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 011 Company The 0il Shale Corporation APRIL 14, 1975 BLM Library p-552A, Building 50 v2 dara) Center Denver Feacra+ ¥ Pp. 0. Box 26047 Denver, CO 80225~ { 0047 veil Gy VIII IX Rote G XI p SIDE I. ie LEE: QUARTERLY REPORT #2. TABLE OF CONTENTS BY VOLUME NUMBER Table of Contents PRE-EXPLORATION ENVIRONMENTAL RECONNAISSANCE SURVEYS A. B. Biological Archaeological 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 8. Aquifer Data - Drill Stem §& Multipacker Tests a. Drill Stemmfests - SG-17 b.: MPT Series 1 - SG-17 GC. MPI Serves: 2 -/SG-17 div MPT Series 3 = SG-17 é. 4 Drish- Stem Tests..- SG-20 fabri Stem lests.-- sG-21 9. Aquifer Data - Pumping Tests 10. Lithologic Logs 11. Geophysical Logs 12. Assays 13. Trace Element Analysis 14. Rock Mechanics 15. Gas Samples C. Air Quality 1. Air Quality and Surface Meteorology . Low Altitude Meteorology 3. Upper Air Studies 4. Visibility 5. Atmospheric Diffusion Studies 6. Radian AQ Data D. Biology 1. Terrestrial Wildlife Studies 2. Aquatic Studies 3. Terrestrial Vegetation Studies 4. Dendrochronology and Dendroclimatology 5. Soil Survey and Productivity Assessment OTHER STUDIES A. Fish and Wildlife Management Plan B. Revegetation Program C. Microenvironmental Program D. Aerial Photographic Study E. Archaeological Studies . F, Scenic Values Program SECTION II C AIR QUALITY The air quality program is concerned with both measurements of atmos- pheric gaseous constituents and meteorological processes which affect their transport and diffusion. Table II C-1 of Quarterly Report #1 summarized data experimental programs in four areas: air quality and surface meteorology, low altitude meteorology, upper air studies and visibility. The fifth area, atmospheric diffusion studies, will utilize a combined experi- mentai, analytical approach. A comparison table, II C-2, reported associated sampling frequency and averaging times for the four experi- mental programs. An intensive, 24-hour "quick-look" at the air quality and meteorology of Tract C-b was conducted on 28-29 January 1975 and is included as reference 8 at the end of this section. Table/Fig. No. Description Page Table II C-1l References for the Basic Data PL €-Z These references are contained at the end of this section. See also Table II C-2. Table II C-2 Air Quality and Meteorology Basic PEC =5 Data Presentation Guide This table summarizes the types of data presented in all the basic references at the end of this section. eC TABLE II C-1 REFERENCES FOR THE BASIC DATA (Contained At The End Of This Section) Air Monitoring Report for C-b Shale Oil Project. October 1974. Report No. 2. Radian Corporation, Austin, Texas. Radian Contract RC #100-056. 8 January 1975. 211 p. Air Monitoring Report for C-b Shale Oil Project. November 1974. Report No. 3. Radian Corporation, Austin, Texas. Radian Contract RG #100-056. 23 January 19752 ) :250' p. Air Monitoring Report for C-b Shale Oil Project. December 1974. Report No. 4. Radian Corporation, Austin, Texas. Radian Contract REsi100-056. ) 4° Marchel975 a7219Np. Quarterly Report. Air Monitoring for C-b Shale Oil Project. September 1974 - November 1974. Radian Corporation, Austin, Texas. Radian Contract RC #100-056. 24 January 1975. 390 p. Upper Air Studies Over Federal Oil Shale Tract C-b During Winter 1975. E G & G Environmental Consultants, Albuquerque, New Mexico. Contract No. 66123. Report No. AL-EC-117-. 14 March 1975.) 101° p: Upper Air Comparison Studies for Winter 1975 Between Federal 0il Shale Tracts C-a, C-b and Grand Junction, Colorado. EG GG Environmental Consultants, Albuquerque, New Mexico. Contract No. 66125. Report. No. AL-EC-116. 14 Mareh 1975. 190 p. Air Monitoring and Analytical Determinations of Volatile Trace Metals at the C-b Tract. Sampling Date January 27, 1975. The 011 Shale Corporation. Laboratory Data Letter ..75-235. February 6, J97>. 0) ep A 24-Hour "Quick-Look" at the Air Quality § Meteorology of Tract C-b. 28 January - 29 January 1975. C-b Shale Oil Project, Denver, Colorado 182. pi: An Analysis of Air Temperature Inversion Characteristics of the Piceance Creek Basin, Western Colorado. William Marlatt and Associates, Fort Collins, Colorado. Report No. 1. March 12, 1975 ilps TEG=2 OD “£0 “VHD “DHL “SCH ‘¢os yquou oy. 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Sulfur dioxide, hydrogen sulfide, and suspended particulates are re- quired to be monitored at all stations. Hydrocarbons, oxides of nitro- gen “and other pollutants” are also required to be monitored as dir- ected by the Mining Supervisor. The required air quality monitoring system was completely operational as of 1’ Novembcr 1974. Subcontractor (Radian Corp.) data reports for air quality and low altitude meteoro- logy have been furnished through December 1974 as of the cutoff date Greze Leviuany elo7s ton this quarterly progress, report. Fisure: 1) (Cal of Quarterly Report #1 shows the locations of the 5 air quality trailers andsthe iIeteorologicar tower. Trazliers 020, 021, and 022 are located in the Piceance Creek valley at Redd Ranch, Rock School and the Gerald Oldland Ranch, respectively; trailers 023 and 024. are on the tract at the meteorological tower and on the ridge between Cottonwood and _ Sorghum Gulches, respectively. Table/Fig. No. Description Page Table ll C-3 Air Quality Summary, Trailer 020 LrG-§ This table summarizes air quality data maxima from Ref. 4 for the quarter (September, October, November, 1974). Datastoueeranlers, 021,022, O25°follow. Table Vi of Ref. 3 gives the daily average concentrations for the quarter. Table II C-4 Traaier 021° - II -€-9 Tables L1-C-5 Tranter 022 Ti G=10 fable Wl C6 Trazler 0235 WF Ca). able Lr C-7 Trailer 024 TE °C=12 Table II C-8 Particulate Concentration | Distributions I C-i13 This table summarizes the trequency distributions of particulate concentrat1o1s along with the geometric mean concentration. Basic data on air quality and surface meteorology are contained in References 1 through 9 at the end of this section. ise -7 (S0:9T) 0€/6 (S21) Lt/ot LOFQRIIUIDUOD "UpPUeg GNUyXEK U0FZBAZUIILOD "2U-T umupxey (pli *sAep aSOu LOF eJeEP SJOTdwoOsuU BEWIXeW PUS SSCLOAG [[PLDAO 9UY UT Po DOTFo1 Jou o1 | x 0°€z02 S°L78T \ ($0'9T) "1/6 " UOFIeIQUISUOD UdOTSZPAQUBIUOD uUdFZPAQuI UND "2YU-E€ wHUzxE;] "2U-g WNUPKeyK "2-47 UnuTxey? (1e2a DtqnD tod swerSo01dTW UL suoT}e12US9U0D) HENAN - pL. WAGWLdaS) AVWWWNS ATUALUVNO ¢-D II FTEVL 020 ° eit z os Reocacace DIpaOoue MS TLVEL 3-8 Lh *sAep 9S0Y} 1OF Blep oJaTduODUT 02 aNp paqus0do1 Q . , EUTXEW PUB OORLOAR T[BIOAO SY} UT Pa}DO[ Jol JOU die Sup uIlt}1o) ~ - > *@9UsIANIO JO TVAXIQUZ OMT? JO JxvISy, ‘aut, ZuzIerzsay esnuzH-0€ - Z ‘uBeeN D7Azd9TOaD - Y UoFIBAIUIDU0D *2U-[ unuzxex uoTZraquadU0D "AY-E wHuypxeyy UdFIBAQUDOU0) "24-9 UNUTXe, UOFAeAQUdDUOD "AY-7% WNUTXey 1ZO “ON S3TiveL (19,aW DTqny sod swe1zZo01dT~ UT sUOT}e12UaDU0)) (vL. UTGNAAON - vd. 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UTGWAAON - 2, WIGNALdIS) AUvAWnS ATHALUWNO 9-9 II ATEVL = sil , 4 Linc “skep asoy} Loy ezep ojeTdwodUT 0} onp pez10dceL BWIXEM PUL OSELOAR T[BLOAO OY} UT Po ETJoL ZOU o1v SAPP ULUILOD x *goueTANIIO JO [EAAGIU VU FO 4202S, ‘OU, BuyZeroay 9InuyR-OL - Z ‘uve DFI99C005 - T pee | Beas Se eS Aa o7ect ye €2 “% Sose[Noz,3sed ——————| (COs ae (0S) (StS) : Woes: . z St/Ote ee ne Shalini alloca aloe) mae | eeior | 2 dR ie os Ce eg ea as Pe oe eae eS ‘ woFIBAIWUIIUOD - yotavzzua.U0y uop erzyUasU07 adezaay zazeseseg "2U-€ WNWEXE}Y "2Y-g WNUPKeER "2y-h% WAUTXBY ‘ papacoog uwoFzerIUIIUOD *ay-T unuytxeyX yozses3uaIIU0D “UpW-G BNOPXeK VZO “ON USTIVEL (x019W DTqnp 10d swesZo01DTW UT SUOTIeIJUDIUOD) (pL, WIGNSAON - v2. WIGNSLdaS) AUVWNS ATMALUVNO «L-D II FTAVL ) he =i JG hast 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 <20 | TOTAL (No. of Samples) GEOMETRIC MEAN (ug/m3) 8.2. TABLE II C-8 FREQUENCY DISTRIBUTION OF PARTICULATE CONCENTRATIONS SEPTEMBER 1974 - NOVEMBER 1974. C-b SHALE OIL MONITORING PROJECT 20 O21 022 023 024 CONCENTRATION 2 1 0 0 0 0 0 0 0 1 0 0 0 m0 0 3 Lege 4 0 14 5 5 9 18 rh ae 9 % "8.3 11:3 LORS @ ecOGh a * Certain days are not reflected in the composite reported here due to incomplete data for those days. II C-13 Subsection II C-2 LOW ALTITUDE METEOROLOGY The lease stipulations require a meteorological tower to be esta- blished in reasonable proximity to the plant site to monitor, at least 95% of the time, wind direction and wind speed at three levels, one at least 100 feet above the surface, one at approximately 30 feet and one at an intermediate level. Temperature is required at two levels, one at least 100 feet above the surface and one at approxi- mately 30 feet. Humidity is required at one level. Low altitude meteorological tower data are obtained at 8', 30', 100' and 200' for wind direction and speed relative humidity, and temper- ature. Barometric pressure and daytime solar radiation are obtained at ground level. Temperature differences are obtained between the 30' and 100' levels and between the 30' and 200' levels. Basic low altitude meteorological data are contained in Refs. 1 - 4 through December 1974 (as for air quality) at the end of this section. Wind roses by atmospheric stability class are presented in Table VIII of Ref. 4 for the 100' level of the meteorological tower. Table/Fig. No. Description Page Figure II C-1 Wind Rose Diagrams Piec-15 This figure presents wind roses for the 100' level of the meteorological tower for September, October, November 1974, and the quarter. Th C-14 FIGURE II C-1 WIND ROSES AT THE METEOROLOGICAL TOWER (100') re her bl Mt QUARTER NOV. ie e- 1S Subsection II C-3 UPPER AIR STUDIES There are no requirements in the lease stipulations for upper air studies. They are required in conditions of approval from the Mining Supervisor. Two winds-aloft and temperature profiles per day to altitudes of 6000 feet above the tract are required for a minimum of 15 days per quarter. Data for this reporting period were obtained by E G § G consultants for the wind and temperature profiles during the 15 day period from January 20 to February 9, 1975. Winds aloft were obtained from pibal releases at the meteorological tower; temperatures aloft were obtained via an instrumented aircraft. These data are correlated with the C-a Tract and with Grand Junction. Basic data of the types indicated above are presented at the end of this section in References 5 and 6 by the E G § G Environmental Consultants. In addition to the above instrumentation, an acoustic sounder was installed (but not required) at the meteorological tower location