and during periods when the surface pressure gradient dictates to a large degree the surface wind direction. IT C-714 FEAIDIAL CORPCRATION Trailer 021, located near the Rock Creek School, has the lowest elevation of the three valley trailers, 6200 feet. At this point, the Piceance Creek Valley widens considerably toward the east, so that nighttime katabatic winds are rather light. Daytime anabatic winds are also rather light. However, northwesterly surface winds caused by pressure gradient forces are occasionally moderate in force because of the slight channel- ling effects of the valley walls to the north and northwest. Site 023, where the 200-foot meteorological tower is located, is atop the plateau at an elevation of about 6940 feet above sea level: It is approximately 2.5 miles south of the Piceance Creek Valley. This location is relatively high compared to its surroundings, with the nearest points having elevations 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, 1C0 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 by synoptic-scale features and are usually separated from terrain 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, with the winds increasing in strength with increasing height. II C-715 F2eFAS IAN corrorarion Trailer 024 is between the Piceance Creek Valley and the meteorological tower location, about 1 mile south of the valley itself. The elevation of this site is approximately 6740 feet. The terrain slopes downward to the west, north, and east, and slopes upward toward the south, in the direction of the meteorological tower. This site is in a transition zone between the micrometeorological effects which prevail in the valley and those meteorological phenomena affecting the tower site. Asa result, the meteorological parameters measured at this location are subject to rather rapid variations. The area is generally affected by a weak katabatic (downslope) flow at night and a weak anabatic (upslope) flow during the afternoon hours. However, gradient wind flows generally take precedence over terrain- induced flows at this location. 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 channelling 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 @ry character of the giz in this perceion tot..the “country. ~ Asa 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 20°F lower than they are on the plateau during the early morning hours. In particular, the drainage effects will be spectacular at Trailer 021, which will often experience IT Ce fi6 E2fADIAAnN ecrrorarion temperatures 10°F cooler than those at the other valley monitoring locations during the early morning hours. This phenomenon results from the pooling of cold air in the area of Trailer 021 because of its relatively low elevation and the light nature of the winds here during the night, which thus inhibits surface mixing and promotes the strengthening of the nighttime pround-based inver- sion. During periods of strong gradient winds and/or cloudy skies, greater mixing of the air near the surface occurs and meteorological conditions (particularly temperature and humidity) are more uniform throughout the monitoring network. (on the plateau and in the valley). Pe 717 SHOWIVIS INIUOLUINOW © OW wu «a oss “~ Ca wut or ° ot ae &= a BLIS YSMOL L3W ; 8669 £270 © HONVWY 3LIS_LOVdWI WAWIXVN, ONV1070 ~ O0¢26 = 129 O Me (@) LOSP = ?) v mm HONVY AY 4 ONVIGT0 a ° USL IVM 5 NOOHIS Luymaig “S 3 9 on mM Ore9 x ? HONVY O HONVY ga3ay 2 Oy, YD ty ,0029 120 Q SdLIS ONIYOLINOW LOaYLOud TIO ATVHS 4-9 Z eansty TOOHOS HOON | es) @: E25, DIFA23 corPoraricn IV. OPERATING TIME ANALYSIS The amended Oil Shale Lease Environmental Stipulations require monitoring air quality for sulfur dioxide (S02), hydrogen sulfide (H2S), and suspended particulates on a continuous basis (when applicable). In addition, hydrocarbons, oxides of nitrogen and other pollutants will be continuously monitored as deemed necessary by the Area Oil Shale Supervisor. Requirements for meteorological monitoring include wind speed and direction at three levels near the proposed plant site, one monitor at a height of approximately 30 feet, one not less than 100 feet, and one at an intermediate level. Temperature is to be monitored at the 30-foot level and at a level at least 100 feet above the plant site. Humidity is to be monitored at one level, height not specified. All these meteorological parameters are to be monitored at least 95 percent of the time over each lease year. The lease stipulations in force at the time the air monitoring network for Tract C-b was designed required monitoring at four sites for S02, H2S and particulates; required monitoring for hydrocarbons, oxides of nitrogen and other pol- lutants as deemed necessary by the mining supervisor; and required monitoring over at least 90 percent of each lease year. In order to meet these requirements for 90 percent monitoring at four stations the network design included a complete spare station to be operated continuously so that even with a failure in one station, four stations would still be monitoring. The met tower was designed to monitor wind speed, wind direction, temperature, and relative humidity at four levels: 200 feet, 100 feet, 30 feet and $ feet? Since the lease stipulations have changed since the net- work was designed, the operating time analysis will be presented 2as follows. IT C-719 en" F2FADDi fils corpernrion (1) Air Quality Stations Downtime will be reported as the number of channel-days in the quarter that each channel in each station was not taking data (Table I), and all five stations will be reported. Calibration time will not be counted as downtime. A particular channel will be marked as down on any day when it collects less than half the available data points for that day. The three stations along Piceance Creek had electrical power prior to September 1 (020, 021,:022). Station 023 operated on power from a diesel generator from September 4 to October 4. Station 024 operated on power from a diesel generator from September 27 to October 4. Electrical lines were available at 023 and 024 after October 4. Table II lists air quality data collection percentages for each species for each month and for the quarter. The quarter- ly average for gaseous species and for all species are also given. For SO2, H2S, and particulates, the percentages were obtained with an effective four station network from the four stations plus one operating spare station (023). For the other species the percentages were obtained with an effective one station network from one station (020), plus one operating spare station (023). (2) Meteorological Tower The channels which will be reported in the operating time analysis include wind speed and wind direction at the 200, 100 and 30-foot levels; the temperature at the 200, 100 and 30- foot levels; and the relative humidity at the 200, 100 and 30- foot levels (Table III). Downtime will be reported as the number of channel-days in each quarter that each of the above data II C-720 FRAARSIAAN ecorrcraricn TABLE I OPERATING TIME ANALYSIS AIR QUALITY STATIONS The numbers represent the number of channel-days the particular data channel in each station was not taking data. STATION: SO2 H.S Particulates NO 5 NO 03 Number of days of electrical power per site: 020 37 5 0) 020 021 022 023 024 Zn (es, I] a8 oT a2 88 64 022 41 29 84 023 mB 43 79 35 34 62 59 45 a9 024 28 19 60 E2EkSSisihdy corPporRAvAtion S02 H2S Particulates DATA COLLECTION PERCENTAGES* SEPT 70 TABLE II AIR QUALITY OCT aL a2 22 oF oy 97 39 a2 13 71 100 NOV 99 100 18 100 100 100 73 73 73 83 97 Quarterly Average for Gaseous Species - 76% Quarterly Average for All Species *As defined in operating analysis discussion. II C-722 - 627% QUARTERLY 80 78 14 86 86 86 48 38 ae tie. 96 FREADILAT corpoRrRarion . TABLE III OPERATING TIME ANALYSIS METEOROLOGICAL TOWER The numbers represent the number of channel-days the particular channel was not taking data. Channel-Days SeDE ;) Oct. Nov. Wind Speed 200-foot Zi 25 0 100-foot Zz. Sy 0 30-foot 24 18 0 Wind Direction 200-foot | 5 0 109-foot 22 5 0 30-foot 24 5 0 Temperature 200-foot 2b 7 0 100-foot g2 8 0 30-foot 22 | 0 Relative Humidity 200-foot 2a 5 0 100-foot Zi 5 0 30-foot 21 5 0 Percent met data collection this quarter = 64% (as described in operating time analysis discussion). Li C-12s FRAAES IAAI corrorarion channels were not taking data. A particular data channel will be marked as down on any day when it collects less than half of the available data points for that day. The percent monitoring achieved will be calculated based on wind speed being taken at the 200, 100 and 30-foot levels; wind direction being taken at the 30-foot level and either. the 100 or 200-foot level; and relative humidity being taken at the 200, 100 and 30-foot level. II C-724 RADIAN conrorarion re METEOROLOGICAL SUMMARY The period from September through November brought near normal average temperatures and precipitation to the Tract C-b region of western Colorado. Temperatures were mild to warm throughout the first half of the quarter, but became much cooler during the second half of the period, particularly in November. However, such a climatological sequence is normal for the region. Although precipitation totals were near normal for the quarter, the actual amounts received were light (about two and one-half inches), since the area seldom measures more than one inch of precipitation during any one month. The western Colorado region had basically sunny skies during the September to November quarter. For the entire period under consideration, the area received about 75% of the possible sunshine. The region had a total of 45 clear days, 20 partly cloudy days, and 26 cloudy days. Cloud coverage in the Tract C-b region averaged 4.2 out of a possible 10 for the sunrise to sunset time period and 3.8 out of a possible 10 for the entire quarter. September had an unusually large number of clear days, while October was rather cloudy. November had near normal amounts of cloudiness. For the quarter, the mean upper flow showed a slight ridging condition through the Intermountain Region and slight troughing over the eastern United States. This ridging was particularly well-developed and persistent during September. The quarter was particularly noteworthy for the large number of upper cyclonic circulations which separated from the main portion of the upper flow and settled over the southwestern United States. As a result, precipitation over New Mexico, Arizona, Texas, and southern portions of Colorado was well above normal during the quarter. 11 C-725 2 Adam | | venwett: | E2AAED ELAR corporation Considering the Tract C-b, the stability wind rose shows that winds on the plateau during the September to Novem- ber quarter most commonly were southeasterly through south- southwesterly and west-northwesterly to northwesterly. The other frequencies of occurrence of wind direction showed a bias toward the western half of the distribution. Winds from the northeast quadrant were fairly uncommon during the quarter. The strongest winds on the plateau, however, were almost always south-southeasterly to south-southwesterly or northwesterly, preceding and following the passage of a cold front, respectively. Winds in the Piceance Creek Valley, which showed a very strong katabatic-anabatic circulation dependency, were generally much lighter than those winds on the plateau and were generally east-southeasterly or west-northwesterly in direction. Nighttime temperatures were normally lower in the valley than on the plateau during the quarter because of the strong radiational cooling which prevailed on clear nights with light winds. Therefore, diurnal temperature ranges were much greater in the valley. Trailer 021 normally achieved nighttime minimum temperatures which were considerably colder than temperatures at other monitoring locations when the well- developed radiational cooling conditions existed. Considering each month separately: [I C-726 REID IAT corrorrrion MONTHLY METEOROLOGICAL SUMMARY FOR SEPTEMBER A. Summary of the Major Features of the General Circulation Affecting Western Colorado The domination of the upper air flow pattern by merid- ional characteristics which existed during August continued into the month of September over the North American continent. The - long-wave circulation alternated between meridional and zonal flow throughout the month, with each regime lasting for a period of about five days. However, the periods of large amplitude in the long-waves were dominant in relation to the mean circulation patter. The mean position of the axis of the long-wave trough during September was located through the central part of North America as it was during the month of August. This circulation pattern produced below normal temperatures and above normal pre- cipitation from the Rocky Mountains eastward to the Appalachians. Rainfall was slightly above normal and temperatures were slightly below normal along the Atlantic Coast. Temperatures were above normal and precipitation was below normal in western North America because of the persistence of the upper ridge in that region. However, the southwestern United States was an exception to the generally dry conditions in the west because of a succes- sion of cold-core low pressure areas aloft which cut off from the main flow and settled over Arizona. These cutoff lows in com- bination with an abundance of moist air at high altitudes off the Pacific Ocean resulted in copious amounts of rainfall in Arizona, New Mexico, and the western half of Texas during September. El Paso, Texas, for instance, had measurable pre- cipitation on 12 days during September, with 2 total rainfall for the month of 6.68 inches, which is 5.52 inches above normal. IVC -F27 RADIAN corporavrion | cs | | September also produced two powerful hurricanes, Carmen | and Fifi. Hurricane Carmen achieved landfall south of New Orleans, Louisiana, during the evening of September 7th. Hurricane Fifi had | a landfall near Belize in Central American on September 19th. How- ever Fifi eventually meandered through Central American into the Pacific Ocean, where it regenerated into Pacific Hurricane Orlene. | Orlene then tracked northward toward the Baha Peninsula and was eventually partly responsible for the heavy rains in the south- western United States on September 22nd, 23rd, and 24th, as its moisture became entrained in the subtropical jet stream which traveled over the Pacific Ocean and then over Mexico, New Mexico, and Texas. Meteorological events on September lst centered on the meridional flow enveloping North America. A strong blocking ridge was centered off British Columbia, while a large amplitude trough extended from Hudson's Bay to Oregon. A strong cold front, featur- ing several surface waves, extended on a northwest-southeast line through Colorado. The blocking ridge aloft began to weaken on September 2nd and the entire long-wave trough began to move east- ward rapidly as the next long-wave trough in the hemispherical flow pattern dug southeastward at 150° W latitude. The surface continental polar cold front strengthened at this time and pushed westward over the Tract C-b region during the morning, bringing much cooler ten- peratures to the area. By September 3rd, the polar front jet stream had weakened considerably and the long-wave trough axis had moved eastward to a position at 90° W latitude. Correspondingly, the long-wave ridge in western North America also weakened considerably. As a result, the plateau region of Colorado had mild, fair weather and light winds with a warming trend beginning to develop in the area. IT G-728 RADIAN corporation September 4th featured the weakening of all of the prominent weather systems in North America. The long-wave trough, which was still centered along 90° W, weakened further as did the ridge in the west. Mild, fair weather and light winds continued at Tract C-b because of the subsiding air aloft and the gradually weakening surface pressure gradient. By September 5th, the upper