by Wm. Marlatt and Assoc. (consultants) on December 7, 1974 and became operational as of 2 January 1975. It is used to assist in assessing atmospheric stability by determination of the height and time-extent of unstable layers and stable layers, including inversions. During the ''quick-look" investigation (Ref. 8), atmospheric stability was assessed by seven techniques: 1) temperature - altitude soundings 2) temperature differences on the meteorological tower 3) wind speed 4) solar radiation index 5) standard deviations in the horizontal component of wind direction 6) standard deviations in the vertical component of wind direction 7) acoustic sounder PIVC- 116 Subsection II C-4 VISIBILITY There are no visibility requirements in the lease stipulations; site visibility measurement are required in the conditions for approval by the Mining Supervisor. A joint proposal request with the C-a Tract is currently being prepared. I (Cay Subsection II C-5 ATMOSPHERIC DIFFUSION STUDIES There are no requirements in the lease stipulations for atmospheric diffusion studies. Conditions for approval from the Mining Super- visor require X/Q estimates for 24-hour and 3-hour averages. These studies will be initiated at a future date when stack emission data become available. An assessment of atmospheric stability will probably be required for input to diffusion models. This assessment has been initiated and is reported both in Subsection II C-3 and in Reference 8. IIT C-18 RAD TAN ayo SPF Ae an AS ae Gos AL Ls & RC#100-056 ATR MONITORING REPORT FOR C-b SHALE OIL PROJECT OCTOBER 1974 Report No. 2 8 January 1975 Presented to: C-b Shale Oil Project Suite 555, Two Park Central 1515 Arapahoe Street Denver, Golorado 80202 Attn: Mr. Max Legatski Prepared by: Radian Staff E19 8500 Shoal Creek Blvd.’/P.0. Box 9948/Austin, Texas 78766 /(512)454-4797 E221 DIM corPporRarion EE: DLE Vals. TABLE OF CONTENTS GENERAL DESCRIPTION OF AIR MONITORING SYSTEM DESCRIPTION OF INSTRUMENT SYSTEMS A. Air Quality Instrumentation Calibration Procedures B. C. ' Data’ Aequisascion Systems... 5 See De Meteorological Instrumentation METEOROLOGICAL AND TERRAIN FEATURES OPERATING TIME ANALYSIS FOR EACH SITE METEOROLOGICAL SUMMARY A. Summary of the Major Features of the Upper Flow Over North America B. Summary of Meteorological. Conditions in the Tract C-b Region “ee eee eeee oe ec ec ee ee we ee ew ewe ew ore eeeee eee e ee @ 8 @ coeeer ee ec C. Meteorological Discussion of Tract) C=b and the Piceance Creek Valley DATA PRESENTATION AND SUMMARY Monthly Averages Dahl y“AVeraces., 5 ote shyeie Sheotkilew ots seine eae Maximum Five-Minute Averages and Time of Occurrence Maximum Independent Sliding Averages..... Functional Dependence of Recorded Parameters Upon Wind Direction ee @ 46.0) 2 © se) 8) te 6 Diurnal Variation of Recorded Parameters APPENDIX A - STABILITY WIND ROSE DIAGRAMS II C-20 eeeeeeee cere eee ee “ee e © © © @ @) [e' (e © 6 © @¢s oeee er ee © SB: oe: 'e ene ‘e.ce0 8 Page Il Li 1B Ie Ly eh 1 EI Mt It iat Ha Et BEG II ah IJ iT 1a Tey Coa C=25 G=25 C-24 C-26 Caan C-36 C-41 C-48 PFREADUARY corPoRATION re. GENERAL DESCRIPTION OF AIR MONITORING PROGRAM Radian Corporation, 1s) under contract to C-b Shale Oil Projects 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. i eat eres Soe | WOSSSUCKII o/V ee rn ee RR ER RT NR EAE 8 OS A LIT Ok RO ill Fl it A | mE i= 22 PEee.Ee Uk corranmnries EE DESCRIPTION OF INSTRUMENTS SYSTEMS A. Air Quality Instrumentation Nitrogen oxides are measured with a Meloy Model NA520 ‘ analyzer. This dual-channel analyzer is based on the chemilu- minescent principle, and continuously monitors both NO, and NO. A subtraction circuit in the instrument provides a continuous NO2 output, but is not used in Radian's system. NO2 is cal- culated once a second by the computer by subtracting the NO value from the NO, value, thus avoiding any drift which might OCCiUGrin, the -NO>, OUEDUG Of —Ehe sanstrument. This instrument has a maximum detectable sensitivity of 5 ppb (parts per billion), and a linearity of 1%. 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 H2S-1 hydrogen sulfide Sserubber. The Model SAI85 is a continuous analyzer, and utilizes the flame photometric principle of operation. The minimum detect- ablewsensitivaety 12s 85) ppb, and the limearity is 217. Ozone is measured with a Meloy Model: 0A350 analyzer. This instrument provides continuous measurement of ozone, and is based on the chemiluminescent principle. The minimum detectable Sensmiivity 16/025 ppp Vand then linearity, 1s. a7, . Total hydrocarbons, methane, and carbon monoxide are monitored with a Bendix Model 8200 gas chromatograph analyzer. This instrument uses a plume 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. Tim€-25 POCA corrarntian . 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 limes sto tne instruments are connected. All joints in the sampling system are secured by G-ring compression fittings. The manifold is contained in a heated (100°F) chamber to prevent condensation of moisture. The teflon lines from the manifold to the ansexa— ments are insulated with 1/78" wall thickness cubber 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. B. Calibrations Procedures Each trailer contains a Meloy. Model) RAD-l) calipieatzon unit. This instrument provides a zero air supply, SOs span gas from an SO2 permeation tube, and NO span gas obtained by pre- cisely diluting bottled NO spam gas The calibration, of alia struments is automatically performed once a day, and is controlled by the computer. Each instrument isafixst ‘swatched toezeno, amd 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 TiG-24 ann. Ya) AI TAA Re are Sf EDALALG cermpaornaria: obtained 24 hours before, and if a drift in excess of l0ppb has ecem-sedhvamvexcess, Zen@ drt Tmeht for the channel in question iS seuLned On One Ee, System otatusyPanel: Next, Span gas is supplied to each channel and the computer decides when a stable span value has been reached. This value is recorded and compared to the pre- vious day's value. An excess span drift light on the System Status: Panel: usturned om ah a drifktsexceeding 10ppb occurs. The instruments are then returned to the monitor mode, and after two minutes the computer resumes data taking. The bottled NO gas used at each site was obtained from Precision Gas Products. Pre-purified grade hydrogen is used in the SO. analyzers. The SO2 permeation tubes were manufactured by Metronics PASSOClation,, ine. | “Thermvourput 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 Model OA350 ozone analyzer has its own calibration system which provides a zero check and a span.check. The ozone Calabration System is) Verified iby .compazuson te: aycalibrated 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 obtaincd 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 Meciane channel. = LhesModel 6200 sus zwerocd with arr froma Ii C=25 => EVENTS ia od Sen mat eee CSR ESEAALG cerrecrarion Bendix Model 8834 zero air unit. In addition the instrument is electronically re-zeroed at the start of every five-minute cycle. The Hi-Vol particulate samplers were calibrated using a Calibration Kit from General Metal Works. GC. 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 wsec 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/outpul unit) fon the system is Texas Instruments KSR 733 Keyboard/printer- | sais 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) recordimg.. Ihe power to venesreke— 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. TIG-26 > Hour sol thc anbrent vale monttorimg) trailers: are equipped with the following meteorological instrumentation: (1) dry bulb Eemperatuce (ourside), (2) selativeshumidity, (3) wind direction, (4) wind speed, and (5) a tipping bucket, heated rain/snow page. 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 Numkdity apparatus’ Cin the aspirated radiation: shield) are all mounted atop a 33-foot crank-up meteorological tower (the WiM-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 Syskeem whlch Obners he opeimum=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 Eeceiver 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 tachometcr is essentially free ssrom maintenance with a, life of well over five years when operated continuously.’ ‘The specifications of the W103 Cup Anemometer are as follows: eC 2,7, Accuracy: + 12 or 215 mph, whenever is greater. Bearings: Sealed and shielded precision Stainless “steel, thresholid:) “OJ miles) perm hous DustanicenCons canted sos Geer The wind vane, the W104-2, is equipped with a 1000 ohm low torque potentiometer and two wipers for 0° to 540° operations. The response characteristics of this vane are: Dead Bank: 0 degrees Damping Ratio: 0.4 Distance Constant: 3.5 feet Threshold: 0.75 miles per hour POtentiometer Linecard ty. Oar, 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 AC=26 element. Its expansion and contraction positions the suspended cone of a incase variankes differential wteransformer (LVDT). - The absence of friction inducing linkazes and wiping contacts minimizes Dy Ste resi swand aimpmovyes accuracy ihe LVDIvoutput sienal ,: when processed, yrs diwect ly proportiond’ te relative humidity.” The Specit1cCacrvons Om) Enis aAnstrument are as) follows: Range of Indication: Of to 100% 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. Accuracy: 5% - 15% RH; + 5% RH Seo Dio RM te Lean 95), ~L0O07, Ri; 2.37% RH A + Signal Output: Analog signal of -150 mv. to Tio Onive ween elecebricall zero atmo0, RH is standard. 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- Eabie from 0 tomo5 Ofm Snow falling into the inllet funnel is melted, The resulting watem (from rain.or snow). drains into a precision tipping bucket mechanism which activates a mercury ewiechaeach time thebuckes filissand tips. The: gage is constructed IC 29 @ of durable corrosion-resistant materials to provide many years of service. The specifications of this gage are as follows: Orifice: 46 inehes Calibration: 0.01 inch Accuracy: ‘0957 (Calabrated atr0.> amy ha - Sensor: Chrome plated exaeune buckets Switch: Mercury, 07 second) clhosunme Heat Control: Thermostat adjustment, Oto 25 2G: & 2. 200-Foot Meteorological Tower The tower has instrumentation. ate fous. levels: oseem 30 feet, 100 feet, and #200 £eets “Atlally four Hevelse stehemerance: 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 30-foet jto L00-footr Vayereanderne 30-foot to 200-foot layer. In addition, this site has 2 Precision Spectral Pyranomeres,. 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, Imc. (MRI). ‘This sensor has a 540° potentiometer for wind direction and a light chopper for wind speed. This senson is rugged, with an all-weather coaxial cup and ir e=50) Fe/fS CEL ecomrcrertsci damped vane assembly. The prototype model has been in operation for years under the most demanding weather conditions, performing Continuously wi Caehiesmemost meliabriaty.. 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 Inxceshold: 0575 mph Response Distance: 18 feet (63% recovery) Flow Coefficient: 7.9 feet/Revolution Accunaey- =) 230-4 mph, On) be (Whitenever is greater) Range: 0-100 mph Wind Direction Stamteing whreshold-| 07 75¢mph Delay Distance: 4 feet (50% recovery) Damping Racoon | 0% to 076 Accuracy (540° system): + 1% Range: Or Mee, S40 Ges ® 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 640 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 vair.) Si@isceui ation 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 Cyto 3010 Humidity Accuracy: §223. 07, Ri Range: 0% to 100% Relative Humidity Measurements of temperature difference are taken for two oe) layers, the 30-foot to L00-foot Payer ‘and ‘the 30)- foot to 00- foot Linc=32 bivd cncsmeterd, tu CORR ORATION layer. The thermistors and circuitry used for these measurements are separate from the thernistors measuring air temperature. The usc 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 ise LumecmMeatLonm are as follows. - Accuracy: + 0.1°C --/ Range of 74E 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 oad with. %'" ‘oficadral ace per ELA 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 paoundeicits. and one Yeanchor 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. Theysienals fromethe tower instrumentation are fed from multiple signal cables into transmitters mounted at the base of Gass we roe Vitale d CONDORATION 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; ihe 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 clements. The signal cable is run underground in PVC conduit in order to minimize damage from the weather or various rocents 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 PO1L-E unit by Weather Measure, with characteristics and specifi- cations as deseribed in Section 1 The barometer 1s themp747 Analog Output Barometer by Weather Measure. This barometer provides an output voltage thet is linearly proportional sto) pressume wine specifications on this instrument, which is mounted inside the monitoring trarler at the site, are asi follows. - Range: Specially designed for the 100 mLliltbar “interval, from 7/25 /moblabaccmee 825 millabars® Resolution: Mintinmee Linearity: = 0.5 mil libarssoversthesi00 Mil libaw antwernval: 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 PEG s54 Sy fe PANS fm PAE Sys = + ~ Fe DIALIN corporarian eliminate the effects from all outside influences, such as BeRLechLon OF Shadows, Onrthe pyranometer. The instrument characteristics are as follows: Sensisgivaty.:, Samy. per call/em*/min - Independence: 300 ohms Temperature dependence: Sensitivity constant to within + 1 percent over the ambient tem- perature range from -20 to +40°C Lineariey-:) Response Linear wp to intensities of 4 cal/cm’/min «4 Response Time: 1 second (i/e signal) All) instrumemterion is factory calibrated and is field- Galibrated at various amtervals. Sling psychrometers ane 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. me C-55 ney KER PO Fe PA PT - : C/E ESEAARS ConrrcraArion Li. 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 unzés jinvehne Pieceance 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 School 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 ttself, ihe lareece gradients in elevation in this area, of course, occur at the Piceance Creek Valley walls. However, the northern valley walls are slightly steeper than those at the southern boundary of the valley, which then slopes upward gradually toward the C-b Tract. The Piceance Creek Valley decreases in elevation from east to west im this area, so that nephttime katabattcmcola. air drainage flows advect from east to west, or from Trailer 022 to Trazier O20) co: Trailer: 021 As mentioned at the otttset of this discussion, tne terrain will have a large influence on the meteorology of this region. Considering first Trailer 022, at the eastern end of the monitoring network, a nighttime katabatic (valley or down- slope) flow will exert a’ tremendous influence on this site. LLEG=56 a ae : ERA ECE SAS corponnrians Of the three monitoring locations in the Piceance Creek Valley, Ehis site has theysteepest. vatley walls in its vicinity. As a Eesulty, Ehe nighteimeykearabatic 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 hour. 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 Guich, 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 Trailer O27 to Trailer i020, sosthat channellingserfectsaare not quite as great at this location. Nevertheless, a well-developed Kkatabatic-anabaure ilow cycle arfectsr 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 directions 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. PieG= 3h PS TAR FA ‘ si abvivcbhsbd CGRPORARVEDSS 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 lights) 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, 100 feet, and 200 feet. The top level of the tower generally remains in gradient wind flow. That is, the winds at that level are normally generated 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. LI G=58 PRLRESEALDY corrorarrorn Trailer 024 is between the Piceance Creek Valley and the meteorological tower location, about 1 mile south of the valley pa tselt. = ihe elevattonyen) this Sitesis 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- Inauced Elows 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 duy seharacten Of senewais in this portion of 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 Daseiewlar ss the drainage effects will be spectacular at Trailer 021, which will often experience Pe C=59 “APTN SH\ESEELEY cerrorarion 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 Smgthe azea Of iuaiten. 02) 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 ground-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). Pr G-40 P22 PAY CORPORATIDY IV. OPERATING TIME ANALYSIS BORSEACH SITE ahi ON EACH SITE This section presents the operating statistics for each of the major subsystems contained in each monitored station. Table II shows the Specific number of hours that each of these subsystems was inoperative for the month. The column labeled COMPUTERS Windicates tthe entire data acquisition System and downtime hours appearing in this column and,. therefore, means Eotal, tosswor data) These instances include, in addition to computer downtime, power failures, no power available, and self-automated shutdown periods such as during air conditioner malfunctions. . Calibration time is not considered to be downtime and is, therefore, not included in the downtime figures. The amount of time used in calibrating the instruments is Sliven at the bottom of the downtime analysis table and is Reported as ‘total calibration hours for each channel for the entire month. As is evident in the calibration figures, channels can be calibrated independently of one another. No calibration time is given for particulate monitoring since Hi-Vol calibration occurs infre- . quently and only during the off-duty cycle for each Hi-Vol while another Hi-Vol is taking date. 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De C47 RRAECEAALY eerPporarion NF METEOROLOGICAL SUMMARY 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 1,4, 7, 1237-135 222) 23,ancercae The flow was generally meridional (north-south) on October 2-3, 5-6, °9; 14-21, and 25-26." Split upper»level flow prevartledton October 8, 1LO-ll1, and 27-31. The net results tof vthese ecm. 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 the 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 generally 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 [IT C-48 E2CAES IL. 3 eccrrPorarion 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 coast 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 Souen from thesesto Kansas. On October 6th, the northern half of the long wave which had been over the western United States was reinforced and moved Ti G-49 Fe;,EaAARY ecorrcrarion 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 PFE 50 RAL EARY ceorpPpcRATION 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. Thevsheort 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 northerh 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 halt vol 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 ris¢—5i FEAR TAARY corre rarion 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: clicarned 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) om) thaseday. 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 Colorado 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 fi .G-52 pel Sold cemmperarion 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 halfvot the matilen on the, 18thwand 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 imathe 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, Tl G=55 RADEAN corrcRrRarion 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; Uarted States to become stationary. Precipitation was scattered along this front from Texas eo New, vouk, » 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 meridional characteristics by October 25th, although the flow was beginning to show splitting tendencies once again in the western United States. An upper ridge extended northward from Colorado through Montana 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 Washington and Oregon and through the center of the nation, along a cold front which extended?from Texas “to the Great Lakesomarmld temperatures and clear skies prevailed in western Colorado. IT C-54 ESS LESELih’ corpPorarion Cloudiness returned to western Colorado as the short wave moved eastward from the Pacific coast on the 26th. Pre- Ciplitativon was restricted ito 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 preci plLtatilon. 