circulation showed definite zonal tendencies. However, a strong short-wave in the northern Rockies was digging through what re- mained of the long-wave ridge at this time. The maritime polar cold front associated with this short-wave trough moved rapidly through Colorado during the day, cooling temperatures slightly and causing a few showers which were mostly orographic in nature. On September 6th the short-wave began to dig into the long-wave trough position over central North America after hav- ing passed through the ridge position. The 500-millibar flow was basically weak. A weak surface high pressure area was centered over northern Arizona, causing warm temperatures, light winds, and generally fair skies in western Colorado. September 7th brought little change in the meteorological conditions at the Tract C-b. The weak surface high was now centered over central Colorado and ridging aloft was building northward into the state. Skies remained clear and temperatures were warm, much above normal for the time of year. Because of the weak pressure gradient, winds remained light and orographic wind systems (valley and mountain circulations) were well developed. On September 8th, a weak, zonal 500-millibar flow pre- vailed over North America with slight ridging over the plateau region. A surface high was again centered in Colorado. Tempera- tures were well above normal with some orographic showers over the Rocky Mountains to the east; winds were fairly trent. September 9th was a continuation of the zonal pattern over North Pi,C-729 RADAR Cesena America. Temperatures were once again well above normal through- out western Colorado. Scattered showers continued to dot the region. A weak surface low began to develop in the vicinity of Grand Junction. September 10th signaled an end to the zonal flow of the previous few days as a strong short-wave began to dig over the northwestern coast of the United States. The developing surface low of the previous day was stationary over western Colorado and eastern Utah. A strong continental polar cold frontal system began to organize in northern Montana. The extremely hot weather continued over western Colorado, but the showers became more mumerous and the surface winds increased in strength as the low deepened. September lith saw rapid changes occur in the long-wave pattern. The short-wave continued to dig southward in the western United States, as lee cyclogenesis took place in southeastern Colorado. In conjunction with the digging trough, a long-wave ridge began to build northward upstream around 130° W. The sur- face low over western Colorado remained intact and was fairly strong (996 millibars). The cold front over the northwestern United States advanced steadily southeastward, passing through the Tract C-b region during the late afternoon. This frontal passage brought showers and thundershowers, a sharp drop in temperatures, and strong winds to the area. By September 12th the upper flow was strongly meridional, with the long-wave ridge continuing to build in the Gulf of Alaska and the long-wave trough amplifying over the plateau states. The cessation of positive vorticity advection over the region during the early morning hours resulted in clear skies during the remainder of the day, but tem- peratures were nevertheless much lower than those of the preceding day because of the continuing cold air advection. Winds diminished in strength during the day. iI C-730 RADIAN corPporaTion On September 13th another short-wave trough dug south- ward into the long-wave trough position over western North America. However, the short-wave trough had the effect of tilt- ing the mean long-wave trough axis to a southwest-northeast line. Also, the vorticity from this system hung back over Nevada and Utah as the rest of the long-wave moved eastward slightly. The development was the beginning of the first of a series of cold-core cutoff lows over the southwestern United States. Cloudiness and a few showers also returned to western Colorado ‘because of this system. Temperatures on the 13th moderated some- what from the cool temperatures of the preceding day. Winds were generally light and variable. By September 14th, a cold low aloft had formed over northeastern Nevada. As a result, cloudiness and showers were widespread over the western half of Colorado and all of Utah. Temperatures were mild and the winds were light and variable. On the 15th of September the 500-millibar low was over northern Arizona. Widespread rains continued over Colorado, as temperatures varied little from those of the 14th and light winds prevailed because of a weak surface pressure gradient. By September 16th the low aloft had moved northeastward to the vicinity of Grand Junction and had filled slightly. There- fore, the rains and cloudiness decreased somewhat in western Colorado, although showers and thundershowers were still scattered around the region during the afternoon. Temperatures remained mild and winds remained Puen. ‘On September 17th, the upper ridge which had extended from California to British Columbia during the pre- ceding three days weakened as a short-wave pushed over it and be- gan to drop into the central part of North America. The weak cyclonic circulation aloft remained over the southwestern United States, centered over central Arizona. A few cumulonimbus clouds nad C-751 RADIA corPpcrRaArTrIONn | . | were scattered over the area during the afternoon. A warming trend | | the long-wave ridge and dug into Alberta, Canada. The weak cutoff | began to effect the region, although winds were still rather light. On September 18th another strong short-wave pushed through low circulation retrograded slightly to southwestern Arizona. Temperatures continued their warming trend and cloudiness decreased | somewhat over the Tract C-b region. The cutoff remained stationary over Arizona on the 19th, but the upper flow pattern became more meridional as a ridge built northward in the Gulf of Alaska and a strong short-wave trough dug southward just east of the Rockies. Although a small surface low developed in eastern Utah, skies were clear throughout northwestern and west central Colorado. Winds were generally light. | On September 20th the strong meridional flow pattern continued, with a ridge in the Gulf of Alaska and a long-wave trough through central North America. The now strengthening stationary cold low aloft was centered over extreme southwestern Arizona. A cold front eased through the area from the east dur- ing the late afternoon but affected temperatures only minimally; the main effects of the front being a drying of the air and a shifting of the winds to a northerly direction. Skies remained clear throughout the day. The low aloft over the southwestern United States drifted southward into Mexico and filled slightly on the 2lst and the meridional nature of the upper circulation over North America continued on this day. Western Colorado was clear and warm because of the subsiding air from the upper ridge to the west. Local circulations (anabatic and katabatic flows) were well developed on the 21st. On September 22nd the cold cutoff low over southwestern Arizona strengthened once again as cold air was advected into it. LD. Ceygae PeADIAR CORPORATION Meridional flow continued over North America as the long-wave trough axis progressed eastward to a position through the Ohio River Valley. Meanwhile, the remains of Atlantic Hurricane Fifi, which had slammed into Belize in Central America three days earlier, reorganized into Pacific Hurricane Orlene and moved northward toward the Baja Peninsula. Generally, partly cloudy skies prevailed over western Colorado on this day, with warm temperatures, light winds, and a few showers scattered over the region. The generally meridional long-wave pattern progressed slightly eastward on September 23rd. The low aloft remained stationary over southwestern Arizona and a small surface low and weak lee trough began to develop over northeastern Colorado. This troughing action shifted the winds to a northwesterly direction during the afternoon, in western Colorado, but the wind speeds remained low. Skies were clear throughout the area except for a few orographic showers and temperatures were mild at. the Tract C-—b- Several large-scale changes occurred on September 24th. The cutoff low over Arizona weakened, as did the entire meridional pattern over North America. However, a strong short-wave in the Gulf of Alaska began to work its way through the long-wave ridge off the western coast of Canada. Scattered cloudiness and a few showers returned to western Colorado, but temperatures re- mained warm. Winds increased in speed somewhat. By September 25th the long-wave pattern became zonal across the United States. However, the strong short-wave continued its southeastward pro- gression through British Columbia. Scattered cloudiness, a few showers, mild temperatures, and generally light winds prevailed Over western Colorado. RRADIAT corrorRaArion _ A zonal flow pattern existed over North American on September 26th. The cold low aloft which had persisted over the. southwestern United States for the past twelve days was finally ejected northeastward into Oklahoma by the strong short-wave in the northwest, which had reached the Washington coast. A strong maritime polar cold front organized along the northwestern United States-Canada border. Meteorological conditions in the Tract C-b region changed little from those of the previous day, with partly cloudy skies, scattered afternoon showers, light winds, and mild temperatures in the area. Rapid changes occurred on September 27th. The strong short-wave dug southward over the west central United States as a strong maritime polar cold front rushed through the Inter- mountain region of the western United States. The cold front _passed through the Tract C-b region during the late morning, causing scattered showers, strong northwesterly winds, some blowing dust, and much cooler temperatures. Skies cleared by sunset. By September 28th the short-wave and cold frontal system had continued to move southeastward rapidly and had reached the central section of North America. Surface and upper ridging affected western Colorado, causing freezing temperatures (during the night), clear skies, and diminishing northwesterly winds. A broad long-wave troughing pattern enveloped North American on September 29th with several strong short-waves en- trenched in the flow. The jet stream and its baroclinicity re- treated northward to a Montana-South Dakota line. Subsiding air continued to affect western Colorado, causing clear skies, moderat- ing temperatures, light winds, and extremely dry conditions. The long-wave pattern became more zonal on September 30th as fast polar jet stream westerlies affected the northern sections of the United States. Meteorological conditions in the Tract C-b area changed IT C-734 RADIAN corPoRATION little from those of the previous day, with continuing clear skies, light winds, mild temperatures, and very dry air. B. Micrometeorology of the Tract C-b Region The Piceance Creek Basin is subject to local circula- tions (anabatic and katabatic winds) of varying intensities through- out the year. These flows are best organized when clear skies and a weak pressure gradient prevail over the area, conditions which are rather common in western Colorado. During the night the higher elevations cool more rapidly than the valley floor, causing cold, dense air to collect and flow toward lower elevations. During the day the opposite effect occurs, in that the higher elevations re- ceive more direct insolation earlier in the day, causing them to warm more rapidly. The resultant density difference between the valley tops and valley floor causes an anabatic flow, with winds blowing up the valley floor and walls. Considering the Piceance Creek Basin and the three monitor- ing trailers located in this valley, the valley-mountain flow regime is very evident. Trailer 022 has the most eastern location of the three trailers in this valley and has the highest elevation above: mean sea level. Trailer 021 is located at the western end of the valley and has the lowest elevation above mean sea level. Trailer 020 is intermediate in both location and elevation. These loca- tion and elevation differences cause micrometeorological effects to appear in the data as a result of the dominent anabatic-katabatic flow regime in the valley. For instance, considering the diurnal variations of wind speeds at these three trailers, winds are strongest (6 mph) on the average at Trailer 022 which has the highest elevation. Winds were Be -C- 735 i | RADIA corPORATION lightest on the average during September at Trailer 021, which is at the lower end of the valley. The diurnal wind speed distri- bution for these three trailers indicates that the katabatic (downslope) wind is strongest at Trailer 022 and weakest at Trailer 021. Conversely, the anabatic (upslope) wind is most strongly developed at Trailer 020 and equal in intensity at the other two trailers. That is, nighttime winds are strongest at Trailer 022 and weakest at Trailer 021. Daytime winds are strongest at Trailer 020. These winds have a profound influence on the temperatures experienced in all three locations. Trailer 022 has the highest mean temperatures. It is warmest at night because radiational cooling is inhibited by the relatively strong winds. Conversely, Trailer 021 has the lowest mean temperatures. This is because nighttime winds are lightest at this location, allowing excellent radiational cooling. Also, cool air from the eastern portions of the Piceance Creek valley drains into this area and settles, caus-. ing colder nighttime readings. Moreover, daytime high temperatures are highest at Trailer 022 and lowest at Trailer 021. Temperatures in the valley during September generally averaged 53.5°F, with an average maximum temperature of 71°F and an average minimum of 37°F. The highest maximum temperature for September was 93°F at Trailer 020 on the 9th and the minimum was 14°F for the 30th at Frazier 02%; Relative humidities during September averaged 50% in the valley. On a diurnal basis the average maximum relative humidity values of 75% occurred at 0800 hours. The average minimum values, about 28%, occurred at 1800 hours. The highest mean humidities occurred at Trailer 022 and the lowest mean humidities were at Trailer 021. Humidities of less than 15% were common at Trailer 021 during the last half of September. II C-756 RADIAN coRPORATION The existence of a local circulation cell in this valley (anabatic-katabatic) is evident upon inspection of the wind direction data. Winds are generally east-southeasterly at all valley trailers during the night when the katabatic flow dominates and west-northwesterly during the day when the anabatic circula- tion takes effect. On days during September with well developed upslope-downslope flow characteristics winds were easterly (90° to 110°) and downslope during the nighttime period from 1900 hours to 800 hours. The winds then went through a transition period for the next two hours, backing into the north and then into the west-northwest (300°) by 1000 hours. These anabatic winds usually prevailed until approximately 1800 hours, at which time they would abruptly veer to a northerly direction and then settle into an easterly direction, usually by 1900 hours, as the katabatic flow again took over. | Conditions at the Tract C-b itself, up on the plateau, were somewhat different. In particular, the anabatic-katabatic circulation cell is not as well developed on the plateau. Also, the cooler air generally drains into the valley from the plateau, causing two main effects: (1) the depth of the ground-based radiation inversion is rather shallow (averaging slightly more than 100 feet in depth during September), and (2) temperatures at night are not as low during radiational cooling nights as they are in the valley. Because the upslope-downslope flow does not effect the tract to the extent that it