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 C55 FReAEDIA ecrpora;rion over central Utah. The surface low had meanwhile moved to eastern Colorado and weakened somewhat. Cold frontal passage occurred late onsthe 29th in western Colorado... By the morning of the 30th, 1t 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 3lst, 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 iract (C=b KReeaion 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,.5,.100 Ye a20) 24. sand 29) abe strongest 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 3355, 10n lie 2? one 27 23 2 ope oe 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 Sst but TT G>56 E2A\ESEARIN] corporation snow amounts were rather light and melting occurred within a few days. Temperatures were below normal during the periods from October Srd through) the 7th and October Tlth 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 i7eh 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 tovwsunset duane Oetober;, and 4:9 out of a possible 10 for all possible observations during the month. The region experienced 1@ clear days, 9 partly cloudy days, and 12 cloudy days during October. Thunderstorms were in the area on two October days mOctobers 10th and. Lith) eGrand Junction, Collorado, about 75 miles to the southwest of the Tract C-b, received .72 inch of precipita- 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 from the National Weather Service pertaining to western Colorado MiG -'S7 IeAESIAAN ecrerorariars 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 wesiterm Uni tedastacesr 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, l7th Stagnattonmeondrt1 ons ane persisting over the western and south- western United States as asresult os Iatele movement of the upper ridge over the Pacific Northwest and no movement of the flat sur- face high pressure area." We (Gauss) E23. ESEJAN] coreerarion 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\tin-affieet for much of this area.” C. Meteorological Discussion of Tract C-b and 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 collider sin the val leyechanvon the plateau during mights when radia- tional cooling occurred and the downslope flow became organized. The diurnal range of temperatures was much greater at the Valley irattlers (020, O21 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 atetratler O23,oOneene plateau, where the katabatic circulation cell was not developed so as to abet rapid cooling. HO (Ges) 8) E2AAD EAA corrorarices On the majority of the nights in October.) Tvarver 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 020eeian 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 IT C-60 OT PA CES OA EA ee Pot ctoekiatd CGRPCRATION 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 Trailery023 winds did not exhibit as much of 7a 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 AS oe 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 iE -O1: FeFACS TAN ceornrorarice 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 structuce. 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 to 31.0 Fatethe 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 lst, 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 LIG-62 FERPA EAA corporarien averaged 2 miles per hour. The highest daily average winds occurned on October sudyand Zlst. On al diurnal basis, the strongest winds OCcUmred from 1s00mto 1500 hoursvat Trailer 020, from-1500 to 1800 hours at Trailer 021, and trom 0100 hours to 0200 hours (katabatie winds) at’ Tmatler 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) 23amiles sper hourtat drailer 021 on October 3rd. The highest _S-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. IL (EOS DJA DIAM corRrpoRATION VE: DATA PRESENTATION AND SUMMARY This section includes summaries for various recorded data at the monitoring sites. The data presentations indicate the variability of pollutant concentrations and meteorological parameters with location and time. In addition, the presenta- tions indicate the functional dependence of pollutant concentra- tion with wind direction. All data except suspended particulates (24-hour samples) are sampled once each second, but recorded as five-minute arithmetic averages of the one-second samples. This averaging technique tends to smooth instantaneous maximum values, and is especially evident when comparing wind gusts to local weather bureau data. | Inherent to any data acquisition system is random noise both from the recording instruments and quantization in the analog- to-digital conversion. The lower threshold fom ally analyereal em struments is twice the maximum noise level generated by the in- struments. This lower threshold is 5 ppb for all instruments, except for the ozone analyzer for which if is O25 ppb.) i bnesesonrer any values appearing in the data presentations that are less than > ppb indicate only a trace of pollutant@im question and should not be construed to be absolute levels. In addition, when concentration levels drop below the lower threshold, the re- corded quantity is simply random noise and averages tend toward zero. Thus, when concentrations are below the lower threshold of the analytical instruments they may appear as a zero entry in the data presentation which does not indicate absolute zero concentration. All pollutant’ data except fomepartrewlate data as taken at the monitoring site in integer parts per billion (ppb) but is presented here im micrograms per cubie meter Cicsma) G64 FOEAIOAADY corPoORDTION assuming standard temperature and pressure of 25°C and 760 mmHg (LOS - 7 nieli bars) pwesesPpectivels,. “ihe scale factors required to convert pg/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 The units of the meteorological parameters are given in the table.. It should be noted here that inside temperature is monitored and recorded as a functional part of the system but is Moe presented, ca yEhts seponc. Tablem ei drsplays the money statistics Lor each MOnTtOLIne StatwoneLoretne month., “fo insure statistical sig- nificance, and to reduce the possibility of introducing a bias in the presentation, averages are computed only when at least 50 percent of the samples are present, except for relative humidity and temperature, in which case 75 percent of the samples are required. If less than the required samples are present for a particular parameter, that entry will be blank. The number (oh C= 65 PAI DAA cyoRPoORATION samples present for a particular channel is defined as the total possible number of five-minute samples for the averaging time less the computer downtime less the channel downtime less the channel calibration time. The averages in Table III are arith- metic averages with the following exceptions: Wind speed and wind direction are computed using a vector averaging technique where the wind speed is treated as the vector magnitude. Particulate averages are computed as the geometric mean. Table IV displays the daily averages. Again, 50 percent of the five-minute samples are required in order to compute an average except for the cases of relative humidity and temperature which require 75 percent. A blank entry indicates an insufficient number of five-minute samples present for that day. Wind speed, wind direction, and particulate averages are computed the same way as described in Table III. Table V presents the maximum daily five-minute average retained in the data base as well as the time of occurrence. A five-minute maximum average is printed if any samples are present for that day. Therefore, the maximum five-minute average for a channel which experienced considerable downtime or calibration time during the day in question may be misrepresentative of the maximum expected for that channel on that day. Table VI indicates the five largest averages for various averaging times. The table shows the period of time covered by the average. Maxima are chosen so that time segments ie C= 66 E2fATOIEADI ceorponrarion are independent. The maximum averages reported are found using a ‘sliding average' technique with the exception of the 24-hour particulate average which is computed from midnight to midnight and the 3-hour hydrocarbon average which is computed from 6:00 to 9:00 a.m. only. 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 and is independent of daily and monthly averaging criteria. To demonstrate the functional dependence of recorded parameters upon wind direction, Table VII shows pollutant con- centration displayed in a bi-variate distribution with wind direction. The tables display the total number of five-minute samples occurring in each concentration and wind speed class. The mean concentration for all samples occurring in each wind class are also shown. This distribution demonstrates the dependence of high pollutant concentrations upon wind direction. Appendix A contains stability-wind rose diagrams. The wind speed classifications used in Appendix A are based on the Beaufort wind scale classification system. This is a system of estimating and reporting wind speeds, invented in the early nineteenth century by Admiral Beaufort of the British Navy. It was originally based on the effects of various wind Speeds On the amount of canvas, that avfull-rigged frigate of the period could carry, but has since been modified and modernized. Imeits present corm: Lor anternational meteorological use it equates: (a) Beaufort force (or Beaufort: number); (b) wind speed; TEC Gy DIA DALAM corporarTion (c) descriptive term;-and<(d) visible effects “pon land opjeces or the.sea surface. One land adaptation is the NRM wind scale. The six basic wind speed classifications used in the report are: 1-3 knots, 4-6 knots, 7-10) knots, 9! —lGainors: 17-21 knots, and winds of greater than 20 knots The follcouame table is a complete description of the Beaufort Wind Scale, taken from Physical Climatology, by Helmut Landsberg, 1969. BEAUFORT WIND SCALE FOR OBSERVATIONS AT LAND STATIONS Corresponding Limits of Wind Speed Explanatory at 10 meters ab. erd. - Force Title Specification for Use —— —_ - _ —_— ume Mt/hr KXnots Km /hr. M/sec. 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Ot rz} ot Gt 6 Ps 7 % & % ct 63 AW S ahs ty ep it 66 Gt Of ol eene YtiQH CpL/te/OF OL pdé/t /at)aolruad Ot Set at *6 wt eesweeeeo «t ot este este a2 BZ S$eanaeevweeak # zen tz Boe AE 62 = °ON YSTIVUL CSeaw/ONISSOIXO NSXGHLIN dO NOITLVIUVA IvNuNta Segre Kg 6. = 86 a 3 & a & ¥ & ¥ o) % % & g 6 % 9 a a & % % 2 > 4 a & % & 8 by % + ry & # Py * Fy @ % % % % * 4 4 & 6 e * % % % ot at i -Ols Vics % % % &% & % % ~ % % = % & ® % & S3— Sie ot -Ct- ‘of Ble 26 Fin Bie LY =O) 264 64 6322 i 962 Se 25 GiaeOb & Gs GS 9.1 Ce i. Oa oe) % > & 3 a} 4 & * a % 4 * # pt LT » 4 6 CP ce Of =Se 60 29%. -6t a 4 6 % % 6 @t 6 Gt 6 6 % Bt 6 gt 9 ¢ i ¢ rd NOMVOSAZUASD mee ye es aA FHP eet # ® 4 IN Om od HM | eat wt QD 2 ——W MO VTMOUON WA VTMFMOmMm DAMA D we wt of ort wt ot wt et wt ore CU EN CY CU OU OS CU OI OS CU 9D FD >- << Qa “63 ereene BR 63 9% 9} NVY3AW V2? ser r & BP 6t ct ot te e$rerept ft 82 4 LNSWNYLENI SHL dO LIWIN S1GVLIOSLE0 WOKINIW 3HL MONEY 3BUdWVS GIIVA ¥ SSLONZG «# *¢ ereseen et t2 eS setswetk &t St vt a? eae eK et ct 61 §9 ee xn eas gt et = WNV3W cGap pede OV 20" 22 Ge Lae rs 7 a a 4 4 a *% ) a” * 4 & § Vo: 924 cel Wel ela et Fet % a % % 4 & * 4 & * # ie @ a ¥ % 6 at ot of ty * % 6 a. -@ % % ) & & a a & z * § + 4 § *% % a a ® 7) a a & gt Py & Ob: Gt 949i. Zi oot Sh 0h oF el Ol et Pt Zi 93. 3Sh. pt Sheet att YNOH Cp4/te/et OL pd/t /@t)d0luad (Ce#W/9ONISSQIXO NSSOSLIN 4O NOILVYIavA “vnynta °Z eo PF SFO B th 9t bt at tc « ete O # vA Lt bt *g estat un ee % a ct esPTrk Hh & Lt Lt ON Y3TI val @ SNOILVAYSSG0 40 YBEWNN TWLOL SC ie ae 9 9 % rs ® * et Fs ot » 6 4 4 4% rH a % % % ve % a * + 4 e % “ % 4 % 4 1} 6ot 66 Ot 9t £t Zt St gt Sh Sot 9 g 4 po UP 8 a # & ® @ Cheops.) % % # 4 5 z 4 § 3 rr & a ® & % & a 4 4 & % r 8 r 4 > | Gh st <9 El oar 48 Seamer ie 9€t OST 2tt ¢ re t Gai OM -« ea mr 7 2) u On aan AM TFOWOR a wet wt wt we CU CU CU COU CU CV GY CY CC a as HUM TMHOWN OA AYQ ‘ — ET . OPTS r ey Fs —e wected ut CORPORATION res Fe x DIURNAL VARIATION OF NITRIC OXIDECUG/M#e3) PERTOOC(S9/ 1/774 TO 10/31/74) ew 29 TRAILER NO, HOUR ek 2e 2s 24 MEA! 22 19 18 SOs 7 15 is i2 12 DAY — OMRON MN wt wt we wee WOO ow 13 17. 16 15 7, AS te 19 12 19 Ye NE ot ~~? ~ & 7 7, ” {5 £526 « 15 14 s { i6 18 w {7 * i2 ai Li {3 * 1 muon a wt et {4 9 we & {6 Qo nm ve -—- uN ot 7 8 . ow = & ar 2 Q & 5 wet e 2 N a owt > & & Oe — 2 = wo —_ & & ot * * Os s _ Tre & od Oe = e ~~“ ws = & et Tee +e a) ~~ 2 @ oi = 2 N es & vs oe vs * -_ Hr z e eo = & = -< & O & ot tt t oF 2 = wo #n t& me A Ve UM we NW OI OS CV wr Ou Ou 23 29 Oo 73 s 2. 7872 MEAN OBSERVATIONS = NUMBER OF TOTAL * DENOTES A VALIO SAMPLE BELOW THE MINIMUM DETECTABLE LIMIT OF THE INSTRUMENT IL (Ce Beas. . ateh We } QF NITRIC OXIDE CUG/Mes3) PERIOD(1@/ 4/74 TO 18/31/74) DIURNAL VARIATION TRAILER NO, = 23 HOUR fomevewecom 24° 22. 25 24 MEA i7 14 15 13 i4 18 16 {6 15 15 15 17 124 1325 Phy 15 122 15 16 i6 15 mwvVTwmow > n rm 0 «es * roy & ot « os ron ao wt * Ss ae a e © ee ont s ae e co ee oo s Pt ee wet * ry 2 “wt ro rs * ra + . = ra e Pa s ra rs * ® s * e e ra # * e ~™ se ot a SJ N OOOH VMOMOVNOWOMmMAD we ert wet ert wt wef et wt ot od Ce CJ cu es =e - ios aa apeeeceae * & & ee ae * * & Ss & t & & 2 & a * 2 = ry oe + xe #& es ve ee se & e & 2 ae eae ae Ow + & a t = a @ w » + bd m win wo OY Cu ed ra) et su Sas SRB = ee + + *. oo * @ s « - @ e «& 2 &£ - s ie ie Nae « S eo 2 we = + * wv Ss 2 m © CC) CY! Cv CU € Ww MEAN 4946 TOTAL NUMBER OF OBSERVATIONS «= MINIMUM DETECTABLE LIMIT OF THE INSTRUMENT SAMPLE BELOW THE * DENOTES A VALID TiCaae0 30 ts & “2 ry "s ue s iG & a’, 8 J, ® ig 4a a) & = t a & sy Py ay Pt Lf) & rl Tt Olas ‘ot 64 OTe eo OT 3Gt LS 63 Bot ener) 'g oT a7 a 9 a ¢ a yt te oC ar & sé a et 66 IV3H v2 LNASWNYLSNI BHL JO LIWIT 319VL931L30 WAWINIK BSHL mON3Ra TQAOtk« oO eee esas Nereneoee ea 19 wo gt Z wee evuvee!e ee casi wv Lt er ere PRES aQAarwet or ee & LP) 9} NV3W eee eepeces . on Soe @ os Ore te Se zB ee ra vt clad teh RH at et = SNOILVAN3SEO gee & -@ ry % & % + & & e % % 4 % * % @ 4 % % a * * a rT * 9t gt ot gt oF os 95 91 ZY ect Gt pt + * & i r g % & % % bo Op % - Qt at a an a MoH Cp24/te/Ot OL pd/t /Bt)G0Tead CQ¥4W/9N) SOLXOIG NSXOMLIN | BeKRetEBHA S at “at oe ekzktrerkr Re A VdWVS QIWWA V S3LONZ0 « 49 eeexewerswes & YSEWNN WLO0L se aeweee#tksewt#tewn¢# Mars f % 82 * “ON YSTIVWHL 3O NOITLVIUVA TIYNYNIG *9 SPePer one et HF NOP ee t/ee Let 2 4 & S 3 &@ 3 4 E 4 4 = S a % 4 + 4 % + ro) # % % & a ry ry Fy a 4 4 5 8 4 & & a $ S @ Bes & % % 4% a 4 & # s i a % % * e % % 4 % Pi> Gi 0 t= St 85 ct 9g9ft 9f PteSrlo ot oF Cte “Clot Oo: ot Gi ot Cte oh el a21 4 % % s ry 4 & @ 4 * a % + = Le LE Cl aOCF oe % 3 % % a Ot 6 Ot, 6 * 6 6 at ¢ v ¢ A e ~ este enrnke + ee GS oe eo «¢ & et F wt wt wt wi ot ot Le) aww FC eEWN SD Beet VTRnRMHMO WO oy 3 K—K$VUMOMWVTFOOR ODA" WNM TWO © ot O82 wt et wt ot ot ot wt ot (YON CY OS OU OL Ce OV GU OU os) KAM TOOK © OO AVG 2G ‘2 a ‘3 ry ° 5 ry Ba ee 5 *Q a, ry He, e ne wef r '¢ Ft '¢ ry oC ry Jo: ry vee *3 8 2 e *g a’, a wg a NV3H $2 eens o ce SNSWNYASNI 3HL JO LIWID 318VL939130 WOWINIW SH M0138 S31dWY¥S GIVVA ¥ S3L0N30 + eases ts & oe eos, etrt th te eesanee WZ ake nea x 61 easneeae “¢ @ NVWIM 9rap Om too eek, aU mee ry ¥ 3 '@ 4 & a a a 4 4 ry 4 ro) Pile cee Cl a 2 4 a 4 4 4 mB a & * & 6 at et 4 » % % % _* 4% e e 4 o a % ® 8 % 4 4a oe a 8 % 4 Gt 2t. “94 .Siko Pie St Cpz/te/ot OL vst s/atja (Q¥eW/9N)FQIXOIG N3IIO @ S$NOILVAYUSSdO 40 YSGHNN Wildl ey Lis) + % * 4 et OF ee ee @ * Senne x ob St unc Ole3d Sy ee & FO D et EG. = *y se Se 2 OO F = *ON YSaTIVYL sent 2 *¢ 2 eetrs & - *¢ ae noses ULIN JO NOTLVINVA WWNUNTA EAS ee ff 3 & F “ese HID DB i A | I> @ x > +t tH 2 & veerke#t @ 5 log eal, NV A HW wt wt of et ot wt woo ct ws wo CY ON CU CU CU CU E&I OAS EU PD OONRNDOAQHKVMVTOONR DAGSKVvMmM FiwoOR BAD we wt -27 OM 9 SULFUR DIOXIDE CUG/M¥*3) PEPIOD(C14/ 1/74 Tu VARTATIGN OF TRKATLER NTURNAL 17/31/74) = 26 Nt, HOUR 24 MEAN io) Wor eel dae 1 LO See EO se 80 8S 14 Te) Ls “wr wa Nolte 18 on mM ™~ * au; 13 1% vk u 3 -< ON 4 ot 107 \e) ed lute. 27 ry 1. de + bd oe ON OM ON wv) LO Sy Cs wv ™ Wy iO (ON Qs (eu Cu XN ay) => e + ot e + Oe) e = fay] = e Fe ¥ Cu ey) = e x = - tae i <8) Zz © oo * 4 bs 25 e | oa * ~_ bd aw —_ oa e = N eC e+ « iT) _— * N =} @ tf % Cc ~ = - 6 = x = uu tr =! ie Mm tay e Fe Zz * _ Pa | _— tu! - 2 e a4 xt ii = . “> =! * Se 9) us 33) iw e te cs x _ = =k a s row e i * a eS < -.- CY e hai * —_ i « ua * - CG * e + o~ e = - < , ~—-— uw iT Cah53 _ : ry 23 22 1b ATOXIOE CUG/M##3) SULFUR PER DOINCIR? 1774 10 19731774) HOUR VARIATION OF NAL 5 1 4 NT 1A 4 © e eeeeee SwoTTsweuNnx7swanh evn st “ cere ere eR Re EE HF Se OO ee io) Lae ie) a a ee ee ee ee Rr ke ee KK He KE rN nm as i eset ec eB KH TF OT * 2 rere yr eee eA Ke} +ree arr F wx * arereereeRryk B ae Se KF RYH BR * * * a ee a | a a ee a ee F = + ere Ee KE KR BRE KE rk Ke KKH eH Ft x* * +e ee KE KR EH EK HF eek axe tet Se a ce fat) > kK we eB EK =e 2 ee a ee ee tat *¥ € +e kK * se +s ee eK KK Ke KOK KFT KF KF MO > ¢ & *~ * ke Fe FR KR KEK * (ie: OW 5 Oren +e x ek th BK RK EK * Ss _- x £ kK x x hk # xe xe kaermrxk k kK x * *¥ ct wee KR KR BE HE HK $e ek& Ke KK HE * eek KR KR He K KE RK HR EK + Kee Ke KR HH ww wv 2 kK RR HK KK HB EH KR rrewrarretk & © wT CY 0 IC Fe Be ee a ae xekewexee xk © KF om © te eee et Ee KB KEKE REAR SE BBE KEKE KE KHER K —_ wy xe KOS ER eH OK Oe Se S x eK kh RD eR KR ~ (aw wt CSS Kee eee ea a, Se eG Sie ee, MOE Ge wae ~ eS £& Se 2S CRS Cok KK RB we xk ht keN ek eR Om Cy Cv G Ci ee OM SK BR RK Ee a a i i | ek RK HR HH KH WM He Dean ee i ees Us Se i a Sle eK Ee EC Ew re £ TR eR A Or. MS SOG Sy Sy ee CN), SS 4, OD) Oe, IS 1) Qe eG let et et te EK AHA NANO 1. Re Burry OFTHE INSTRUMENT DETECTABLE MININUM at JNAWNYLISONT SHL 5JO LIwI) 399VL09490 WOWINTHW AHL KONG Diadsve OLavhA Vo Galungqe « *t = NVAW 4800 8 GSHONTLVAS3SSAN 49 aden Waits i ee Mee Me ee ee eR I i ee Oy Oh Oy *2 r a ¥ % rm 4 * * # # # % # 4 x % % 4 4 * *4 r % » P 4 a r % 4 % * * # % * x * Pr * ¥ » % ans * % * * % * * » * * e a ry & * 4 * * + % 4 ‘4 ¢ % rT * * * * * % * * ¥ ¥ % * * % » * * ¥ NVAK Ue> OC - ce Ne We Oye a al sn mt) ee eet yy Z 3 Q i . QOH Cyd/te/at OL vpd/t /etynulsegd 26 = *ON aaTiveL CQeen s/n) FOI KOIG ematiS so NOLivievan Wsysilg NS oe On t CE Ce ir ~ ie N anny Ow CO (GO; mw wet we OW OK OO OU — <— a) \ ¢ & NOMWECdIUuOD & 24 MEAN 23 Be 21 18 12/31/74) 17 VARIATION OF SULFUR DIOXIDE CUG/ Med) PERIONDCIAS 1774 TH repay 1& TURN AL i - «+t owt e& * * sv Saeeenoe & eH ‘Oo _ —T rT e B® reOe eke ea FO KH ES n ~ ~ LP] e x a Or 2 i 2 oe i i aes) o — - iP) — e Pid = rae Ff RPO eR KEM ~ sas — _ rm 2. = e &Y s FOND PEK eHeHeem wo Lbs —a—) _ rm WG z es b heed ray FOO F FR ees te weet nH wW wt Cc ro uJ 3H e - * * F-NOOR wR EKH A SKM “ww a -_ mm & ce G Oo & « eTOR kK RKO RHR ED ~ = “ _ rm vax ae e a _— x eee KH Be BrexXae nn 5 -_ te) me uJ e a =! xz + Ox & Me KR ee ve) uw xD — e qc + * * cK = kee x ee fae a co we MN (ce x x x ee com eR zs v fat tt S35 == e = = * * Keezw xe * 2 n = a = ia) om e re >= «co x Mrnre O we ‘oS a = a" +t Lan ‘wi - BG « -~ — ale = wal SS a G me | * * * SJ € 3 © mK OF er 'G u} _ - = FS e ul » * Or et EN +t # “ S ai = wt - fi. aya Su e ti! 714 a * a a a ar RR nm c I> _ _! <. = oa e Zz tm a ae * MaKe ek oF HR KR Ke) —t ou = Ben | < < > e - K * * i ee a a a ee ee ae Jt Se = o oo = ay e ua! x * * Oe a a a a ee a ee Nn = ¢€ ui ex '°o = & ye RK BU ew OR SS J a _ -_ -—_- bd e ow es + Wee ae 4 OS a a He 2 — Cw -_ -_ € * 2+ ONT (1S Sts SW Be RRS ay) - ~_ > Re Lt -G=t56 AWVNMONDOWN WAL AN MAM OR CA VAN HM TiIOWR DO ws =a a= we ete et ees at est tw OOO ON OG COG QA ofS 22 G ® @ 6 Chee < * V3W be ge *G od ANBHMYLSNT SZHL JO LIWIT 374VL992390 WOWINIW SHL 607390 Sldwve OLTIvA ¥ SILONSO «# az & NV3W gG8 = SNOLLVAUSSHU 4U Asesin Whos ®y Sp 8p D “6 *p ac Its) *9 af, *3 5 ra) *& Lars) *% Ws Ce ae » a * » * » % * * * % x % * * * + * + he ¥ % ip * % * * * % * ¥ * % ‘ Gs Wes “Oh “Sh Z lO Sie seb cl ah sa iiaeer A f ) si y y df CpZ7TE/at OL pd4/t /atdacgliusaa ve = ON w5TT VAL Coeaw/O) 3O0YXULG UNnaTWS AG KOLLVTaVA Vvieily ey ROMLYVUVOIUSD Go ou mm -_4 a) LP) cm © ™ ec NS 5 5G (BT 6S CH! St ee ee © © a © OG «WOW owt wt we "2 << WTO SN 2) a NS § MN rm oO MH -<¢ ia) -_ ia.) ~~ (ON OE GN NO wz NZ we ot rm? AN es 16 17 nN NI Os oS onN al a “1 W MN MW Oy tS - W rm Sd NY & 23 24 N ite) cy NON A ow WN oO ot wv mM Mm wr 2 MEAN 2 2. MEAN 8659 TOTAL NUMBER OF OBSERVATIONS = * DENOTES A VALID SAMPLE BELOW THE MINIMUM DETECTABLE LIMIT OF THE INSTRUMENT LC S58 ® DIURNAL VARIATION OF WIND SPEED (MPH) TRAILER NO, @ 21 cma abd Ce CORPORATION ¢ 5 PERIODC(I9/ 1/74 TO 10/31/74) ROUR 24 MEA evo ceiomee 25 {7 19 16 15 i DAY Mw Ww rm ian mw onr~ = rm ec ZT Le ee) few a @)) 2 @Q oD aS NG Te OE & rm ot w Ww wt we Tn 2 mM YS © c a wv ew Orn on Mm wt et ot ot O © w 11 ee 14 ot Lat Ces) wo rm cay) No NW rd Baa wa QO" WA emgnn -— AO - @ <-t* ~ ws TON -<« 19 ooo 6 om oo on owt mm - NI ay CV os wt ‘9 N ~ fe.) 4) Mt Cc CY mw nw mw vy NN ei - OF GN re La) c3 MEAN Se = SAMPLE BELOW THE MINIMUM DETECTABLE LIMIT OF THE INSTRUMENT MEAN 7220 TOTAL NUMBER OF OBSERVATIONS ¢& * DENOTES A VALID DIURNAL VARIATION OF WIND SPEED (MPH) TRAILER NOg ~i wae ue PERIODCIG/s $/74 TO 10/31474) 2 22 HOUR i} igeeeOenael 22 25 24 MEA 18 16 14 13 12 DAY ooo ve momgewoww Qn rt nw OWN ~_ oon anvnwwo Taw rgo AN A ND mowewme wttVuer OD mmmna ewe oe NM WwW <- 8A ~~ wot OW Mm 9 aM a <2 RON e Tn MO wo [ a? (ot om om em ?) ~_ NMwmaw aovrnwwo Ono oO aoanvnwo wm nn Oo Oo RON Mm O wTosS Tt VT TS = Non Qa sr nO Ho ft mf ~~ OR Baoan & MN ORK © QA A « oa -_ “1 -_ : -—OHe > — ir G& 9D vt = tot 2 mono vc wtw«t VNOanM ON © — NO oO ft ma oOoOn Oo “ot N&O D> TNONOM wt wt Oana LP i @ in @ se) wt ct SHNM YT MOONKR BHVHeAUdawvsoOowonr DA Vet NN TINON ot et ot wt wt eet we ws wt we CU CW CU CU ON MG OU Cy | cu ONT oer rv My 2 g Le; Cs wz cS mm fat tal a RVATIONS = 93531 ~ i = TOTAL NUMBER OF OBS * DENOTES A VALIO SAMPLE BELOW THE MINIMUM DETECTABLE LIMIT OF THE INSTRUMENT II C-140 eee last Vile Oz rrr ES OFS 22 ee Fee ae em Neat ON a om mere ~~ Cc DIURNAL VARIATION OF WIND SPEED (MPH) PERTOOC14/ 1/774 TO 19/34/74) 2 23 TRAILER NO, HOUR Zia ee. 20 24 MEA 20 19 18 16. 