does the valley, wind directions on the plateau have a high frequency from the southwestern quadrant, in connection with the geostrophic flow (large-scale flow related to pressure gradients). In particular, the 200-foot level of the tower has a very high frequency of southwesterly winds, even at night when the lower tower levels are enveloped by a ground-based radiation inversion and drainage flow. Il C-737 FPALLAN eccrrPornv7icn Winds can be rather strong on the plateau and around the tower site. The highest hourly average wind speed recorded during September was 24 miles per hour on September 27th, as a strong cold front passed the area. Winds increased in speed with height dur- ing September, as was to be expected. The average wind speed at the 100-foot level for the month was 9 mph, higher than in the valley. . The air was much drier on the plateau than in the valley (moisture occasionally becomes trapped in the valleys) during» September. Humidities for the month averaged in the low 30's. Mean temperatures for the month of September were slightly higher on the plateau than the valley. Daytime temperatures averaged about 2 degrees lower at the tower site then in the valley, but nighttime temperatures were about bere higher, with an average minimum temperature of 42°F and an average maximum of 69°F. The average temperature at 200 feet was 55°F, but the diurnal range of temperatures was smaller than at the lower tower levels. lI C~738 E2ZAD IFAT corrornation MONTHLY METEOROLOGICAL SUMMARY FOR OCTOBER A. Summary of the Major Features of the Upper Flow Over North America . North America during October alternated between periods of zonal and meridional flow, with two sequences of split upper level flow. The upper flow was basically zonal (or west-east) over the United States on October 2,4, 7, 225°13, 22; 23,7288. The flow was generally meridional (north-south) on October 2-3, 5-6, 9, 14-21, and 25-26. Split upper level flow prevailed on October 8, 10-11, and 27-31. The net results of these cir- culation patterns for the month of October were: much below normal temperatures and below normal precipitation over the north- eastern United States; below normal temperatures and much below normal precipitation over the Atlantic seaboard states; near normal temperatures and precipitation over tke Central United States; below normal temperatures and slightly below normal pre- cipitation in the South; much below normal temperatures and below normal precipitation in the north central United States; below normal temperatures and above normal precipitation in the South- western United States; slightly above normal temperatures and near normal precipitation in the Rocky Mountain regions; and penerally above normal temperatures and below normal precipitation in the West. October began with a mean long wave ridge axis extending from western Canada to northern California. A rather deep long wave trough was positioned through the eastern United States. Precipitation was confined to the far northeastern portion of the United States. A stationary cold front extended from Montana through Wyoming to southern Nebraska. By October 2nd, the long wave pattern had amplified so that a well defined long wave trough mite 7152 FRADE AN corPORATION extended from the Great Lakes to Florida. A strong upper ridge extended from Utah to north central Canada and a deepening upper trough was approaching the Pacific coast. A weak upper low was off the California coast. On the surface, a large, cold high pressure system was centered over Illinois. A warm front extended southward along the Rocky Mountains from Canada, while a strong maritime polar cold front came inland along the Washington coast. Precipitation was confined to California, Washington, and the northeastern United States. On October 3rd, all of the major features of the circula- tion over North America moved eastward. The long wave trough along the Atlantic seaboard moved eastward slightly and amplified. The upper ridge also moved eastward to a position from Kansas to Minnesota and then northward into Canada. The upper trough in western North America also moved eastward and flattened somewhat. On the surface, the large surface high was still centered near the Great Lakes region, while a cold front advanced across the Great _ Basin. Precipitation was widespread across the Intermountain Region. By October 4th, the cold front had pushed completely through Colorado into the Midwest. The large surface high moved southeastward to a position along the Atlantic seaboard. At upper levels, strong short waves were located off the ccast of the eastern United States, along the Rocky Mountains, and along the west coast. Precipitation, mostly light, was scattered throughout the western two-thirds of the United States. On October 5th, the general positioning of circulation systems remained about the same. The long wave in the western United States amplified slightly. Precipitation was moderate from the Great Lakes to Montana and south from there to Kansas. On October 6th, the northern half of the long wave which had been over the western United States was reinforced and moved II C-740 RADIAT corPORATION eastward, thus causing the southern half of this wave to be sheared off, forming a cutoff low aloft over California. The cold front which had been across the Midwest was reinforced by the deepening of the northern half of the short wave and moved southward as a result. Cloudiness and precipitation were widespread in a band from Arizona and New Mexico to Minnesota and the Great Lakes on the 6th, but decreased throughout western Colorado. By October 7th, the western two-thirds of the nation was under the influence of a large dome of high pressure. The short wave that had been over the Midwest on the 6th moved eastward rapidly, to a position over the Great Lakes. The cold front associated with this short wave extended southwestward from Maine through Tennessee to central Texas. The low aloft over California persisted, causing precipitation over southern California and Nevada. Precipitation also extended along the front from Texas to New York. Skies were clear to partly cloudy over western Colorado. The upper flow pattern was split in the western United States on October 8th, as the upper low persisted. The cold front and short wave in the eastern United States con- tinued to push eastward to a position off the coast. Most of the nation was under the influence of a large, weak high pressure system. Precipitation was confined to California and Nevada. By October 9th, a short wave approaching the western coast of the United States caused the upper low to be ejected northeastward to a position over Nevada. A weak cold front extended from the Great Lakes to Nebraska but no other significant weather systems affected the United States. Temperatures were cool in the Northeast but seasonable elsewhere. A weak surface high pressure area affected most of the United States, resulting in many areas of light winds and stagnation. Precipitation in the United States was confined to the Great Basin area. October 10th PG: /4 RADLAM ccorrPorRarTion saw a split upper level flow regime return to the western United States. A short wave trough was located from Idaho to southern California. Showers and a few thundershowers were scattered throughout the Intermountain Region and the western slopes of the Rockies. A few showers fell in the Tract C-b area. ‘The split flow regime continued in the western United States on October llth. The short wave from Idaho to California stayed nearly stationary. A cold front extended southwestward from a low pressure system on the Minnesota-Canada border through Nebraska to northern New Mexico. A secondary cold front extended westward to Montana, also from this low. Precipitation was wide- spread throughout the western half of the nation on the 11th, with showers and thundershowers again dotting western Colorado. By October 12th, the two cold fronts through the northern Plains States had organized into one strong frontal system which extended from the Great Lakes southwestward to the Texas Panhandle. The short wave trough which had been stationary over the western | United States for the two previous days finally formed a weak low pressure circulation aloft over western Arizona. Precipitation covered a large portion of the United States extending from Arizona northeastward in a broad band to the Great Lakes region. A large cold high pressure system dominated the weather in the western half of the United States behind the cold front. Considerable cloudiness and a few showers persisted in western portions of Colorado. By October 13th, another in a series of upper level short waves moving rapidly into the northwestern United States from British Columbia caused the upper low center over the southwestern United States to move slowly eastward. This approaching short wave had associated with it a moderate polar maritime cold front, which was located across central North Dakota and Montana on the morning II C-742 PADIAAI corPORATICN of the 13th: Precipitation was widespread across the middle of the United States on the 13th, extending from New Mexico to the Great Lakes in a very broad, nearly solid band. Skies cleared over western Colorado on the 13th as the upper low was forced eastward. The short wave amplified rapidly on the 14th, causing the cold front to move southward rapidly. The front passed through . western Colorado during the morning of the 14th, causing cooler temperatures and a continuance of clear skies. Precipitation once again occurred in a broad band across the central part of the United States because of the strong short wave and cold front. The short wave and cold front continued to move eastward rapidly on October 15th, thus forcing the precipitation area eastward with it. A large upper ridge and surface high covered the western half of the United States on the 15th, thus causing a continuance of fair, dry conditions.in western Colorado on this day. October 16th and 17th were very similar with regard to the upper flow patterns which prevailed over North America on these two days. A large surface high pressure cell dominated most of the United States during the period. Precipitation was confined to the eastern fourth of the country. A large upper ridge prevailed over California, Nevada, Utah, Idaho, Wyoming, and Coiorado on these two days, while a large amplitude upper trough extended from the Great Lakes region to the Gulf of Mexico. Fair and mild weather prevailed over western Colorado on these days. The same basic meridional flow pattern persisted over the United States on October 18th and 19th. A strong upper ridge dominated the flow in the western United States on both days, with a deep upper trough along the Atlantic seaboard. The systems pro- gressed eastward very slowly, so that another long wave trough reC-745 RADIAN COoRPORRTION began to approach the Pacific northwest by October 19th. Pre- cipitation was minimal across the United States on both the 18th and 19th. A weak cold front progressed southward through the eastern half of the nation on the 18th and 19th, but did not affect Colorado at all. Meteorological conditions remained fair and unseasonably warm throughout western Colorado on both of these days. The upper flow began to change on October 20th. The upper ridge and trough progressed eastward slowly, but a strong short wave began to dig southward along the west coast of the United States. A cold front associated with the short wave extended southward from eastern Washington into northwestern Nevada and northern California. Precipitation was confined to the northwestern and northeastern portions of the United States. Fair and warm conditions continued in western Colorado. The short wave in the Northwest continued its easterly movement on October 21st, forming a closed upper low circulation in the process. The polar maritime cold front continued its eastward movement, passing through western Colorado during the afternoon of the 2lst. Because of the upper low and its associated moisture and positive vorticity advection, cloudiness and scattered rainfall returned to western Colorado on this day. Actually, pre- cipitation was scattered throughout the entire length of the Rockies. Precipitation and considerable cloudiness continued in western Colorado on October 22nd as the upper Low strengthened Slightly and remained stationary over northern Nevada and northern Utah. The upper flow became fairly zonal on this day, with the jet stream located along the United States-Canada border. The polar maritime cold front moved eastward through the northern Plains States but did not advance southward because of the zonal nature of the upper flow, the northern position of the jet stream, II C-744 RADIAN corPorRarion and a blocking high pressure cell in the southeastern United States. Precipitation was widespread throughout the southwestern United States on this day. The upper level flow over northern Nevada strengthened further by the morning of October 23rd, causing the broad area of precipitation to persist over the Plateau region and southwestern United States. Temperatures were cooler and cloudiness and pre- cipitation were widespread throughout western Colorado on this day. The zonal character of the upper level flow and the northward retreat of the polar front jet stream into Canada caused the maritime polar cold front through the central part of the United States to become stationary. Precipitation was scattered along this front from Texas to New York. Rains continued in western Colorado during the morning of the 24th but began to diminish in areal coverage later in the day as the upper low over northern Nevada began to fill gradually. A short wave moving south from Canada into the northern Great Plains brought with it a weak cold front which extended into northern Wyoming during the morn- ing. Precipitation was heavy in Texas and Oklahoma on this day. Clearing took place in western Colorado during the night of the 24th as the cold front passed through the region and a high pres- sure ridge built southward into the area. The upper flow once again had meridicnal characteristics by October 25th, although the flow was beginnirg to show splitting tendencies once again in the western United States. An upper ridge extended northward from Colorado through Montama and into Alberta, Canada. A long wave trough extended southeastward from Hudson's Bay into New England and a short wave and upper closed low came onshore in the Pacific northwest. Precipitation occurred in Wasnington and Oregon and through the center of the nation, along a cold front which extended from Texas to the Great Lakes. Mild temperatures and clear skies prevailed in western Colorado. DY (C=745 P2ADIAM corRPORATION Cloudiness returned to western Colorado as the short wave moved eastward from the Pacific coast on the 26th. Pre- cipitation was restricted to the Pacific Northwest, the Southwest, and the Midwest as an upper ridge which extended from Florida to Alberta, Canada brought fair weather to most of the nation. The upper flow became split in the southwestern United States on the 27th, as a cold pool of air at upper levels became cutoff from the longwave circulation and formed a closed low over western Arizona. This low caused scattered light precipitation throughout the Southwest on this day. Cloudiness increased throughout western Colorado as the day progressed and light precipitation was ex- perienced in the area during the evening hours. ~ An approaching short wave from the Pacific caused this upper low to be ejected northeastward by October 28th, resulting -in continued cloudiness and scattered precipitation in western Colorado. This approaching short wave caused the generation of @ strong surface low pressure area (cyclogenesis) in Oregon, from which trailed a polar maritime cold front into California. The split flow characteristics and broad upper level troughing which prevailed in the western two-thirds of the United States caused this entire region of the nation to be covered by cloudiness and precipitation. The split flow in the polar front jet stream continued on October 29th, with a strong upper low forming over Nevada. A strong surface low was centered over western Utah during the morning of the 29th, with a moderately strong maritime polar cold front trailing southward. Cloudiness and precipitation continued in western Colorado, as the storm produced the first widespread snow of the season in the Intermountain Region. These cloudy and snowy conditions persisted in western Colorado on October 30th, as the upper low intensified and moved northeastward to a position IL C=746 RADIAN corPcrRarTion over central Utah. The surface low had meanwhile moved to eastern Colorado and weakened somewhat. Cold frontal passage occurred late on the 29th in western Colorado. By the morning of the 30th, it was located on a line from eastern Colorado southward to western Texas. Much of the nation received precipitation on this day due to the amplitude of the upper level troughing over the western United States. Cloudiness and snows continued in western Colorado on October 3lst as the intensifying upper low was pushed northeast- ward by an approaching short wave just off the northwestern coast of the United States. On the morning of the 31st, this upper low was located over central Wyoming. The split in the upper flow over the western United States continued, however, with a broad upper trough continuing to affect the western two-thirds of the United States. A surface low was located in Wyoming by the morn- ing of the 3lst, while a maritime polar cold front extended from Idaho into central California. Precipitation was widespread through- - out the western and central portions of the nation. B. Summary of Meteorological Conditions in the Tract C-b Region ——— es Precipitation totals and temperatures were near normal in the Tract C-b region of western Colorado during the month of October. The area experienced seven cold frontal passages during the month. (October 3°55, 10,14, 209.24. "and 79). .Theistroncese of these fronts was the one which passed through the region on October 29th. Precipitation was experienced in the area on twelve days of October (October ‘3, 5,10, G.822 23, 26°27, 28, 27942 31), but most of the daily totals were low. Snow was experienced in the area of the Tract C-b on October 29th, 30th, and 3lst, but TE a747 RZADIANM corrcoragrion snow amounts were rather light and melting occurred within a few days. Temperatures were below normal during the periods from October 3rd through the 7th and October 11th through the 15th. Temperatures were much below normal on October 29th, 30th, and 31st. Temperatures were above normal on the other days of the month, but were much above normal during the period from October 17th through the 22nd. : ; The area received 62 percent of the possible sunshine. during the month. Sky coverage by cloudiness in the general area totalled 5.3 out of a possible 10 during the period from sunrise to sunset during October, and 4.9 out of a possible 10 for all possible observations during the month. The region experienced 10 clear days, 9 partly cloudy days, and 12 cloudy days during October. Thunderstorms were in the area on two October days (October 10th and llth). Grand Junction, Colorado, about 75 miles te the southwest of ‘the Tract C-b,;, meceived 72 anch of precipi ta— tion during October, which is .21 inch below normal for the month. Poor dispersion or air stagnation conditions occurred occasionally in western Colorado during October. .The period dur- ing which dispersion conditions were worst in the Tract C-b region was from October 17th through the 20th. During this interval, the region was influenced by a large persistent upper ridge over the western portions of the United States. This ridge brought clear skies to the Tract C-b area but also brought rather low mixing heights and subsidence aloft. The weak surface anticyclone associated with this upper ridge further compounded the problem by causing very light surface winds throughout the area. The net result was an extended (3 or 4 days) period of locally poor dis- persion conditions. The following is a summary of all air stagnation messages fiom the National Weather Service pertaining to western Colorado II C-748 Fe ADaIsaAzd corrPoRATION | during the month of October. The messages were received in Radian's facilities via the Service "C" Weather Teletype Circuit from the National Weather Service, a cable service to which Radian subscribes. These Air Stagnation Narratives are coded as "FKUS" messages. * October 2nd: “In the western United States, the ridge moving through the Intermountain Regions of the Rockies is supporting the development of stagnation in portions of Colorado, Arizona, New Mexico, and West Texas...The stagnation will diminish as the ridge moves eastward." * October 9th: "The stagnation through the Rockies this morning will diminish during . the day as the trough moves into the Intermountain Region." * October 16th: “Deteriorating local disper- sion conditions over much of the United States west of the Rockies during the next 24 hours.” )’ October. 1/th: “Stagnation ‘conditions are persisting over the western and south- western United States as a result of little movement of the upper ridge over the Pacific Northwest and no movement of the flat sur- face high pressure area." Ii C-749 RADIAN corRPoORRTION - October 19th: "Large-scale stagnation exists over the western United States from extreme West Texas through New Mexico to western Montana. An ASA (Air Stagnation Advisory) is in atfect for much of this area. i C. Meteorological Discussion of. Tract. C-band the Piceance Creek Valley Meteorological conditions often varied considerably from the Piceance Creek Valley to the Tract C-b itself during the month of October. Anabatic and katabatic circulations were much better organized in the valley at Trailers 020, 021, and 022 than on the plateau at Trailers 023 and 024. Nighttime temperatures were much -colder in the valley than on the plateau during nights when radia- tional cooling occurred and the downslope flow became organized. The diurnal range of temperatures was much greater at the Valley Trailers (020, 021, and 022) because of the mountain and valley circulations, with daily temperature ranges of 35° common at these trailers during October. Trailer 021 generally had the largest diurnal range of temperature, mostly because of its location. At this location, the katabatic winds were fairly light at night because of the widening of the valley just upstream to the southeast. As a result, the mixing of the air was diminished during the’night and cold air from higher elevations was allowed to collect in this relatively low area of the valley. Thus, radiational cooling was allowed to proceed uninhibited and temperatures fell rapidly dur- ing the night. Nighttime minimum temperatures were generally at least 5°F colder at this trailer than at the other two trailers in the valley and at least 10°F colder than minimum temperatures at Trailer 023 on the plateau, where the katabatic circulation cell was not developed so as to abet rapid cooling. It C-/30 IRAADEAAM corPpoRaATION On the majority of the nights in October, Trailer 021 had the lowest minimum temperatures, followed by 020, 022, and 023. Temperatures were higher at Trailers 020 and 022 during the night because of increased wind speeds from the katabatic circulation, which mixed the air near the surface to the extent that the ground-based radiation inversions that formed near these trailers were not so intense as the inversion (coldest at the lowest level) at Trailer 021. During the afternoons, temperatures were much more uniform at all trailers because of increased vertical mixing from convection and the anabatic (upslope) flow. Daytime maximum temperatures during October were generally highest at Trailer 023, followed closely by Trailers 022, 021, and 020, in that order. Relative humidities were generally rather uniform in the Piceance Creek Valley during the month, averaging about 62 percent. Humidities were a little lower on the plateau (because of slightly drier air and higher average temperatures), averaging about 53 per- cent at the 30-foot level of the meteorological tower. Winds were generally much lower in the valley than on the plateau during the month. Winds generated by pressure gradient forces were normally decreased in strength substantially from the plateau to the valley. While the strongest winds during the month were generally the result of synoptic-scale developments on the plateau at the meteorological tower, the strongest winds in the valley were often the result of katabatic or anabatic circulations. Winds at Trailers 020, 021, and 022 exhibited marked channelling effects because of the steep valley walls in the vicinity. Winds at Trailer 022 were normally either east-southeast or west-northwest while winds at Trailers 021 and 020 were normally either northwesterly or southeasterly because of the katabatic- anabatic circulation cycle. However, during transition periods TI Gaol BEDI corporarion between upslope and downslope flow, or vice versa, the wind direction was rather variable at these locations. In addition, on occasions when the surface pressure gradient was weak and an anabatic or katabatic circulation cell was not developed, the | winds were often calm or variable in direction. At Trailer 023, winds did not exhibit as much of a terrain or micrometeorological dependence. Pressure gradient forces for the most part controlled the wind directions and speeds at the meteorological tower. Both the mode and mean of the dis- tribution of wind directions at the tower were south-southwesterly or southwesterly, depending on the level of the tower under con- sideration, which is a reflection of the pressure gradient forces which existed in the Tract C-b region during October. Winds generally veered in direction (clockwise progression) and increased in speed with increasing height at the meteorological tower. Average temperatures in the monitoring network for the month of October ranged from 39.4°F at Trailer 021 in the valley to 47.3°F at the 30-foot level of the meteorological tower at Trailer 023. The average temperature at Trailer 020 was 41.3°F, two degrees higher than at Trailer 021. At the meteorological tower, average temperatures were fairly uniform, ranging from 45.7°F at the 8-foot level to 47.3°F at the 30-foot level, with the 100-foot and 200-foot levels registering intermediate values. However, the average temperatures do not reflect the diurnal variation of vertical temperature structure which occurred at the tower. During cloudy, wet days, near-isothermal conditions prevailed at the four tower levels. However, on clear or partly cloudy days, the normal thermal pattern was: (1) inversion to 100 feet, with unstable lapse rates above that during the night, and (2) unstable lapse rates to 100 feet with an inversion above that during the day. The layer above 100 feet seems to have been LI -C- 7352 ER.ADTAR corporation decoupled from the layer below that level much of the time. How- ever, during extremely windy or cloudy conditions, there was more uniformity in the vertical temperature structure. The highest daily average humidity reading in the valley during October was 93.9 percent at Trailer 022 on October 29th. October 5th also had average relative humidities above 80 percent. Likewise, on the plateau, October 5th and 29th had the highest average relative humidities. October lst and 2nd were the driest days of the month, both in the valley and on the plateau, with daily average humidities in the twenties. The highest daily average temperature in the region for October occurred on October lst. The average temperature this day at the 30-foot level of the meteorological tower was 61.0°F. Meanwhile, in the valley, the average temperatures ranged from 46.0°F to 48.1°F. The much lower average temperatures in the valley were due to much lower temperatures from strong radiational cooling during the night. The lowest daily average temperatures in the network during October were recorded on October 30th, a snowy day, when temperatures ranged from 27.6°F.to 29.9°F in the valley and from 29.8°F to 31.0°F at the four meteorological tower levels. The highest maximum temperature recorded in the valley during October was 73°F at Trailers 020 and 021 on October 2nd. The highest temperatures recorded at the meteorological tower during the month occurred on October Ist, 2nd, and 15th. The lowest temperature re- corded in the valley during October was 14°F at Trailer 021 on October 15th. The lowest temperature recorded on the plateau was 24°F on October 30th. Considering the valley stations, winds were strongest at Trailer 022 during the month, averaging 5 miles per hour. Winds at Trailer 021 averaged 3 miles per hour and winds at Trailer 020 ba ay Pet Pes eo a or ae : enemas. | | pies | Fe CARI AT coRrPpoRATION averaged 2 miles per hour. The highest daily average winds occurred on October 3rd and 21st. On a diurnal basis, the strongest winds occurred from 1300 to 1500 hours at Trailer 020, from 1500 to 1800 hours at Trailer 021, and from 0100 hours to 0200 hours (katabatic winds) at Trailer 022. At the meteorological tower, wind speeds averaged 2 miles per hour for the month at the 8-foot level, 7 miles per hour at the 30-foot level, 6 miles per hour at the 100-foot level, and 9 miles per hour at the 200-foot level. The windiest days of the month on the plateau were October 21st and 3lst. On a diurnal basis, winds were strongest on the plateau during the period from 1300 to 1500 hours. Winds were lightest from 0800 to 0900 hours. The highest 5-minute average wind speed recorded in the valley during October was 23 miles per hour at Trailer 021 on October 3rd. The highest -5-minute average wind speed recorded at the meteorological tower site during October was 35 miles per hour, at the 100-foot level, on October 21st. FRAUD EAAIN corrPoraricn MONTHLY METEOROLOGICAL SUMMARY FOR NOVEMBER A. Summary of the Major Features of the General Circulation over North America During the month of November, the general circulation over the United States was fairly normal. That is, in general, the various sections of the country did not experience prolonged periods of abnormally extreme cold or heat. In addition, most’ sections of the nation did not deviate appreciably from monthly precipitation norms. The long wave circulation in the upper atmosphere generally alternated between periods of zonal and meridional flow during the month. Split flow dominated the upper flow from November lst through November 6th. Otherwise, meridional or zonal flow regimes prevailed. Zonal flow, or west-to-east flow which promotes rapid variations of a rather weak nature in the meteorological conditions in a region, occurred in the United States from November 7th through the 9th, the 16th through the 23rd, and on November 30th. Meri- dional flow, or north-south flow which causes rather extreme meteorological conditions (hot or cold, depending on relative location in the circulation pattern) of a rather persistent nature, existed from November 19th through the 15th and from November 24th through the 29th. | The results of these circulation patterns over the various sections of the country during November were fairly uniform. In general, much of the nation had temperatures which were above normal for the month and monthly precipitation totals which were also slightly above normal. Specifically, the north central portion of the country, including the upper Midwest and Ohio Valley, had temperatures and monthly precipi- tation totals which were slightly above normal. The North- east had near normal temperatures but below normal precipita- tion. The Atlantic seaboard region had temperatures and Pi C=755 ea. 2 2A 339 ee - precipitation totals which were slightly above normal for the month, while the South had near