17 {5 42 14 10 DAY mw o> rD Qa @ a 2 & S -<® we SS @ a 8S & (s] -— & 8& Mm @& > ~ & Le ao - 2 v g cas} ve Lo) S © NW @ a Le) _ S&S <>) wz Ww ~~ w ia) is) &S > Ge Q wy & eS ™ iss) i=) Mw ® SS << sS & mvs INwon OD S w —S fali a.) oo & 8 iat wt © Ls] ts) ot <= eo S-< bs wh) ot oe? ot eQ is) iss] iss VAN NAO AAW - UWA Net OV NNO TS rm od wt ws <9) ie} o w ec 7 wt <= Nw -— w a; ® ow 2 rm S mW S wt — or 1D —_ mm 6 wz we fF? ty wt ot Ss Cs <4 Ss Cw“ ®@ D W~ @ oo of ~m Oa © Le) ue as ws we OV 4 1% 15 Poe Tos Me Ta 13° 87 “et 4s. 2. tee ats ii NSS AN ne MM cu MEAN Tin O Mm OO M ® er MG Oo OY ee OP? ro MEAN 4749 OBSERVATIONS & NUMBER OF TOTAL ® DENOTES A VALID SAMPLE BELOW THE MINIMUM DETECTABLE LIMIT OF THE INSTRUMENT TI G14 -142 C 1] co wt wt wt ot oo wt ws wt wt we OY GON MNMAMATMONR ADA VDaeNNONWTFMNON OAS 7 WHO Tt AVG NVSN VS C2 22 $2 B86 6b CEO Zh Slo Sh et fier tone 8 Z 9 G v c @ t uNOH (ypd/tO/Ot OL vdZ/t /Bt)Q0LYad ve * *ON YsTIvYL (HdW)Q3adS GNIM 4O NOTIVIYVA TvNuNnta ve) ee) _ ROWMVAOAaNoD 2 LNAWNALSNI SHL JO LIWIDT SUSVLIFLZG WNWINIW 3HL MO138 BldWv¥S GIWVA V S3LON3O0 # 11 *29 2 NW3H 6699 2 SNOITAVAYNSSGO 40 YSGNNN WvLoL “yd 532'°99 °39 "OS *Sp “Sp woot he Sse or (pp Sey CG 9G G7 G7) Uuetg 64 shu 225 -o2 “be NVAN SZ 88 98 S@ 6 O24 €2 89 9-99 Po 79 G9 99° 969) $20 Pe = G2. -G2. 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CON CO Gume GmeOp mye 00 ssOCmarC ht ce seCGe pt 8 $e SE 4 SC. — th. Gr =o9 26 ~0O BC sbG eto Como. (Gn Gee GC) BCl 6G n6c™ 608 Go me sce CC Z SY 9¢ 2&2 9 - \e (cp 6 Ge Cove ce 9 ep GS Oc “£8 68 €?. SG2-GG= CG Coe 20s Vie Cr = lett) Oy eGoe Ce Gf CC oe oC Cf coy ¢ SS hy Ob 6b 25 SS 65 ¢9 §9 69 TG v 7 Sy 9b 9b Ob OY vr OP g S oy &h “Gh 9 Io= 96. 69-07 Of 8412) C2. soeaees Hou CPs 6e =the (Ch GP © che < Oo bere kh SNL SN eo. een So ee DIURNAL VARIATION OF HYDROGEN SULFIDECUG/Me#3) wend Ve CORPORATION PERIONCAG/S 1/74 TO 16/31/74) TRAILER NO, = 20 HOUR 16-19 20 21- 22 23 24 MEA) {7 15 14 {2 11 12 DAY mow WO es CO) ow wet 13 14 {3 we 17 18 x ~¢t CM <4 ie) Lat Ww a0 26 © GM ¢ of MEAN 8346 TOTAL NUMBER OF OBSERVATIONS 2 * DENOTES A VALID SAMPLE BELOW THE MINIMUM DETECTABLE LIMIT OF THE INSTRUMENT Cara DIURNAL VARIATION OF HYDROGEN SULFIDECUG/Mew3) — a oe ORATION core PERTOD(I@/ 1/74 TO 18731/74) = 21 TRAILER NO, HOUR 24 MEA ao Moly oe ts 6 ©2806 2406~«é 88 12 DAY * © @& ~7 NM aed Lae) wt oo QO Q rman --8 8 Qa ite? Co) 14 S 21 Ur we MN CU OY & in cu mS © ON 27 38 MEAN 8057 OF OBSERVATIONS TOTAL NUMBER * DENOTES A VALID SAMPLE BELOW THE MINIMUM DETECTABLE LIMIT OF THE INSTRUMENT Liven DIURNAL VARIATION OF HYDROGEN SULFIDECUG/Me23) 19/31/74) PERTOD(Y@7 1/74 TO 2 22 TRAILER NO, HOUR 24 MEAD 20,2. “ee 29 19 17 9 DAY 10 ~~ ti Les) ‘9 e = @ = eS o ee & bd * oe 8 2 & * se <4 ee = a > * er bal e & * ee = bd = = bad = % = s = 2 < & & aod = e * a = ~ ¢ TINWO KR DOQQ UMTFMNOWRDAADRDK ANY ws oS wd we ort wt wt ws es ot OC GW OO CO CU 25 © GN c CW 32 - @ & “ a 4 -“ le e ss oe rl ~ © # — . & * od . & * ~~ . @ 3 - es s ~ . & x ~ ree 2 os ~ & 2 — on CS e — oe * ~~ e R ~ e # ot | 2 ~ e * _ cs > ~ e R nN . © * rod . @ # — es wa << e & ~ vd < lu - xz m 1, 3 * DENOTES A VALID SAMPLE BELOW THE MINIMUM DETECTABLE LIMIT OF THE INSTRUMENT MEAN SSi4 TOTAL NUMBER OF OBSERVATIONS = +> - al = a2 { A UN ZO - Lt . ra as 7 WY S ‘ mL) 4 | : . 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Because of the relatively low heights above the surface (9 meters) at which the wind data is taken, the stability distributions are skewed toward the unstable end of the spectrum. That is, the unstable classes (A, B, and C) have a much higher frequency of occurrence than would be obtained with the Pasquill method of stability categorization (or with instruments at higher levels). Taplemideprers the frequency distribution. of Pasquill stability categories based on ora from data collected by M. M. Pendergast and T. V. Crawford at the Savannah River Plant GActwal Standaimd Deviations of Vertical and Horizontal Wind Direction Compared to Estimates from Other Measurements", Symposium on Atmospheric Diffusion and Air Pollution, September Donn toy 4). sineCendi Stanct; range vpattermns of stability class PI Cai 97 CLEACSEMALY corcceorATIan distributions were observed: low, mid, and high, according to the height at which the Gg measurements were taken. AB eee Frequency distribution of Pasquill Stability Categories Stability Categories based on Oy Himes B C D E F G a v O% >23 «+18 £0 <3 aS Op <1&a 8 £99 <1 PS a e w ? VERY UNSTABLE MODEMATLY NEUTRAL MODERATLY UNSTABLE O° 8 10 (5 20 25 30 STANDARD DEVIATION OF LATERAL WIND CIRECTION Og (de9) - The vertical variation of the lateral wird- direction standard deviation (9,) for various stability regimes. The curves represent average or typlica conditions with the exception of the two outer “very Stable’ lines, which represent extremes. The large surface values of So for unstable conditions do not decrease very rapidly with height. As in the case of very stable conditions, the greatest lateral fluctuations during a very unstable thermal structure occur with very light winds. Acvavreneral rule, for a pivyensansolation condition, inereasing wind speeds are associated with profiles of oa 0 that tend* toward Nevitial Stabuiaty . Theymajyority of the trailers in the network recorded vVenyelaehit wands. throughomt, the month.” Therefore, the stability distributions had a predominance of high ore values ands wnence, wnisiablewelaccuiatcateons. hose trailersiwith the highest average winds (and fewest nearby obstacles to the flow) generally had the more reasonable and representative low-level stability class distributions. Pine-199 -200 ~~ 4 te es tC %-9e°e izes) © JAOGVY G3ZLNAIYLSIG SWIVD 4O YZ@WNN IvloLl FORCE OKSHETE FETE FECHUKSKSEGOSKEHEFS HHS KKEFT EHR ec eoEHOEKGC HKG DEG HHRKFER ERO RaHHKGI HEHEHE OO OHoeeKaKLKEBHL OHHH EKHKEROCKEEKBHOSES ‘egee 9292 £96 2ez Lt f Awilod 98° $9 82 MNN Sey 9tt ly MN 4 ‘ ‘ 1 gt . ‘ 5 ’ i i i seid t 4 ‘ H 4 ; ‘ val Gre 6t2 est tee eee oot (eel Zac 676 vile, Cy Gy Gee: Wi0d ett 69t 2c Got vat Got Gx. 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BS 84 x % 70° * aALIVIavis 3 40 39VIN3S943¢ % BuO ® ALITIQvis G 40 39VLIN3943d % Aa°o ® ALIVIGvis 9 40 39VIN3943d % 62°Q * ALI iIavis @ JO 39VLNSD43d % @8°@ * ALINIgvis vy 30 39vViN35943d € % Bo'D 0 “ SAO8V G3SLNGIYLSiG SwIVI 4O YS3aWNN AVLOL Hite eet) OD) UL OUO ONO OCU GOO SOG IS OUNH OOOO ROUU GOD A GUObUMDhbObEbObn bon ohn. frees i Ss as th wees , .¢ OS ar Ser ‘ ; € ee belies hoe SH fe eg, Ce age a) Ma gees emg) concer MM a Gv ugmt 0.) -S W104 4 $ ¢ 114 t t £ hee g 3 Zt = £ $ : gt = ZT : ; t pe Se : | 3 p2 19 Hd Q33dS GNIM WwiOh NN MN MNM OM MSM MS MSS § 3SS 3S Js35 4 3N3 aN 3NN ON NOITLIZYIO ONIM WiOl = Ssv¥19 ALI Ievis (yd/TO/OE OL w/b /Bt)001Nad be = *ON HaTIVeL ANVdWOD GTSL4HOIY ITLNV Ly ee Sy) on & Ca) : — MOMUEOsSD . — elf \LOD Ia AEN : eer “fae eis 2IPOLe Ets ghee eee RC#100-056 AIR MONITORING REPORT FOR C-b ‘SHALE OIL PROJECT : NOVEMBER 1974 Report No. 3 & 23 January 1975 Presented to: C-b Shale Oil Project SuLtEe 555% Two. Park. Central 1515 Arapahoe Street Denver, Colorado 80202 Attn: Mr. Max Legatski Prepared by: Radian Staff mi C= 250) 8500 Shoal Creck Blvd./P.O. Box 9948/Austin, Texas 78766 /(512)454-4797 FLAS ELAR cerrormrion ame Tit: VI. TABLE OF CONTENTS GENERAL DESCRIPTION OF AIR MONITORING PROGRAM.... DESCRIPTION OF INSTRUMENT SYSTEMS A. B. C. D MICROMETEOROLOGICAL AND TERRAIN FEATURES. ........ OPERATING TIME ANALYSIS FOR EACH SITE MONTHLY METEOROLOGICAL SUMMARY A. DATA PRESENTATION AND SUMMARY Monthly Averages Daily Averages Air Quality instrumentacioneyc.se a eee meee Calibrations? rocedure.oe er ae ree ae eee Data Acquisitton Sys Gems yi. a ocas cee eanee ee Meteorological Minstrumentation a. eae eo @ @ © @ 6 Cee el Ue 6 U6 (le 8! he 6 ee 6) Summary of the Major Features of the General Circulation over North America....... Summary of Meteorological Statistics in Western Colorado durine Novemberay.. eee Discussion of the Meteorological Conditions in the Monitoring Network during November oe ee ee ee © ew ee ee eee we “8 © © © © © © © © © © © ew ee ee ee ee ee ew ee ee ew 8 oo -@ @ © © 6 © ©) © 6 « e © « @€ © \o © ‘ee @ 6 0 8 © ‘0. © @ ee ‘0 © (0 ‘6 2 Maximum Five-Minute Averages and Time of Occurrence Maximum Independent Sliding Averages @) <6" 10; ce) eu 6 (07 te 4) @, (eo) *e) a. Functional Dependence of Recorded Parameters Upon Wind Direction Diurnal Variation of Recorded Paraneters @ Ww @ 6) (eis) ie) ie) ce. 0) eo 16) ‘60. 