normal temperatures and slight- ly above normal precipitation. The central portion of the United States had above normal temperatures and slightly above normal precipitation during the month. Meanwhile, the Rocky Mountain region and Intermountain Region had slightly below normal temperatures and precipitation totals which were slightly above normal. The Southwest also had temperatures which averaged slightly below normal, but had above average precipitation. Finally, the West and Pacific coast areas had temperatures which were much higher than monthly normals and precipitation totals which were above normal. No extremely cold Arctic air masses advected south of the Canadian border during the month. The mean position of the long wave trough over North America was through the west central United States during November, while a weak mean ridge was situated on a north-south line through the eastern portion of the nation. November began with a broad upper troughing pattern over the western United States, with ridging over the Atlantic seaboard. The split flow conditions caused one large upper low pressure area over northeastern Wyoming and another over northern California. A stationary front extended from the Great Lakes to southern Texas and a cold front extended south- ward from a surface low over eastern Nevada, Precipitation was scattered throughout the western half of the nation and also along the stationary front from Texas to Indiana. Skies were overcast in western Colorado in the vicinity of Tract C-b on the lst and rain and snow showers were widespread throughout the area, E2AADIAN corPornarion November 2nd was much the same. The upper low in Wyoming moved northeastward to the North Dakota-Canada border and the upper low in the Southwest strengthened slightly and moved southward to southern California. A surface high pressure region began to build (anticyclogenesis) over the western portion of the nation. The stationary front through Texas moved northward as a warm front to a position along the Red River Valley, while the low over Nevada moved to southern Arizona. Precipitation was widespread across the western three-fourths of the nation. Cloudiness decreased somewhat in western Colorado, but scattered rainshowers still persisted in the region. On November 3rd, the upper low in the Southwest moved to northwestern Arizona and filled slightly. Meanwhile, an upper ridge began to build into the Pacific Northwest. A stationary front extended from the Great Lakes to southwestern Texas. Precipitation, much of it heavy, covered the entire midsection of the country. High pressure continued to build into the western portion of the nation. Colder air advected into western Colorado, with rain, snow, and fog persisting throughout the area of the Tract C-b during the day. The split flow regime continued on November 4th, as the upper ridge in the Northwest continued to strengthen. Weak upper lows were centered over western Kansas and western Utah. A cold front extended from New York to a low over Arkansas and then southwestward to southern Texas. Precipitation was heavy in a broad band from southern Texas northeastward to the Great Lakes, with many precipitation totals exceeding one inch. Western Colorado continued under a moderate high pressure regime at the surface, although a very weak surface low was centered over southeastern Utah. Middle cloudiness and a few light showers were scattered throughout the area of the Tract C-b. . ka C=¥S% RADIAN corrcernarion The split flow pattern began to break somewhat by November 5th. A strong upper low was centered over Iowa and a very weak upper low was over southwestern Utah. An upper ridge extended from Oregon to Montana, A strong long wave trough began to deepen at about 150°W longitude. At the sur- face, a weak cold front extended southward from a low pressure center over the Great Lakes to Alabama and then into the Gulf of Mexico. An occluded front made its way onto the Washing- ton coast. Precipitation was confined to the eastern third of the nation and to the Pacific Northwest. Weak high pressure at the surface covered the eastern two-thirds of the country. Skies cleared in western Colorado with only a few scattered middle clouds dotting the sky. November 6th marked the end of the split flow regime over the western portion of the United States as zonal flow began to establish itself. Upper lows were centered over Illinois and the Arizona-Utah border, while an upper ridge extended from Nebraska to Minnesota. Precipitation occurred in Texas, along the Gulf Coast, in the Northeast, and in the Pacific Northwest. On the surface, the cold front moved off the Atlantic coast, while the occlusion in the Northwest re- mained essentially stationary. A weak surface high centered in Kansas dominated the circulation throughout the nation. Generally fair weather prevailed in western Colorado, with some scattered middle cloudiness in the area during the morning. A zonal circulation prevailed on November 7th, with a strong upper low in the East and a weak upper cyclonic circulation centered in southern Colorado. A weak upper ridge extended northward from Mississippi to Wisconsin. A short wave moved onto the Pacific coast. A large weak anticyclone [I C-/58 RADIAN corPorRaAricon was over eastern Missouri at the surface. A maritime polar cold front extended through Washington and a weak continental polar front dropped southward into Montana. Precipitation © was widespread in the Pacific Northwest, Texas and its ad- joining states, and in the Great Lakes region. Skies were clear in western Colorado, with a very small high pressure cell centered over central Colorado. By November 8th, an upper level short wave had advanced rapidly eastward to an Idaho-southerm California line. Upper lows were located over Missouri and off the Atlantic seaboard. A cold front extended southward from a low in Alberta,Canada, to Nevada. Precipitation was widespread throughout the Gulf coast states, Texas, and the Intermoun- tain Region. The cold front passed through the Tract C-b region around noon. Cloudiness increased during the day and a steady rain began to fall during the evening. The short wave moved eastward and dug southward on November 9th as the upper circulation began to exhibit some meridional flow characteristics. An upper ridge extended from southeast Texas to an upper high over the Great Lakes, while the upper trough was located on a Montana-Arizona axis. A cold front extended through the northern Plains states and another weak maritime polar cold front came onshore in Wash- ington. Weak high pressure dominated the eastern half of the nation. Precipitation occurred in Florida, the Pacific North- west, and over a large section of the nation's midsection extending from Texas to Minnesota and from eastern Utah to Missouri. Cloudiness covered western Colorado during most of the 9th and light rain fell during the morning hours. The upper flow became meridional by November 10th, as the long wave trough dug southward along a Montana-west LisC-759 res Lei, be ee ee ee te he ee ee ee Texas axis. Long wave ridges were located along the Pacific and Atlantic coasts of the United States. The cold front continued its eastern advance through the Midwest, extending along a Minnesota-Central Texas line during the morning. The cold front in the Northwest began to undergo frontolysis (decay) because of decreasing upper level support. A warm front moved northward from the Gulf of Mexico into south- eastern Texas. Precipitation was scattered through the Pacific Northwest end the Intermountain Region. Precipitation was also concentrated along the cold front in a broad band from Texas to the western Great Lakes. In westerm Colorado, skies were overcast during the morning and some snow flurries occurred, but skies began to break by the afternoon as high pressure built into the area. The meridional pattern amplified on the llth, with a major trough through the center of the United States and strong upper ridges in the West and East. A strong cold front extended southward from a low over the westerm Great Lakes region through the Mississippi Valley to a low in southern Alabama, from which a cold front extended southward into the Gulf of Mexico. Precipitation extended northward along this front in a rather wide band. A large high pressure cell dominated the western half of the nation, bringing clear skies and light winds. Western Colorado likewise had clear skies and mild temperatures on this day. This meridional pattern changed little on November 12th. The long wave trough and western ridge retained their amplitude and moved eastward slowly. High pressure continued to dominate the western two-thirds of the country and precipi- tation was confined to the Atlantic seaboard, Great Lakes, aad Ohio Valley regions. However, a strong short wave began to dig southeastward through the upper ridge in British Columbia, portending a strong continental polar outbreak. EY C-780 RADIAT corPporRaArion Skies were generally fair (high cloudiness) and temperatures were mild in the Tract C-b region. The meridional long wave pattern amplified on the 13th as the short wave dug southeastward swiftly on the up- stream side of the trough. Cold continental polar air streamed southward down the lee side of the Rockies behind a cold front extending from a low in Kansas to Colorado and then northwest- ward to Washington. Precipitaion covered the northern portions of the country. The cold front passed through the Tract C-b region during the afternoon, lowering temperatures slightly. Skies remained fair. The meridional pattern continued on November 14th, although the amplitude of the circulation was somewhat reduced. An upper ridge dominated the West while a major trough covered the eastern half of the nation with cloudiness and precipita- tion. The continental polar cold front continued its south- ward march, pushing into the Atlantic Ocean and Gulf of Mexico by nightfall. A weak maritime polar cold front moved into the Pacific Northwest. The moderate continental polar cold front retreated eastward out of the Tract C-b region during the day. Broken middle and high cloudiness advected over the area throughout the day. Temperatures were mild. The meridional circulation pattern of the five preceding days began a transformation into a zonal flow on the 15th, as the ridge in the West flattened and the eastern trough began to lose amplitude. A weak cool front extended westward from a small low pressure center in Wyoming. High pressure covered most of the nation. Precipitation was confined to the Northeast. Middle and high cloudiness covered western Colorado as mild temperatures continued in that region. i..G- 70d TRADIAAI corRPoORATION Zonal flow re-established itself over the United States on November 16th. A short wave, located ona Minnesota-New Mexico axis during the morning, moved through the center of the nation, causing widespread precipitation throughout the western half of the country. High pressure and light winds covered most of the country. Mild, fair weather prevailed in the vicinity of Tract C-b. Zonal flow continued on the 17th as numerous short waves progressed eastward across the country. Short waves were located in the Ohio Valley (a rather strong system), Texas, the northern Plains, and the Northwest. A weak con- tinental polar cold front was in the northern Plains and a maritime polar cold front moved eastward onto the Washington coast on this day. Precipitation covered the easterm third of the nation as well as the Pacific Northwest. The short waves continued their eastward progression on the 18th. The strongest of these waves was located in the Northwest. The weak continental polar cold front in the north- ern Plains remained fairly stationary, while the maritime polar cold front progressed eastward to a Montana-central California line. Precipitation was scattered through all areas of the country except the Southwest. Cloudiness increased throughout the day in westerm Colorado. The maritime polar cold front passed through the Tract C-b during the evening, bringing scattered showers and a few thundershowers tc the region. The upper flow became a bit more organized on the 19th, with a long wave trough through the center of the United States and minor ridges along the West and East coasts. The maritime polar cold front extended southward from Minnesota to Kansas and then curved into the Texas Panhandle and New II C-762 ER SASS YAR CORPORATION Mexico. High pressure began to build in the West behind the front. Precipitation occurred throughout the eastern half of the nation, in the Northwest, and in the Intermountain Region. After some snow pellets during the early morning in western Colorado, skies cleared gradually during the day, becoming virtually clear during the evening. The short wave trough moved eastward to a Minnesota- Louisiana axis by November 20th as an upper ridge built northward over the Intermountain Region. On the surface, a cold front extended southward from a low over the Great Lakes region to Louisiana and then to the southern tip of Texas. A high pressure system, centered in western Colorado, affected the western half of the United States with its circulation. Precipitation amounts were large throughout the eastern third of the country. The Pacific Northwest also had precipitation. Skies were fair in western Colorado, but temperatures were rather cool. ‘The short wave troughs and ridges continued their eastward progression and by the 2lst, short wave troughs were ‘located off the Atlantic and Pacific coasts while a ridge extended northward from Texas to North Dakote. A cold front and low pressure system were located just off the coast of northern California. Precipitation was confined to the Northeast and the West. High pressure dominzeted most of the nation. The Tract C-b region had mostly fair skies on the 21st, with some scattered to broken middie and high cloudiness over the area. The zonal upper flow pattern continued its eastward progression on the 22nd, as the Pacific short wave system advanced inland to an Idaho-southern Califorria axis. The maritime polar cold front associated with this short wave It C-763 Ss SS Eo ae | RADIAN corrporarion extended from southeastern Montana to southern California by the morning of the 22nd. Another cold front, a continental polar front, dipped into Montana and North Dakota from Canada. Precipitation covered the western third of the nation and the Northeast. Cloudiness increased throughout the day in western Colorado and the cold front passed the Tract C-b region late in the afternoon. A few scattered showers fell during the evening. The upper flow began to change from zonal to meri- dional characteristics on the 23rd. A strong short wave trough dug southward over the Intermountain Region on this day while upper ridges built northward over the eastern and western portions of the nation. On the surface, a maritime polar front extended southward into Texas from a low in Kansas. In addition, a relatively strong continental polar cold front rushed southward through the central Plains states. High pressure dominated the East and the West. Precipitation fell in the Pacific Northwest, the Rockies, and throughout the central portion of the nation. Some snow and rain fell during the early morning in western Colorado, but skies cleared during the late morning hours and remained clear for the rest of the 23rd. The upper circulation became meridional on the 24th as the troughs and ridges amplified rapidly. Long wave ridges were located along the Atlantic coast and in the western United States while long wave troughs dug southward through the central United States and near 140°W longitude. The mari- time and continental polar cold fronts of the 23rd merged into one cold front which extended from the Great Lakes to southern Texas. A weak high pressure system dominated the western half of the country. Precipitation on this day was confined to the Pacific Northwest and along the length of the cold front. II C-764 RADIAN corporarion Western Colorado enjoyed fair skies and cool temperatures be- cause of the high pressure system centered in northwestern Colorado. Meteorological systems moved rapidly on November 25th, as the long wave trough through the central United States moved eastward, as did the upstream ridge and trough. As a result, a strong short wave pushed eastward to a position from Washington to southern California by the morning of the 25th. The surface maritime polar cold front accompanying this short wave extended from Idaho to central California at this time ‘and was moving eastward rapidly. High pressure dominated the central portion of the United States as precipitation was confined to the Atlantic seaboard, the Northwest, and the Pacific Northwest. Western Colorado remained fair throughout the day, with some high cloudiness advecting over the area during the morning. Skies were clear during the remainder of the day. The maritime polar cold front passed through the Tract C-b region during the evening of the 25th, lowering temperatures somewhat. The eastward progression of the long wave systems continued on the 26th of November. Large amplitude troughs were located in New England and on an Alberta, Canada, to Texas axis, while sharp ridges extended from Missouri to Minnesota and northward into Canada and also long the Pacific coast, northward into British Columbia. A cold front extended southward from Canada into Minnesota and from there into Oklahoma, at which point it curved westward into New Mexico. High pressure cells dominated the Ohio and Mississippi Valley regions and also the western third of the country. Precipi- tation was scattered throughout the northern third of the nation. Clear skies and cool temperatures prevailed in the Tract C-b area. It C-765 Thee os RR Oa RE ORS | imate: | E25A DIAM corrPorRation Short waves and upper level lows moving eastward in the meridional long wave troughing pattern were the major meteorological forces on November 27th. Upper lows were centered just north of Maine, just north of Minnesota, and in southern Washington on the morning of the 27th. One cold front extended from the Great Lakes to Tennessee and southwest- ward into central Texas on this day while another maritime polar cold front extended from Oregon southwestward into northern California. A weak high pressure system dominated the Plains states and the Intermountain Region. Precipitation was confined to the Great Lakes region, New England, and the Pacific Northwest. High cloudiness increased throughout the day in western Colorado in advance of the approaching upper low and surface cold front. A middle overcast covered the Tract C-b area by evening; temperatures remained cool. Rapid changes took place on November 28th. The upper low in Washington moved to a position over northern Utah and strengthened, while the other two upper lows over North America also strengthened but remained stationary. Meanwhile, the upper ridge over the Pacific Northwest amplified dramatically, which caused surface anticyclogenesis in southern Canada and the northwestern portion of the United States. The development of this large cold continental polar high cell caused a new frontal system to form from the Texas Panhandle westward to northern Arizona. Cold air streamed southward over the north- western half of the United States. Precipitation, mainly in the form of snow, occurred in the Great Lakes region and in the central Rockies and Intermountain Region. Western Colorado was cloudy throughout the 28th, with intermittent snow showers. Rather cold air advected into the area during the day. Clearing took place in western Colorado during the evening. II C-766 Fe Zi D324 coRPORATION The deep long wave trough and strong upper ridge progressed eastward during the 29th as a transition to zonal flow over the United States began. The upper trough extended from Minnesota to New Mexico while the upper ridge extended “northward from California to Alberta, Canada. The upper low over Utah filled as the trough was propelled eastward. A cold front extended from Tennessee to Arkansas and then into southern Texas. A large cold high cell centered just north of North Dakota dominated the weather over the western two- thirds of the nation. Precipitation, much of it in the form of snow, occurred from the Rockies eastward to the Mississippi Valley and southward to the Gulf of Mexico, and snow flurries occurred in the lee of the Great Lakes. Skies were clear throughout the day in the Tract C-b region, but very cold air continued to affect the area. By November 30th, the upper circulation had changed to a basically zonal pattern. An intense upper low was center- ed over northern Missouri with a strong upper ridge over the Intermountain Region. On the surface, a large, complex low system was beginning to organize over the Southeast while a strong ridge of high pressure extended from North Dakota to southern Texas. Cold continental polar air and high pressures dominated the western two-thirds of the United States. The eastern half of the United States was covered by cloudiness and precipitation. Snows occurred in the Rockies. Heavy snow fell in Missouri, Illinois, and Iowa. Skies were fair through- out the day in western Colorado but very cold air persisted in the Tract C-b region. II C-767 IRADIAAN corporation B. Summary of Meteorological Statistics in Western Colorado during November The area of western Colorado in the vicinity of the Tract C-b had below normal temperatures and above normal precipitation during the month of November. The area ex- perienced five cold frontal passages during November (Novem- ber 6, 13, 18, 22, and 25). In addition, ‘the passace of an upper trough on November 28th brought extremely cold air into the region. Precipitation fell in the area on twelve separate days of November (November 1, 2, 3, 4, 8, 9, 10, 18, 19, 22, 23, and 28). Of these precipitation occurrences, five involved snowfall in the area of the Tract C-b (November 1, 3, 19, 23, and 28). In general, the first twelve days of November had slightly below normal temperatures. From the 13th through the 26th, temperatures were generally near to slightly above normal. From the 28th through the 30th of November, the Tract C-b ‘experienced temperatures well below normal. The region experienced about 75 percent of the possible insolution during the month. Cloud cover (all types, but mostly high clouds) averaged 5.1 out of a possible 10 during the period from sunrise to sunset in the region and 4.5 out of a possible 10 for all 24-hour midnight to midnight periods during the month. The area experienced a total of twelve clear days, six partly cloudy days, and twelve cloudy days during November. Thunderstorms were scattered over the region on November 18th. Grand Junction, Colorado, about sixty miles to the south-southwest of the Tract C-b, measured 1.18 inches of precipitation during November, which is .57 inches above normal for the month. [Il C-768 FADIAN corrporarTion The following is a summary of all official FKUS Air Stagnation Narratives issued by the National Weather Service during November which pertain to the Tract C-b region. These messages were received over the National Weather Service's "C'' Service Teletype Circuit, to which Radian subscribes via a terminal in its Austin facilities. - November 7th: "Gradual flattening of the upper ridge over the Southwest in conjunc- tion with the surface high will result in localized marginal dispersion over sections of California, eastern Nevada, Utah, western Colorado, Arizona and New Mexico today..." "Localized dispersion problems due to weak low level gradients through the interior Southwest will improve rapidly after the morning of November 8th..." ‘. November 13th: "The ridge over the Pacific Northwest is forecast to weaken and be forced southeast, spreading stagnation into the Great Basin and Idaho tonight...stagna- tion in the Great Basin will affect mainly night and morning dispersion conditions." * November 14th: "A short wave moving into Colorado by Friday evening will cause weak- ening of the ridge in the West..." - November 22nd: "In the wake of the upper trough moving out of the Rockies, computer- ized upper level progs show some ridging from California to Colorado by the morning II C-769 | ec) perenne ELA DIAM corporarion of the 24th. This, in conjunction with the surface high and its associated light low level winds, may result in some mar- ginal dispersion conditions in the usually susceptible areas in sections of California, Nevada, Utah, and Colorado during the next 36 to 48 hours. Low mixing heights during the late night and early morning hours will also support this stagnation although trans- port winds will generally be above the re- quired minimums..." IIT C-770 E2ZAISISAD corPoRarion C. Discussion of the Meteorological Conditions in the Monitoring Network during November Cold temperatures and periods of snowfall became rather common in the ambient air monitoring network in and around the Tract C-b during the month of November. Average tempera- tures in the network ranged from 26.7°F at Trailers 020 and 021 in the Piceance Creek Valley to 33.3°F at the 200-foot level of the meteorological tower at Trailer 023 on the Tract C-b itself. Winds during the month were moderate in force on the plateau around the meteorological tower and rather light in the Piceance Creek Valley, where katabatic and anabatic (downslope and upslope, respectively) circulation cells accounted for much of the wind. Monthly average relative humidities both on the plateau and in the valley ranged between 60 and 70 percent. Vector wind directions were southeasterly in the Piceance Creek Valley where the flow is constrained by the. valley walls and south-southwesterly on the plateau, where syn- optic-scale pressure gradient forces normally control the direction and speed of the wind. The katabatic circulation cell continued to exert a large influence on the meteorology of the Piceance Creek Valley during November, althouth the anabatic, or upslope, circulation cell which normally develops during the daylight hours was almost non-existent during the month. The katabatic flow was normally strongest, about 10 miles per hour sustained winds, at Trailer 022 at the eastern end of the monitoring network in the valley. The strongest drainage winds at this station normally occurred from 0100 to 0500 hours in the morning. When northwesterly gradient winds extended down into the valley, they were normally strongest at Trailer 021, at the westem end of the valley monitoring network. IT G-774 cre 6 RADIAN corporation Vector resultant winds for the valley stations during the month were: 1.4 miles per hour from 138.6° at Trailer 020, 1.3 miles per hour from 123.2° at Trailer 021 and 3.2 miles per hour from 108.9° at Trailer 022. The highest five-minute average winds recorded during the month in the valley were 19 miles per hour at Trailer 020 on the 18th, 23 miles per hour at Trailer 021 on the 28th, and 18 miles per hour at Trailer O272-o6m the: 2/th... The highest daily average winds occurred on November 28th. Relative humidities were rather uniform in the Piceance Creek Valley during the month. The monthly average relative humidities ranged from 69.9% at Trailer 022 to 62.6% at Trailer 021. Trailer 020 was intermediate with a 66% average relative humidity. The highest daily average relative humidities during the month occurred on November 21st. Nighttime temperatures once again were coldest at Trailer 021 during November, due to the light winds, dry air, and strong radiational cooling which normally prevailed at this site. The other valley sites also experienced strong radia- tional cooling conditions, but not to the extent that they developed at Trailer 021. On a clear night with light winds, the air at Trailer 021 was normally 5 degrees colder during the early morning hours than it was at Trailer 020, 10 degrees colder than the air at Trailer 022, and 15 degrees or more colder than the air on the plateau near the meteorological tower. It can therefore be said that nighttime temperatures on clear nights generally increased as one progressed eastward up the Piceance Creek Valley. However, on nights when winds were strong, skies were cloudy, and precipitation fell, the streng radiational cooling did not develop and temperatures were rather uniform throughout the monitoring network, from the valley to the plateau. IT C=772 RADPIAN corroratTion Monthly average temperatures in the valley ranged from 26.7° at both Trailers 020 and 021 to 28.9° at Trailer 022. The highest daily average temperatures in the valley during the month occurred on November 22nd, while the lowest daily average temperatures were experienced on November 29th. The highest five-minute maximum temperature in the valley during November was 54°F at Trailer 022 on November 21st. Daytime maximum temperatures in the valley were generally highest at Trailer 022. The lowest temperatures recorded in the valley were -17°F and -16°F, both occurring at Trailer 021, on November 29th and 30th, respectively. On the plateau, meteorological conditions were often somewhat different from those in the Piceance Creek Valley. The diurnal variations in temperature and wind direction which were so prominent in the valley were not of as much importance on the plateau. The diurnal range of temperatures was much smaller within the Tract C-b itself because of three factors: (1) the plateau was not affected by the katabatic circulation cell to the extent that it affected the valley, (2) radiational cooling conditions were not as strongly developed on the plateau as they were in the valley, and (3) thermally induced vertical mixing of the air during clear or partly cloudy days resulted in rather uniform afternoon temperatures throughout the monitoring network. The fifteen degree differences in temperature which existed during the night were not present during the day. During cloudy, windy, or wet conditions, how- ever, the temperatures were approximately the same at any given time, whether it was a meteorological tower level or a site in the valley. Winds were generally much stronger on the plateau than they were in the valley. This can be attributed to the fact that the synoptic-scale pressure gradient force winds which affect the plateau seldom extend into the valley because of the terrain constraints, ime Cower site, in particular; is often Il C-773 PA PIAN corrornvrion affected by very strong winds which are affected only mini- mally by the terrain and its frictional dissipation forces. The meteorological tower continued to monitor some remarkable meteorological effects during November. On days with light winds and little, if any, pressure gradient forces, the winds varied considerably in direction with height and the winds were normally strongest at the 100-foot level. On days with strong south-southwesterly winds, the winds increased in speed by about 25% from the 30-foot level to the 200-foot level and generally veered in direction (progression in a clockwise direction) by about 10 degrees from 30-feet to 200-feet. When strong northerly winds prevailed, about a 20% increase in speed from 30-feet to 200-feet occurred and the winds generally backed in direction (counter-clockwise) with increas- ing height. However, these phenomena are consistent with meteorological rules. When windy, cloudy, or rain/snow conditions existed, temperatures generally varied little with height at the meteo- rological tower, a Situation which is to be expected because of the neutral stability conditions which prevail under such conditions. However, on clear days or nights when winds were fairly light, the lowest 100 feet of the surface boundary layer on the plateau were often decoupled from the atmosphere above it. That is, the ground-based radiation inversion generated during the night often was confined to the lowest 100 feet, with the temperature decreasing with height above that level. Conversely, during the daytime hours