'e: © jelre oe Be HTS 66) 109 6 SLs PE G73i Page LI iM ime il Jat 19 I] Ol ry I] I] I] I] Vall I] all I] Ih I] I] C2252 Caos G=Z254 GeZ55 G25" C756 Gaz47 G-S52 C255 GaZ50 Gazz FOALES IAA CORPORATION 1S GENERAL DESCRIPTION OF AIR MONITORING PROGRAM ee EEEVALNG PROGRAM Radian Corporation is under contract Go, C—b) Shaile Oil Projects 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 hydrocarbons, 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 meteo- rological tower at one of the sites provides meteorological information as a function of height. Il (Cee F2FALDSIAAR9 corPorRarTion BOSSSUCKOS o/V iasoy *3 277 caanece} I Tea y! WOVYL AILVO || | SA0gY O} ae esty Graz (Oe SIV OYSZ ERA ELAS corroravrion ip wa DESCRIPTION OF INSTRUMENT SYSTEMS Pee) eA Quality Instrumentation Nitrogen oxides are measured with a Meloy Model NA520 analyzer. This dual-channel analyzer is based on the chemilu- minescent principle, and continuously monitors both NO, and NO. A subtraction circuit in the instrument provides a continuous NO2 output, but is not used in Radian's system. NO» is cal- culated once a second by the computer by subtracting the NO value from the NO, value, thus avoiding any drift which might occur in the NO2 output of the instrument. This instrument has a minimum detectable sensitivity of 5 ppb (parts per billion), and eaelinesrity of 1%. Both sulfur dioxide and hydrogen sulfide are measured with Meloy Model SA185 sulfur analyzers. The hydrogen sulfide analyzer uses a Meloy Model 50-1 sulfur dioxide scrubber and the sulfur dioxide analyzer uses a Meloy Model H2S-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 ae Ozone is measured with a Meloy Model OA350 analyzer. This instrument provides continuous measurement of ozone, and is based on the chemiluminescent principle. The minimum detectable Semeltivity 1s,0%5 ppb and the Pinearrey 2s"). Total hydrocarbons, methane, and carbon monoxide are monitored with a Bendix Model 8200 gas chromatograph analyzer. This instrument uses a plume ionization detector and has a minimum detectable’ Sensitivity of 5 ppb for all three components. The Model 8200 works on a five-minute Cycle ines, One aun Sample is analyzed every five minutes. PING e254 Fe -AEDEAARS CORPORATION The air sample is drawn in through a glass cane and manifold supplied by the Ace Glass Company. The system has a 25mm diameter, 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 conmected. All joints in the sampling system are secured by O-ring compression fittings. The manifold is contained in a heated (100°F) chamber to prevent condensation of moisture. The teflon lines’ from the manifold tojtnevinstca- ments are insulated with 1/8'" wall thickness rubber stubing The trailer has four heavy duty high volume particulate samplers (Hi-Vols). Fiberglass filter paper is used fer coltec- tion of particulate samples, and each filter\is breugmestouc controlled humidity before weighing. Each Hi-Vol has a flow recorder to permit correction for changes inva flow saswene 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. B. Calibration Procedures Each trailer contains a Meloy Model RAD-1 calibration unit. This instrument provides a zero aig Supply, 1s0> Spanepas 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 zeno, sand the computer monitors the output of each channel and takes a new zero reading aiter a-stable zero signal has. been reaened..) ines zero reading is compared by the computer to the zero reading eos FRAG EAIN corporavion obtained 24 hours before, and if a drift in excess of 10ppb has eceurred, an excess zero drift Iaeht for the! channel in question is turned) on on the System Status Panel. Next, span gas is supplied to each channel and the computer decides when a stable span value has been xeached. This value is recorded and compared to the pre- vious day's value. An excess span drift light on the System SEatus Panel is turned on 2h avdrikt sexeeeding lOppb oceurs: The instruments are then returned to the monitor mode, and after two minutes the computer resumes data taking. The bottled NO gas used at each site was ebtained from Precision Gas Products. Pre-purified grade hydrogen is used in the SO, analyzers. The -SO2 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 SO2 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 SO» monitors The Model 0OA350 ozone analyzer has its own calibration System which provides a zero check and a span check. The ozone calibration system is verified by comparison to a calibrated ozone Enenractore Marntarlned ian kadiam s. laboratory. in Rie le. & y The Model 8200 total hydrocarbon, methane, and carbon monoxide analyzer is calibrated with undiluted span gas obtained Enom Airco sSeRare and Specialty ‘Gas Division. This span pas contains methane and carbon monoxide in air, the methane being used to calibrate both the total hydrocarbon channel and the mechine channel. “ihe Model 8200-uws zeroed with air from a Li C=256 ReARPIAAN corPcRATION Bendix Model 8834 zero air unit. In addition the instrument is electronically re-zeroed at the start of every five-minute cycle. The Hi-Vol particulate samplers were calibrated using a Calibration Kit from General Metal Works. C. Data Aequis ition System The basis Of the data acquisteren 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 pestare Leatunes sine computer utilizes ROK L6= bat 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 unites Sacmec 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 lével, the trailer system is switched back to line power. NIE Oa 7s nH ~] Fe fabpafakd CORPORATION D. Meteorological Instrumentation 1. Ambient Air Monitoring Trailers PHoumvoL the ambient air monitoring trailers are equipped with the following meteorological instrumentation: (1) dry bulb Eenperatune (outside), (2) snelarive, humidity, (©), 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 33-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 ehnopper systemsy There arejmo light bulbs or photocells to, burn OUE- | pewcr consumption 2S Lows and the system 1s insensitive to NOtseUe TCONGeIsat Lon OLmdustedeposttion.) The solid state tachometer Powesscielally freestcom Maintenamce.wiLth a)life of welll over five years when operated continuously. ~The specifications of the W103 Cup Anemometer are as follows: Le -258 FRRESESIAAIS corPoRATION Accuracy: |) 2.1% ox 415. mph, awhachever 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 ohm low torque potentiometer and two wipers for 0° to 540° operations. The response characteristics of this vane are: Dead Band: 0O degrees Damping Ratio: 0.4 Distance Constant: 3.5 feet Threshold: ~O275 miles per, hour Potentiometer Linearity: 0.57 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 Electronies. ~The Sensex assembly contains a newly-developed hygroscopic inorganic sensing I GeZs9 ERZ2ESEAALY corporation element. Its expansion and contraction positions the suspended core of a linear variable differential transformer CLYDE) eeThe absence of friction inducing linkages and wiping contacts minimizes hysteresis and improves Sea ey ae he LVDT output signal, when Processed, is directly Proportional to relative humidity. The specifications of this instrument are as follows: Range of Indication: 0% to 100% RH Response: The sensor FEeSponse time to a step change of 10% in relative humidity ES) ess than 2 minutes with the sensor exposed to moving air. Accuracy: 5% - 15% RH; 5% RH 15% = 9579RH: 2 9% Ry 95% -L007 RH: + 3%° RE + I+ + Signal Output: Analog signal of -150 mv. EO .+EDO mv. with electrical zero at 50% RH as standard. 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 felvapi lacy of a tipping bucket Cageware combined with heavy-duty electric heaters to make this an all-purpose precipitation sensor. ines Bage may be used to measure snowfall and carnal iy An insulating cover of poly-vinyl chloride and a thermostatic control insure the proper gage temperature. The thermostatic control is adjus- Eabtes trom 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 page is constructed Il C-240 FRA\IDIAIN corPorarion @ of durable corrosion-resistant materials to provide many years of service. The specifications of this gage are as follows: Orifice: 8 inehes + \Caltbwationss,, 0.0% sineh Accuracy: 0.5% (Calibrated ‘at.02 5. ami/ tae - Sensor: Chrome plated tipping buckets Switch: Mercury, 0.1 seconds closure - Heat Control: Thermostat adjustment, 0 to 35°C. & 2. 200-Foot Meteorological, Tower The tower has instrumentation at feur Levelis cu rece 30 feet, 100 feet, and 200 feet. At all four levels, there are: wind speed, wind direction, and temperature and relative humidity sensors in a power aspirated radiation shield. Temperature dif- ference thermistors (also in power aspirated radiation shields) and their associated circuitry take lapse rate measurements for the 30-foot to 100-foot layer and’ the 30-foot to 200=foot Payer. In addition, this site has a Precision Spectral Pyranometer, a barometer, and a tipping bucket rain/snow page. 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 directiom and a light, chopper form wand @ speed. This sensor is rugged, with an all-weather coaxvalcupeana LLC 2a E2ZL.EDoc0d cerperarion damped vane assembly. The prototype model has been in operation for years under the most demanding weather conditions, performing ConEmnuously with the wtmostwrelaability: 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: Stastang Threshold: i0:75 mph Response Distance: 18 feet (63% recovery) Flow Coefficient: 7.9 feet/Revolution Aceunacy = = 0 .4inpmor- 2, Ghichever is greatcr) * Range: 0-100 mph Wind Direction Staztine threshold: 0.75: mph Delay Distance: 4 feet (507 recovery) Dampane Ratvo) O25 to 076 Accuracy (540 eystem). + +917, 0 Range: 0° to 540 Be ili AA corrorarion 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 atvapproximabel yl 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’ themmirstoz 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. Cireumlalvon 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: O25 aC - Range: =50°Getor 50 © Humidity « Neeunicy 7 2 Oa Range: “OO, te, L007. Relative Humidity Measurements of temperature difference are taken for two layers, the 30-foot to 100-foot layer and the 30 -foot to Z00>ioor 1 an ee B2AIDIAADY ccrrorarion Payer. | Ihe thermistors and circuitry used for these measurements are separate from the thermistors measuring air temperature. The lis¢G OL iceparate themumiystoms and tcircuitry 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 aeat the 100-foot leveiu and one ws jae the Z00-foot level. All of these AT thermistors are mounted within power acpurated radiatvonwsnrelds, Ihe specifications ‘on the AT ine tcumenecatLonm are as. folliows:. ACCUracy: = Cale ~ sRange of AD yCircunt (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 boons are S-anchepOssbeans whLehmane on woOllers 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 Glinbing. twowbase ground kits and one anchom pround kit. The cable-type Safety Climbing Device consists of a cable and attach- ment. mechanvsms with a locking sleeve and safety belt. The tower Pouleeneed and paimcecd) accordang sto FAA specifications. tbe sipnals from time tower anstrumentation are fed. from . . . . on was pee! PS Nubeuplemsaonal cables: intoweransmictess mounted at the base of II C-244 FREE EARLY corPoRAtTIONn ® 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 shrelded and iansulaced fiom the clements. The signal cable is run underground in PVC conduit in order to minimize damage from the weather or various rodenés in the -reevon. The auxiliary equipment at the tower Site comsistsuorsea heated tipping bucket rain/snow gage, an analog barometer, and a Precision Spectral Pyranometer. The rain/snow gage is the Model POLI-E unit. by Weather Measure, with characteristics yandyspeemer— cations as described in Section 1. The barometer sis the 8242 Analog Output Barometer by Weather Measure. This barometer provides an output voltage that is linearly proportional to pressume wine & specifications on this instrument, whieh Ws mounteduamsadertme monitoring trailer at the site, are as follows: - Range: Specially desipned for the 100 millibar interval from 725 millibars to 625. millibars. Resolution: Imfinate : > ~ Linearity: +4 0). 