on sunny days, the tem- perature normally decreased with height up to the 100-foot level. Above that height, however, an inversion layer some- times existed. On such occasions, therefore, the mixing depth over the meteorological tower site was only 100 feet. This elevated inversion situation was not a common occurrence, Il C-774 EF2.4'DIAM corPpornrion but occurred often enough during November to merit some mention. The average vector resultant wind speed increased with height at the meteorological tower. The resultant speed was 3 miles per hour at 30-feet, 3.4 miles per hour at 100-feet, and 4 miles per hour at 200-feet. The vector resultant wind directions were 202.4 degrees at 30-feet, 189.9 degrees at 100- feet, and 214.0 degrees at 200-feet. For purposes of comparison, Trailer 024, about 1 mile north of the meteorological tower site, had a vector resultant wind direction of 145.5 degrees and a resultant speed of 1.1 miles per hour. The highest daily average wind speeds on the plateau, up to 18.6 miles per hour at the 200-foot level, were recorded on November 18th, while the lowest daily average wind speeds on the plateau occurred on November 9th. The highest five- minute average wind speeds at the meteorological tower occurred on November 25th. The monthly average temperatures at the tower site increased with height, ranging from 31.8°F at 8 feet (partially because of radiational cooling effects) to 33.3°F at 200 feet. The 30-foot level averaged 32.4°F and the 100-foot level averaged 33.1°F. The highest daily average temperatures during the month, 41.2°F to LIEGE, occurred on November 21st. The coldest ‘daily average temperatures on the plateau were recorded on November 29th, with the daily averages ranging from 13.6°F to 1523 Ey. The highest five-minute average temperature recorded at the tower site during the month was 53°F at the 8-foot level on the 21st. The lowest temperature recorded on the plateau was 3°F, at both the 8- and 200-foot levels on the 29th. LG aitS RADIAN corroratrion Relative humidities were fairly uniform over the plateau during the month, averaging in the low 60's at all four tower levels and at Trailer 024. November 3rd and 9th were the most humid days of the month on the plateau, while the 21st was the driest. Solar radiation measurements showed a direct cor- relation with cloud cover, atmospheric moisture, turbidity of the air, and solar elevation during November. The highest hourly totals of solar radiation received at the meteorological tower during the month were 49.20 langleys from 1100 to 1200 hours on November 29th and 48.50 langleys from 1000 to 1100 hours on November 5th. . [I C-776 E2ZAIDI 21 corrorarion VI. DATA PRESENTATION AND SUMMARY This section includes summaries for various recorded data at the monitoring sites. The data presentations indicate the variability of recorded concentrations and meteorological parameters with location and time. In addition, correlation of concentration with wind direction is shown. All data channels except suspended particulates (24-hour samples) are sampled once each second, but recorded as five-minute arithmetic averages of the one-second samples. In some cases, the one- second sampling rate is faster than the time required for the instrument to process a sample; however, these instruments have sample-and-hold circuits that retain the previous value until updated. This averaging technique tends to smooth the recorded parameters and reduce the effects of electronic noise inherent in any electronic instruments. The random noise is present both from the recording instruments and quantization in the analog-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 the ozone analyzer, for which it is 0.5 ppb. Any values appearing in the presenta- tions that are less than the threshold indicate minimal levels and should not be construed as absolute levels because of recording system noise. In addition, averages of the random noise tend toward zero, and any zero entries appearing in the data presentations do not necessarily 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 (g/m*) Pi? / 7 eae | EQLFADIZAA CcorrPoraricon assuming standard temperature and pressure of 25°C and 760 mmHg (1013.2 millibars), respectively. The scale factors required to convert ug/m* at standard conditions back to ppb for the various pollutants are given in the following table. POLLUTANT - TO CONVERT pg/m? At 25°C AND 760 mmHg TO ppb MULTIPLY BY It should also be noted that NO is measured as NO2. No regulations presently exist for NO, and it can be oxidized to NO. quite readily so it is more meaningful to report the NO2 equivalent of the NO. In addition, it permits simple subtrac- tion of NO from NO, to obtain NO2. It also should be noted that total hydrocarbons are measured as the equivalent methane value. II. C-778 FRA IZAADI corrPorarion Table IV displays the quarterly statistics for each monitoring station. All averages are arithmetic except for suspended particulates which are geometric means, The maximum average for various averaging times is also shown. The averaging times are selected to provide comparison to ambient air standards. It should also be pointed out that the maximum l-hour SO, concentration is actually a thirty-minute average. The 24-hour particulate "average" is actually one sample taken from midnight to midnight, and the 3-hour hydro- carbon average covers only 6:00 to 9:00 a.m. For averaging times less than or equal to three hours, the sliding 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. Table V demonstrates the distribution of particulate concentration. For each site, the number of recorded samples occurring in each of fourteen classes is displayed. In addition, the geometric mean of particulate samples at each site is shown. Table VI presents daily averages for all of the baseline gases that are monitored, and for total suspended particulates. The averages are grouped by month and individual location. A blank entry in this table indicates that less than 50 percent of the five-minute samples were recorded for that particular day. (Note: Particulate samples are 24-hour samples.) All concentrations are in micrograms per cubic meter. 1G EM Gomes gi 8 Peele eR | ere | a we. | ERCADIAAN corporation 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 shom. This distribution demonstrates the dependence of high pollutant concentrations upon wind direction. Table VIII, which depicts the stability wind roses for September, October, and November, and the quarter covering those three months, was generated by means of the STAR Program. An inspection of the stability wind roses reveals that of the Bix sstabilityzetassas. VAY. “BAe CY Db, 2 ee atid ete), and "F" stabilities were rather common during the period, while "A" stability occurred only rarely in the vicinity of the Tract C-b. The STAR Program incorporates meteorological techniques and methodologies developed by Dr. F. Pasquill and D. Bruce Turner to produce a bi-variate frequency distribution of six wind speed classes and sixteen wind direction sectors as a function of six separate stability classes. The wind speed classes in this Pasquill formulation correspond to the first six wind speed (or force) categories of the commonly used Beaufort Wind Scale, which was devised by Admiral Beaufort of the British Navy in the early nineteenth century. The wind speed classes in these tables are constructed using knots (1.16 miles per hour) as the unit of measurement. The sixteen wind direction classifications are referenced to true north, with each direction representing a 22% degree sector of the full 360 degree circle. II C-780 RADIZAN corporarion The wind direction and wind speed measurements used in this stability wind rose distribution were obtained from the 100-foot measurement level of the meteorological tower (Trailer 023) on the Tract C-b. The tower wind data was used in preference to wind data from the valley stations or other meteorological sources because that area of the plateau was deemed to experience wind flows which were most applicable to the points of interest in pollutant modelling; terrain factors were also of less importance in the wind speeds and directions experienced at this location, so that synoptic-scale meteorological features exerted a larger influence on the flow. The 100-foot level wind data was used because the wind instruments at this level had more "up" time over the quarter under consideration here. The wind data at the 100-foot level may differ slightly from that at the 30-foot level or the 200-foot level (mainly because of the variability of wind direction with height during periods of light and variable winds and the general increase of wind speed with height which accompanies gradient winds that exceed 7 or 8 knots), but the differences will not affect the stability wind roses appreciably. Therefore, the wind data used here should be considered to be highly representative of the plateau region. The radiation data which made up the other half of the data input to the STAR Program was obtained from cloud cover and ceiling data from the Grand Junction, Colorado, National Weather Service Office. The inputs which combine to determine the radiation index using STAR Program methods are: (1) cloud cover in tenths, (2) cloud height above the ground if a ceiling exists, and (3) solar elevetion (or time of day for nighttime applications). The cloud data from Grand Junction was used because it was deemed to be the most representative data available in the area of the Tract C-b (approximately 60 miles to the south-southwest). Moreover, Et G-78) Keg |: SRS | | FRADIAT CORPORATION since the majority of the cloudiness in this area during the quarter was of the middle and/or high varieties, which are nor- mally uniform in their coverage characteristics and heights over a region while at the same time extending over a large area (a synoptic-scale feature) during their occurrence, the -use of Grand Junction cloud data is deemed to be meteorologically sound. Periods of clear skies should also be uniform in spatial and temporal extent in the Grand Junction - Tract C-b expanse. Some slight variances in cloud coverage amounts could have occurred during periods of iocal storms, low cloudiness, or terrain-induced cloudiness and fog. However, there was probably only a minimal number of such occurrences, so that the stability wind roses are applicable to the Tract C-b region. This method of radiation index determination (use of cloud cover data from Grand Junction) was chosen over the pyra- nometer data recorded on-site because the pyranometer data was not available for the entire quarter. Radian recommends the use of pyranometer data for daytime hours, and the change in temperature versus height (lapse rate from met tower) for night- time to determine the radiation index. This method will be used in future reports. II C-7/82 — —— -_——— - EOEAIDILANM corporaArion _BEAUFORT WIND SCALE FOR OBSERVATIONS AT LAND STATIONS Correspondinz Limits of Wind Speed Explanatory at 10 meters zb. erd. 5 Title ~ ” Specification for Use $$ ——<_——— ea : 3 Mi/hr. ICnots Km/hr. M /szc- Fefecc. i 0 Calntazciece as sisce Smolce rises vertically... ..cecee cee eee 2. eee S mntene) ee — eee “ be ad . ” ‘ . . 4 . 2 & _ - , *@OUPIANDIO JO [BAIIQUT OWTI JO A1BISy a ee ZuyB8erVAy VINUTW-OF - Z ‘Uea_ OfFzqewoeD - J (0:9) | ¢- (CRUST) tals , ‘ ea fareey (SO'T) | -. \ ; fortes lo cusn (os:g)| 5-793 \ i (00:2) ‘ (OT: ZT) é (S79) | Z°9T86€ (00'9) | 6°ISTLT 0° Ec ia sa ZZ/1t €Z/1T A ($0:0) (00:9) ah : suoqied a ae r \ oe ee, LB ra ei ee ie seit a es eS os OI : (0Z‘ST) (00'€) Z 12/01 uoT3e1qUasU0D uoT{earjUsouU0| woTIPAQUaDUODU uot zeazqUs.U0g uotjeAQUsOU0D aSeisAy ao joueieg “uyw-¢ unUTXeY_ "AU-T: wnutxey *2YU-€ wNWTxXey] *azy-g unwyTxeyy *iy-77% whwupXeyl : pepscosy €@ ‘ON YaTival (2a30W OFqnd z9d swvirZ0z9Tu Uz, sUoT IvAQUBOUOD) (72, UAIGNAAON - 7£, UAGNALUIS) AUVWHNS ATUaLUvNd “AL DIAVL /89 -78 LS ae *@OUSIANIOO JO [RAISUT BUTI JO 31PIS, ‘eM, Bupserzoay sanNuTW-OE - Z ‘UBPaY DTAIeMOeD - JT | Si a ee =e 2 | suoqies -oiphy [eIOL sazeTNopy_ieg (Oz! 97): ¢- CATE ; 5 S/Tt os S/1t EB 00 scx (S02). lin. 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Mod Os uot PAqUaoU0D uopAevazqUaoU0] ‘ WOTABAJUaDUND uopAvaqueouo0g uotTaePaquaou0) aseroay zaqecrieg ‘upw-¢ unWwqzxe *AY-T unwtxey ‘AU-€ wNWTXey] *2y-g WNWEXe;; ‘zY-7 wNnWTXeR papz0oey (2930W OFqnd zed suvrzZ019TU UT sUOTIPIQUaDUOD) (72, YAINSAON - 72, YIGWILdIS) AYVWWAS ATUALAVAdD “AI FIEVL 7% “ON BATIVEL / 90 . 4 ( I] E2fRIDTZAN corporarion TABLE V SEPTEMBER 1974 - NOVEMBER 1974 C-b SHALE OIL MONITORING PROJECT SITE 020 021 022 023 024 CONCENTRATION ug/m? >260 240-260 220-240 200-220 180-200 160-180 140-160 120-140 100-120 80-100 60- 80 40- 60 20- 40 (eo) loy fo Noy te) way Oy ie = el f=) fe) fey f=) oie <7) ply E 14 TOTAL iz 18 7 9 GEOMETRIC MEAN So. 2 o23 t B EONS a Ei ¢-791 NO RO Oe CO on SC a Ci tae Pe BE Oy BE rane | | 1 Ee ee ae iE Se aes ae 970 £20 220 120 020 720 €20 e20 120 (“on) SAdIXO NADOULIN 7161 USAKAAON * 7461 USENILIS w/3n) NOILVYLNIONOD JOVUSAV ATIVa IA aTaVvL i 7-792 C I] Cet eee Bnet re CO ee” 8°41 0°O | o¢€/TT ae |B 82/11 Sia | Lz/tt 0°92] OT/TT 6/11 8/11 L/1t 9/11 ¢/tt 9/11 €/1T e/1t T/T 2 ‘os 920 £20 220 120 020 920 £20 220 TZ0 - 020 (ON) SGIXO OIULIN 7161 USAWIAON + 7161 USAWILdAS w/3n) NOILVYINJONOD ZOVUSAV ATIVAG ‘IA ATAVL . 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OPE 61. “02 oO Oba 5 OS tee Ob. ba a ri et. “6 * % * a * # * & 6 ot. 6 6 * » a % % a “ a g & *% * * & a * * * « * % % e * r] 8 & > 4 » * * @ t % * * & * % ° * ® * i * % * rY ® ® =) * * rt * * a % + a ® 4 * ® a Y a cy r 5 ry % 4 ® % & ¥ * * ry ® ® ® 6 » ® & % * * r * Gl2 it - Ot St oi C) Set tt OF. 6 8 l uno (yZ/0C/6 OL pZ/t /6 JOOTYSd @2 = *ON YAW VL (Q#¥W/9N)ZOLIXOIO NADOSLIN 40 NOTLvVIUVA TIvnyntia 9 avr Dk AX “~ seeetrtse »*) wo OO & se V2 51 70 ry wr » 148 179 178 164 188 142 4382 125 £22 419 195 114 114 197 187 1A4 104 143 181 182 102 120 182 103 141 141 102 181 183 $804 186 104 1e 120A 122 173 141 124 1A1 1844 184 102 140 {5 98 88 ft r r w * * ] * «- 65 96 69 98 120 135 837 7o4. 54> f7 wie * 128 Ny ae i Je I ae {27 ™ we ¢ 18 {9 Sad CV Cy PD OY MN OA CU WwW NS 28 Q > a 11, MEAN 7886 TOTAL NUMBER OF OBSERVATIONS 3 * DENOTES A VALID SAMPLE BELOW THE MINIMUM DETECTABLE LIMIT OF THE INSTRUMENT C-897 —_ 9/30/74) PERIND( 9/ 1/74 TO - 21 DIURNAL VARIATION OF sie DIOXIDE CUG/MeeS) TRAILER NO, 3 —_ wa CONMPORATION HOUR ii 22 23 24 MEAN 19 20 2% 18 i7 CS [ats 12 1@ Oo: = Lae 4 e o | © z¢scdk & o es @ —-~egeee#eeetetretrses wz - re | NN w e) w” ae e | on ~y fe, sec. 5d s aQa2eTerertertrrtrtetrresrrrts sts wv ; ~—t wz N uJ ; A _——_ « e- von wo sete £ a *@® nan &eeteotrtketeewrewsesesetets se wv wv - L- @) NI Se i ae 4 ~ _ [ >] ~ e -_ cam oa ® sat & e eon oereewsttttetsette wv - > L 9) we e.™“ x= — so € a al = sset f + eo & QOrwre etie&z#eetete#tfFteEe ETB Se wz = ~ fa os oo z ul 5 Ee - © = a — s223 ¢ od =O ft VTes3stkttesteT«k«& Fears ze wv ul fen) i uw - Lf) = = an \ - 4 wn~ oe 2) >< ot wv es+23 f = +o ze s*eowe@w¢#gegegetetrtreEetiss £ > al © -_ e a | os o LJ 1 cq oc: -_¢ GC Cc LP] zee VTn@MEeEns st Fee etewseernert fw oO @ iii =~ =“ oOo & ww S MN io] = Dao = be] = sa © = we > ~ O.° N set « ow = cet tft te &EeseeTeetRee«aweete wy & u tH = & (r ot wo ~ MN a om ui = WN ww _ mr oa { e - « =z = [ra xv “e*eoetrst & QOseseeteet Fe BPeecreeQ rm Co e oO “ “o) rm CS ,) nN L os ii fal N - aE zm . © <= te é. oa S&S tts GS cs.ete ee ete HBPereeveTs S > - & wt in ~ Ww or ac et nw tu oO me ae LS) a - © i 2) etereies e+ 2ettettker#tTrt ee EN rat ~m uJ @eza S La) | aq = <« CP) > t& us it. ut us @ ett 6 cteeteéc HO Ke KEK KEE EELS & Co = % eae teat @ N a 3 ei ee : te) e*n2es & i" wmoeeeoeerke se ee xeezexea rm oO <= = Vw > Le.) MN -— re N w QO 2 a lw fs wv eect = Ook ££ ht k& Fe KE RK SK AN AN t— Oy re Dn --< 2 fs a z G ce iJ Lae) zest tne © mE F.C S et * £ KEK ES wo 2 i¥ w °> GQ * -V ate GC esRet et wore e ze er_eaxerkr FS Hee MN =y . e Sa cee wh & © ea ¢e¢etette2t ROE DHT A = - -_ - wv 4 < wer. > tu II ¢-899 OQ es Not wet eter eter en et (VCO OA NN ‘Ss »* *9 Ps dp ee oS "et &t Tobe 6} *¢ 2 nd ry NV3W pS C2 22 ANSWNYLSNI JHL 4O AIWIT 37GVL9391L390 WOWINIW 3HL MOT13E 31dkhVS GIIVA VY S3LON30 # *9 s NV3H 6SZ3 8 SNOILVAYSSYO 30 YSEHNN WLOL meeieeive Ore 6 £92 "On fed "9 8% *9 5f SL fe % 4 * ba * % ¢ » % * + a & » 9} s a a % 4 ‘ % vt co * 4 * 6 8s 6 a r rN 4 ry » rf rT a * ry 8 % “ 6 St 9t 9 bt 2b te 6 17-2 ey 2 ee X- : | r a 4 6 & 4 r % 6 r s & » * » r * 9 & 6 reo ce 96) OT “Zio Ot St. Pi Ct 2b Tt Bt uNOH (yZ/00/6 OL vZ/t /6 JQOTHSd fe & - eS (S#eW/9N) ACIXOIO “oe NOTLVIYUVA Iwnunta “9 “9 9 + * @ * * * a ® * om ” * 6 8 Z “ON YSTIVUL A es | ea es ie 2 Ee ” ” 3 » ey ” & % & & * * ey # ~ ~ % oe 36 * + et Cle PA Ss Zt &t @ ® G & 4 YOO —=VOTVMNOOR OGAOKi NMOMNVMODOM ODN VM > mmm nH ® CO MN! O& CG rD iy ' v (UNM ¢€ Oo pO ey wm OO OU Oe er en S wt OF 9 SPE OO Bm 69) O1 ~ ONS wt , © ot (mM WT © eo. G2 &@ &. € Oo VB Q & © - *e 8 asa + eo 8 soar ss x*ess st ss ees 8 os x*ee2s = 2 sf ¢£ es @ 5 5 ae es 2 s¢ tf Sd st ¢ = = * ees @ ad test ¢ + +t 5 ol . a a sf seste + st st2s3¢ ee c¢ez«eR * zs tt tc eee £ se =*t =e * & xs 7 * *ee & + ote 7 e rnin ® ™m™ @ me 9 —_ — ~< 16 16 16 13 11 18. 18. - 18) Lees ts 16 18 253 22 23 ~@e 16 7; isn)6 64). I 16 aS $6 16 ie) =< 16 16 23 22 c ant CaN at ¢e * 8 2 ee ¢ s ef zt = 8 =f 5] = = + bd 5 + = * 5 = 2 5 * s * ad * ft * + oa + ° SA NOW > (NV 26 ™ m Cc Las ie 2% a e¢ DENOTES A VALID SAMPLE BELOW THE MINIMUM DETECTABLE LIMIT OF THE INSTRUMENT MEAN 79814 TOTAL NUMBER OF OBSERVATIONS «a I | U-90Z MEAN ca 02 23 24 49 20 2% 18 Mews) TO 9/30/74) 17 16 LPIDE(UG/ 4/74 HYDROGEN @® pERLOD(C SF o e » i @a) Qe Me oe « ° r e a 6e MEAN 4953 SERVATIONS © re) * Oo RK oO AG Lam cw @.. SULFIDE (UG/M#e3) PERIOD( 9/ 1/74 TO 9/30/74) DIURNAL VARIATION OF HYD! TRAILER NO, = 22 -_ : ; % ee | COCREORATION t HOUR 22 235 24 MEAN 19 20 2% 18 15 13 12 4) DAY , ' —UMVTWNMOOnR OMY —_ -. @& «© & @ a & @ nNOMowernanr wo oi nn ft & ~~ nN an Ss e XO on s - ~ nw 2 ~ ~ nw & bd ~ s n~ wn = 5) ~ ~ # s ~ ~ & OO 2 ~ xn = @ & ~ ni tern 2 Qetranast ect ft a = & es ee & * 2 7 ¢ ee o oOo ~ & “unm vwrwnmwo wm et wvtetact+ ot ot ot i 27 11 ONAawwaAmM TN wt we WO OY OY CU 26 MEAN le | * DENOTES A VALIO SAMPLE BELOW THE MINIMUM DETECTABLE LIMIT OF THE INSTRUMENT MEAN 5887 TOTAL NUMBER OF OBSERVATIONS 28 C-904 *9 *g s 49 ® i | a #9 & “o.- ee *9 *g 9 3 NVBN pe 2% 22 eecet? dv? eee 8 & ANSWNYLENI BSHL JO AITWIT 378VL99130 WOWINIW SHL M0138 JVdWVS OIIVA ¥ S3LON30 »# eoetesst + sceect2r¢ csevrtsests @ 12 682 «COGS eee f 8t (yZ/2@c/6 OL pd/t /6 JA0TYSd CCeen/ONAGISINS NB sees & . 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GS Wi Ca GW o ~ Lp) o> ~ Ont O td eosw mM MD Ni # «8 won NS a r-) 5, MEAN 3531 TOTAL NUMBER OF OBSERVATIONS 28 * DENOTES A VALIO SAMPLE BELOW THE MINIMUM DETECTABLE LIMIT OF THE INSTRUMENT II C-98; es is, ESS OES ceRB ka UcLLwlUlUC ECU Ka we = oeCeee de gO 8 Oo O "8 °O °o. (8 “ea *2 *@ “e@ “a -*o@ “ea *8 “a fa oe NW 3h te pee be 2 6é 8¢ Zé 9¢ Se ve ee wa wrt ot ot 2st et et ot “UNO WVTMOOR WADI AMY OOM AYO NV3W 92 CS 28 Fo BS 6F OF 4b OF Gt wt Sb St TE Bt 6 g rd 9 g v e 4 t YNOH Cpd/TC/Ot OL wd/t /OTI00TY3d 92 * °ON YZ VYL (HdW)Q3adS GNIM 4O NOTAVIYVA “WNUNTG { @ @ NOmMveocUuosd eh ra EM TR. em ’ ’ %, ae i ‘ e DIURNAL VARIATION OF WIND SPEED AT 8 FEET (MPH) re ner | wid ra ae” 29 Fe BLT OD eon a riage PERYOOCLA/ 1/74 TO 19/31/74) 2 23 TRAILER NO, HOUR. 22 23 24 MEAN 19 280 ai 18 17 15 9 yAY e n @& “- o ®& wt ot t=) ot S ts ea eo & OF an we Qu- all Gi « & oer Cb a AOMCTWMON ONG ss Ao Tw | @eueeveseaeoeeesweaacee#r#e New~rs DO Oe? 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PERIODCIBO/ 1474 TO 10/33/74) DIURNAL VARIATION OF WIND SP 22 23 24 MEAN HOUR ii 19 20 21% 13 14 {5 16 17 {8 12 12 ) > <7 MMMmMT-oO THM wt ANMwTAnR OM a J NOMMNRKANO ot wt mnNTONODNOMM ~ TONINIDNRAN GA mrTnnrOoOso TN ; ~ FVM aon | PF WN -_ QmweTFeenw N wan mS NO\/rtertWTo vO OG of -< IO rIN NW T iO os > FD wt nv “ mAUrnmA TA wo wT wt VFTNMONAN _ NN OO © _ NOt NOHO SAN OAK OPM @tN VN A WIN MO —CUMmTWMOoOn OA De VND FTwoWhm CO On AN MO ORO WNOR wot ot 18 20 10 Th i if TOW MW OANA F -s MEAN 8 79 MEAN 3697 TOTAL NUMBER OF OBSERVATIONS & #® DENOTES A VALTO SAMPLE BELOW TME MINIMUM DETECTABLE LIMIY CF THE INSTRUMENT 22 23 24 MEAN 19 28 2% 10/31/74) ‘4-415 “(6-47 496 PERTOOCI@/ 1/74 TO HOUR i@ Nw VFOQOGOOQMRAD"ANNAHMA GFTIN OO ad Ow NO ot ot oe) SBaeoqou arvwe~nN er si MNUMNOTOnR DT Qs Tom AA ONOoge Gee Me DONANNMNMNNOM®D mow A wo we wt ot bd Rica NS SHQEeqanonMm=ntNOHtzsrNDMNAANH aSamoonwoa ed wt Pee "BD OMG OMe TTIVOnrwn TOIOWON AH wt wi wt ~ a 6. 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Be. Ge t€> ce 2 @2= ZI* Z2= GIs J NVAW PS C2 22 32 B2 6 Bt LE OF SE HF EE St TF OF 6 8 d 9 ¢ v ¢ 4 t (pZ/te/ot OL vpL/t /Bt)GQOIe3d €2 © *ON YSN VYL (2P44 930) 18202 OL 108 WONS BONVHD BYNLVYSdW3L @ e@ ikea © virveat Wot DIURNAL VARIATION OF i‘. OXIDES CUG/M#*3) PERIONCLI/ 1/74 TO 11/30/74) = 20 TRAILER NO, HOUF MEAN 22 23 24 14. 15. 16° 17 28-19 - 2eer es 13 19 rm DAY Ss * & +e = — & xk - * eK = * “NVM WOON i ii D CO 17 a2 37 aq 20> 20° >-29 “seo 4A e A A? 34 39 1 4 14 2s / cu RS — WN PD NO A vw i” 13 tO OX 18 15 J an 27 | 12 ak lg i. a g a m~ 13 ju MEAN I ef iW = Se, 16 a4 b— ” z tH uJ ps — ° oe wo Oo — Sd = i _ — ae uj =z a uJ 6 = < — uo w — _ ul _ Cc Ww @ = —J x td HH =. an mi wid oe Se - lids toed zs <= - > oO = uw > w pas a8 ut a fee io we a | wd < = “ = - = = <= = > ee S —t | comet Cc} tis -— Cc tt x II C-1025 ao EQ Kay [ ae | . ko ki. ad orn FF NIYURNAL VARIATION OF @ ccs OX IVES CUG/Me#3) os) CORPORATION — PERIONCI1/ 1774 TO 11/30/74) - 23 TRAILER NO, HOUR 22 235 24 MEA 21 19 20 La. VO “f6" liaise is DAY “=WwW Mm VY Nn - es) ~ © OH 18. @1. 94 -A7. 26 37>. 26246 eo 20a ome 2a 19 17 15 13 Lo 5) 15 —_ w~ Ke) 16 oes) _ 22 21 Ow id ee xnes x zt + * ee ERE * ER EER x Ak kee + ae ee x ot a oe ae + KeeER * eek Es * SRK EK * eK & * x eR ES * VMNMNOnRN CSA set wr oe et on CY SS a A Cu 23 24 6, 7, 12-17 19 24 12 3 3) Q i” 14 i?) 1 11 Ay iy | 27 af 27 21. eae een 38 24 29 15 18 30 2 7» MEAN 7923 O¥SERVATIONS 2 NUMBER OF TOTAL MINIMUM DETECTABLE LIMIT OF THE INSTRUMENT A VALID SAMPLE BELOW THE DENOTES ® II C-1026 22 23 24 MEAN 21 19 20 i4 915. 365 47-18 PERIODCI1/ 1/74 TO 11/30/74) 13 HOUR - 2h NO» NTURNAL ancemen @e NITRIC OXINE(CUG/Me#3) TRAILER ~m pen yee DAY & s2Ftreeeseeeaenee#estrxteeaern esetueutstsetTet¢tttets#«ts oa t oP) © eet eeveeaetnstexerteereeeeeetereerteereee se N N @ *s & rec cee enet Kt eexeerreeeeeertereeereeestse “ La?) — e a 72 ceseezeee8t8teoe et &Feeereerewrreenereeeeee Kee eA E Sea iW N = a e x zs ste ereeteenoztkrFtet et er sCKeeeeeezeeeKtpree e 4 Lol N wa z c Coal es & ete ers niartxkxkereeeorkeeereeeoeretteertenxnx Fs — WN ui ee & - *st se eoezp ee cvretetrtkterzexeeertettekeereentts«* st ot NS - ww Ww oO © sa & * ee Boek eRe KR Kr KT Ke KE CK KT RE KE KTHeEe Ee EK wt - NWN ond x e u _= z+ + cee k&eeezcHowk Fee eKeeereearaeker KeEeKeE KR EX Pod — Zz uj ¢- x lu moO | ie & « iL tut S * © Kee eee oanrnrkwkxeeaex at Se Ke SOR Ee Ee ee NR ee mm Oo at - vTe_e x 4 = © ul <= xeeexe kee EKO OK PEEK HK F FexeexreKkrnKks m9 rn & ie) VIN = = a © Zz ee Nak Fe KH KK KEKE DN HK KEMAH ME x*xekxekexxwxxnx»xK Le) = —" we NW a <= <= > . = SP KORE KR He RD) ek oe Oe Ko a fo ee er i fs i i ek re a - § -_ Mm pe ws Ad uJ CNR ier GE Se I Se er RAN) ee ea, 20 {7 45 11 24 i @) MN 20 20, 21 13 14 yo 4. 28 17 17 i? 36 ts av HP] MEAN MEAN NUMBER OF ORSERVATIONS & 7919 TOTAL MINIMUM DETECTABLE LIMIT OF THE INSTRUMENT THE BELOW DENOTES A VALID SAMPLE * II C-102§ ews Nal av" NIURNAL VARIATION OF . fon NIOXIDE (UG/He#5) PERIOOCIL/ 1774 TO 11/30/74) 28 NO. TFRATLER HOUR i 22 23 24 MEAN 21 19 2a t7 «66 16 15 13 1u CO; > —< =) 11 —NVNM ITI OWOR OO, Vy ia 11 _— ™ on tM a a * 2 =e ® 7s +s 5 I Te ol exe «2 xx *s * * * * * * & Lor) * * * o7) * o>) * Le) 5 © ol * - ~ * * * + ® * a * coo & NW we ru Ww ve i8 19 16 1a ce¢es @ NOM Smad 2 ; a 2 * = * fs * s+ * So) > = o — ~~ Bod + aa *¥ a x + * * = x * =: x oc xD -_ ~ SDH -_ ~~ a2 Smo Smad et Xx: nt Tt 5 ee | KH —< & wt wr i>) an * _ co Oo * fa mn = - _— ™~ S * -— _ ie ©) oO S aS * fe Io © 3» 4. MEAN MEAN 8284 TOTAL NUMBER OF OBSERVATIONS BELOW THE MINIMUM DETECTABLE LIMIT OF THE INSTRUMENT A VALIO SAMPLE OENOTES * tI G-1029 CT 86a 3 cae oa | Basa | rer PERIOOD(L1/ 1/74 TO 11/30/74) OIURNAL VARIATION OF @ sev DIOXIDE (UG/Me#d) 23 « oO Fut 1¢ ee) = - <= re af — 7 1 F) zZ 0 fle qd ff 9 p, f% © vi] HOUR 22 23 24 MEAN if 2 i135 24.43 16.17 248 GLE. Beer 10 a NAY “ON n> oO Ct GN ~“_ —_ {4 WwW) WH “oe ce - .o) 23 24 eee | 19 23 Fe) {2.406 <91 400s 47) is 12 1¢@ 11 13 9 12 14 14 13 16 i » | {4 i 13 2 @] Ow 1¥ 1 a S CO MEAN 2 MEAN 7999 R OF OBSERVATIONS s TUTAL NUMBE I] INSTRUMENT DETECTASLE LIMIT OF THE MINIMUM BELOW THE SAFRPLE VALLIN C-1050 22 23 24 MEAN Sy Ea Gio 19 (20°. 64 18 fin |6|6C6L 3 4/74 TQ 11/30/74) ta; tm ASe SiGe -T7 PERIOOCI1/ HOUR 4 = OY NO, NIURNAL VARIATION OF Je NIOX ION (UG/meed) TRAILER =e bs el sad DAY = Zz wW = —_ ec — ” = - uJ ae — % oe ik S oO e ee eee eee Re KER KKK AE KSEE )hU UF - _ = e " _ ee KR Re KE SB Seer eerer ere nee eeanxr exe eae SS walk z uw e < oe eR RE x £ SeeReERRKR Ree RRR HR KEKE EERE Ee TS Ww = <= — ° iS) a ze ee ex xs dee t eRe Ee B sezs2 G ut — - ww o>) = e a eee ET SRR KEKE HK ® tree eR RK = hs ce = « = tee eke ee KER RE ee K eee ® 2 * © H m 2 ” al 2 = + Oo mo - =x es — Ke RR ER EE ee KR eK RK ee R REP ee RAE Ee DS > Y = w Oo ° Oo aS eee KR RHE KEE Re KR Ree eS RRR RRR KH > («a ~ ts o>. a ee WY Ww eee KR RE KE eee Ke ee Se ec nreeencexe SF Co Qo. 9 = e t& < sR KR HK RE KK RR KE HE eeRR eK eE * xR * S° «a, > 0) > aa e = - ee Ke KT KER HER RR EE x PRK RHR EK AEE SD =! —s <= e oF eR RK RK RR KR KER HE Fe REP RR EK KEE S. So t- iw e ts! ee RR KR RK EK eRe BK KH eRe KR eK eee s e wa Se RR RH KE * eee eR EK cee Ke Re HE K > 2 + e ee XR eG RE KE HX RRR HE KH PeEK RE He Ree D SE S e eRe Ee He eH Ft PERE He eH i. Soae eS oR Se ee ~ z < tu HAUNMOTMCA DAS HNVNMVYRH OR TAS ANMTHWOANDAD = Il C-103] ee tet et ANNA NENA WOO 7 | Nad NIURMAL VARIATION OF 5 Was DIOXIDE CUG/Mee3) ATION was cone PERIONCLL/ 1/74 TO 11/30/74) - 21 TRAILER NO, HOUR 24 MEAN {3° 20 23 22° 28 18 17 oO ecceeeeerkkehec«&ée Vouoe ov eevoeone® ® =e et <= z e«x« £ ze * *2f ent Sd 2s ez ek A es zstx*« 2 es«zt sexes + ** er? « + *s x xr ze xx ¢ x*s2 8 = «sk t e+ +t ft + +t ex z+ = sxx xz * * ee2«x £ * x x Kx ** e+ sex xe ee * +z zest sx xe & eet * * * * *+t+ Se a ee > ke ® x Ket a oe 7x st K sx st Cx A ea bi xs * *- tt + *_* +* ot N 5 V nm won Do — -AV ON st or ot o& NM 'O et ws ~™ & -! On “ > WNW OT AMO VY io) 24 26 24 23 Pe, i7 ‘oO m ce Os ANwWAWN A A -. =~ ) ve de MEAN 7476 BELOW THE MINIMUM DETECTAHULE LIMIT OF THE INSTRUMENT TOTAL NUMBER OF NBSERVATIONS A VALID - SAMPER LOTES OE! * II C-1052 Sey oe) @ - OIURNAL VARIATION OF J OIOXIDE CUG/M*%3) TET PROT eY — ve PERTOOCAL/ 1/74 TO 11/30/74) HOUR 22 23 24 MEAN {6-17 Wai alS -2e 2) 15 id 14 ie 6 N DAY * * x*xektak ke * * x*er eK KK * * es eR EK EF TE KR * + x ecrexnx £ * * * RK EK KR HK K A NMI TOONR OOS 4 ie ie 14 me oO ot {7 cS 19 res oma GW Mr) ON SJ W fw it @, fat] aN 9 » c 3Y 3. MEAN NUMBER OF OBSERVATIONS = 8291 TOTAL THE MINIMUM DETECTABLE LIMIT OF THE INSTRUMENT BELOW SAMPLE ES & NALD ce * NENOT Ti C-1655 ee aq oa Ey fay es be _ ’ DIURNAL VARIATION OF 2... DIOXIDE (UG/Mee3) 1 24 ~a Oe 23 PERIODCLI/ 1774 TO 11/30/74) TRAILER NO, HOUR 22 23 24 MEA! iS UO 47 28 eee ee 14 DAY “aU OT OOM WO oO. ot W 9 IO « — OW N cu NW OW 25 28 29 MEAN BO. MEAN 6863 SERVATIONS OF O08 NUMBER TOTAL OF THE INSTRUMENT A VALID SAMPLE BELOW THE MINIMUM DETECTABLE LIMIT w“OTES DE * II C-1034. — eo, 1 bss Saad AHIURNAL VARIATION or sQtus DIOXIDE (UG/Ma#3) PERINOCL1/ 1/74 TO 11/30/74) = 24 NO« TRAILER HOUR 22 23 24 MEAN iy £68 £9. 20. 23 15 13 NAY 2. esx & = * si i i od ** ext t 5 . i 2 ed zt si 8 * * e+ xizet * = * = se * * * ee KK + + 5 i i i 3 « = * eK * * ere * * xe £ * > ek KR * * eK K * + s+ St & * * ee kK ¥ * me Oe ee NM VIN OR C 9 i -— OW PO roe _ 123 * a \ 16 en 2 5 o7 D 34 MEAN Oe NUMBER OF OBSERVATIONS TOTAL INSTRUMENT MINIMUM DETECTAGLE LIMIT OF THE THE BELOW SAMPLE ¢ . A VALID NENOTES u LE. C=i0 cy fo kg EWG kos kw Ew ag 23 C22 ef ™~ OGEN SULFINE (UG/Me#3) @ DIURNAL VARIATION OF HY ‘ a ‘ed PERTOD(L1/ 1/74 TO 11/30/74) - 24 NO, TRAILER HOUR 22 23 24 MEA 21 19 20 14 45 76 i748 13 16 DAY D ~ DAD oe — oe Qo ww VG & MN ol Tw — | QOS & 2 & sees z2e 8 a a aR e FREER ee x . a a a’ zsz+s x nEeER® * * * *+ * ee + x** Sd zx * x * = x « * x + * x * 5 * = * + *~_ * * * * x & * m OO wt met 26 27 28 ON MEAN Be MEAN 78469 HER OF OBSERVATIONS & » i NU TAL TQ DETECTABLE LIMIT OF THE INSTRUMENT MINIMUM SAMPLE BELOW -THE A VALID DENOTES * EL. Calo: PERINOCLI/S 1/74 TO 11/38/74) N OF 1y¥Qroen SULFINE (UG/Ma#3) 21 HOUR 14 NO. DIUPNAL VARIATIO TRAILER i CONPORATION — 22 23 24 MEAN 16 17 “L8:.49 20. 21 15 13 18 ite) + et HM es Ff ee! * bd 26 34 0 24) «36 38 .o7) 19 11! 1¢ 2 26 MEAN 611A BELOW THE MINIMUM DETECTABLE LIMIT OF THE INSTRUMENT NUMBER OF OBSERVATIONS & SAMPLE TOTAL S A VALID a DENOT * MEAN 25 3M Ea £2 Em Ea ka 3 i. cr N OF 1 Qycen SULFINE (UG/M##3) DJURNAL VARTATIO PERTOOCIE/ 1774 To 247309774) = 22 TRAILER NO. 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SPEED (MPH) 21 TRAILER NO, PERTOOCIL¥ i774 TO Lt /sarras HOUR 22 23 24 MEAN 21 19 29 $2. 2S. 24° 4S “26 “a7 ee | \ DAY N tt {A tat) 6 4 {4 7) ¢ “A mm Ow G) Ss 4) 14%) Y CN w= Pe ot mA A NOV NOCKW OG Ss ~~ nm ONRM ® NN NT LY > SS 2 wt ot Mmm GS AWW. > OU Om Sua Ts 4) 4) (~ rau 3 CM fay =~“WNO TNOOR DM ~“ o ho ot os - “wot yi 4 - CN wT Si Maa 11 0} 2 “4 4) A ”~ vi oO “i 4) a e A 7 ot NPD OA WNW Oe ) toa) NPD c ma Ao) NS © NS n~ «4 oO Le ee) ne) N rr LP) uw % 3 3 wy Or NAS _ ASDVAA st ‘ =eown N73 19 O oO Mm Q mm MEAN MEAN 8155 NUMBER OF OBSERVATIONS TOTAL TI C-105: LI/3SB/7 4} PERTIOOCII/Z 1/74 TO HOUR tf DIURNAL vir en ceouene WIND SPEED (MPH) 22 TRAILER WO, Conronrarion Pte 22 23 24 MEAN {> 20 23 t¢ 23 £6°97 «38 {35 {a NW DAY Senora & S&eeosnoe tn) Saanvwonws & & « oon 1A S > an Sw ow oN es SN oe ON @o mown x ~ S c Ce @) noo NTN —= a: mm a COON x © N © © iS a rm ~ oO ‘ey So co = H a 4) 7 = KNMNYT OCKN DOO HOAWwMTOGSGRS oO “ HAO eMMOna COND SeNTONMS oO wr SWOWDONAAR YD a Sma a«a«eeN LY wo NTA ew HNO eA TAN HY HH nMnamMmom == = 12 DO O “aN as = Nw A i A 4 VJ A a 1 8 SS 3-4 -t N -_ O nm NA WeN . NOso Ww Mmmono MANY Nye 1 TOON 1 f) io a fan CG a ion 2 —_ ra i) a a wt oO @ > 13 14 mw ow 1% 14- Y 1a = oO be) Ee) 1a ton i mee ii oO Si 1A 9 6 MEAN 8321 TOTAL NUMBER OF OBSERVATIONS 28 MEAN — . “o> tom. —_— a > he, Ge el — — eS) ———= ae a =. 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SPEFD AT 209 FEET(MPH) at | PERTODCLI/ 1/774 TO 11/30/74) 23 TRAILER NO, HOUR 22 23 24 MEAN 21 19 28 io 6h 2a 657 ore i2 iu DAY wn © a 14 7 13 » #9 Q he) Ki 1A vv 13 12 1% MN re, ©) ty 12 2 oe 14 “w > 10 oO Al Y) -_ 13 ‘3 “> 6 © aww wn _ 3) ee aX 12 13 co) i) 14 ia ar Nn “w> - 11 12 14 19 13 16 Qa 28 ae) = 19 Ww =D 3 , Ag) 4 NH & wn OG 9 19 12 -4 18 138 413-13 46 48 20 “98 247) 317) ie eee 1¢ > fo ag Le 18 14 2 {5 A 13 4 18 16 19 23 32-32 26 os) ie) mm =A O A 8 Ww Las) 11 =< Fy 14. 616.) fh -1S ir 36 OU ee 2a ee it mo nH Q A O* ~N 12 1% 3 MEAN 2 8, MEAN 8378 R OF OBSERVATIONS = E NUMB TOTAL 1 CeslO5s ck Es ES Ea "ZUT*Gutl*9ot*uot’Zé eet 06 Cth Kd ras Tot Got Le} 22 Gut ect e8 96 BET tet 86 86 ALT 48 c6 Te} Tut vey 16 9ct vg Vee 8k Rot 2 act Cut ett Ore G6 Cet Zot vet 162 Cul Cct OVt 26 gut Tet gut G6 9S 96 a] gut Tet Tut 614 C6 vet get Lud ede c6 C2 e Bg 66 £6 Tg ott Bot bet “ct eee $6 ect cut gg pit wet Gat £6 C6 ect CTt 26 Tet 66 643 Out Zt Zut £92 162% Gat 74 g2t THY Zve cut C6 96 944 cet S872 po pit Gut bt¢e 6uT om § RG 66 26 AZT Vo RZ oe Oe ect 66 Gul pl Lee C62 avS ve “tt Zat Lue tut Out tot put Oct pie 86 6ct Mul 922 cut 16 Gut Crt 96 Ev £28 82 Cot O8 edt To 6uT 66 ¥62 i | °96 Sul 9o Gee cbt 46 69 9eT Bit 61T Gut Let 6uT V6 Wit Tot duty wtt 66 £8 Got 6ve Qt “0g Go Ge 6ut H6 Ev? “Ee 6uF 6t ES Ea bo *btt 3s NW3nW oe as Li Shiv eGR Es pa Ge sye c9e REE GET Poke VEL Lev toe. 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Two types of samples are taken: 1.