5. miblibas, overwehe 0G MullLubaice interval: The. pyranometer atthe site as the’ Eppley "Psecisuon spectral, Pyranometer. This instrument is wsed for thesmeasure— ment cf 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!’ Came ohas beens taken te Ld C=245 ERA BAAS corperarion eliminate the effects from all outside influences, such as reflection or shadows, on the pyranometer. The instrument characteristics are as follows: Sensitivity: 5 mv.) per cal/cm*/min : “Independence: ~300 ohms Tempesature dependences Sensitavity 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 ord 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 “nite is -wsed to calibrate the anemometers. The wind direction IMstrumMentattou 1s aligned) to true north (reference direction) .by means of a surveyor's transit. Il C-246 FeALISEAALS corPporRarion 1 gl) 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 Rieceance 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 School 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 area, of ycourse, Gccuneacmene 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 fromueast, to west) omy trom Prauven 022 to Trailers 020. .to, dialer aG2i, As mentioned at the outset of this discussion, the terrain will have a large influence on the meteorology of this region. Considering” first. Trad ler 7022, at theveasiterm end von the monitoring network, a nighttime katabatic (valley or down- slope) flow will exert a tremendous influence on ‘this ‘sree. I C247 RADIAN corporarior Of the three monitoring locations in the Piceance Creek Valley, Eniswsite has the steepest walley walls in its vicinity. As a result, the nighttime katabatic flow is Stuoneest Inere.. That is, the downslope winds are constrained or channelled at this point such that the nighttime drainage winds often reach 15 miles per hour. 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 Trailer O22 eGov lrailen 020>. iso that channelling effieets 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. 1ice24e IREAGS SARIN cerroratrion Trailer 021, located near the Rock Creek iSchool, vhas 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 /000 feet being .5 miles to the south of the tower. The tower itself is on the top of a small knoll Vocateds between Scandard and Sorghum Gulches. Because of its location and the irregularities of the surrounding terrain, meteorological patterns are Vatled here. Wind instrumentation is mounted at four levels of the meteorological tower: 8 feet, 30 feet, 100mtect, “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 windsilow is strong, all. four tower level wa reflect a gradient wind flow, with the winds imereasing in strength with increasing height. Linea2a9 RADIALLY corrcorarion 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. As a result, the meteorological parameters measured at this location are jsubject ‘to rather rapid variations. The aréa 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 diya wandy 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 dry character of the air in this portion of the country. As a result, the diurnal range of temperatures will be extremely large. Because of the katabatic flow in the valley, nighttime temperatures will generally be lower in the valley than on the plateau. During the winter, especially, temperatures in the valley may be 20°F lower than they are on the plateau during the early morning hours. In particular, the drainage effects wild) be spectacular at) Trailer 021) which will often experience L11G7Z250 RABIUARY corrPoraArion 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 ground-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). me C=251 EQFARSIALRY ecorpora7ion LV" OPERATING TIME ANALYSIS FOR EACH SITE This Section presents the operating, statistics for each of the major subsystems contained in each monitored station. Table II shows the specific number of hours that each of these subsystems was inoperative for the month. The column labeled "COMPUTER" indicates the entire data acquisition system and downtime hours appearing in this column and, therefore, means total loss of data. These instances include in addition, to computer downtime, power failures, no power available, and self-automated shutdown periods such as during air conditioner maLEunctLons. Calibration time is not considered to be downtime and is, therefore, not included in the downtime figures. The amount Of tEimerused in calibrating the instruments is given at the bottom of the downtime analysis table and is reported as total Calabration hours forveach channel for the entire month. As is evident in the calibration figures, channels can be calibrated independently of one another. No calibration time is given for particulate monitoring since Hi-Vol calibration occurs infre- quently and only during the off-duty cycle for each Hi-Vol while another Hi-Vol is taking data. PinG=252 e S © NY Qesseusrsdssgyssynd o—. 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Summary of the Major Features of the General Circulation over North America ee ee ee eT CN (OV EE NO BEM amleaalea 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 EL, 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. SpeCLiical Ly. 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 PrECipl ta— tion. The Atlantic seaboard region had temperatures and Ei C=Z59 ESAS EDEAACS corPORATION precipitation totals which were slightly above normal for the month, while the South had near normal temperatures and slight- ly above normal precipitation. The Gentral 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 PEeCI pi tatwon’. 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 PortheruCalitornia, “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 Vieinity of | teaet C-b on the lst and rain and snow showers were widespread throughout the vared. hie e-260 RAL IAN ecrporarion 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 lof 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. DInG2Z6i FADD ILA cerpcrarion 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 made "elouds dotting thei 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 im hexas, alone the Cult Coast, infithe Northeast, and in the Pacific Northwest. On the surface, the cold front moved off the Atlantac coast, while: the occlusion in the Northwest re- mained essentially stationary. A weak surface high centered imekansas dominatea the e¢ixculation throughout the nation: Generally fair weather prevailed in western Golorado.” 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 C2262 EQAASSIRARY corPcrRATION 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-southern 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 PacitireWoren— 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 Jipht 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 IT. €=263 EOAILOIAIN corporavrion 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- Castern Texas, Precipitatronjwas scattered through the Pacific Northwest and the Intermountain Region. Precipitation was also concentrated along the cold front in a broad band from Texas to the western Great Lakes. In western Colorado, skies were overcast during the morning and some snow flurries occurred, but skies began to break by the afternoon as high Pressure, DuLIt 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 western Great Lakes region through the Mississippi Valley to a low in southern Alabama, from which a cold £ront 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, and Ohio Valley regions. to dig southeastward throu . a oe | . ne a Strong continental polar outbreak. However, a strong short wave began eh the upper ridge im British Columbia, portendi i C=264 EQLAID EAE corPOoRATION 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 througherne 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 Wes@ 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. LisC- 265 F2eAAGSEAAN corrpcrarion Zonal flow re-established itself over the United States on November 16th. A short wave, located on a 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 9 Mild fair weather prevailed in theivicinity 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 eastern 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 western Colorado. The maritime polar cold front passed through the Tract C-b during the evening, bringing scattered showers and a few thundershowers to 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 Li G-Z00 FREE, EAA cerpPcrRarion 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 Dakota. A cold front and low pressure system were located just off the coast of northern California. Precipitation uwas, confined) to, tue Northeast and the West. High pressure dominated most of the nation. The Tract C-b region had mostly fair skies on the 2lst, with some scattered to broken middle and high cloudiness over Ehewared: The zonal upper flow pattern continued its eastward progression on the 22nd, as the Pacific short wave system advanced inland to an Idaho-southern California axis. The maritime polar cold front-associated with this short wave eG 2a; ERAS EAA corporation 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 torthe Pacific Northwest and along the length of the cold front. IC =268 CAE EAA cereorarion 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 ‘thes 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. Ling=209 FeFARDELEARS corpcorarion 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 ecentexed just morth of Maines. justynorth 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 haltvof 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. Li €=2710 EZRA IAN ceorperarton 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. DIG 20en FRASES ELAR corporation B. Summary of Meteonelopical, Statistics in Western Colorado during November fhe 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- Der son s)he 226 and! 75) aeineaddsitton) the: passacelor ian upper trough on November 28th brought extremely cold air into the region. Precipitation fell in the area on twelve separate daysnor sNovember, (November 175.2,,/3,. 45.8, 9, 10, 18819. 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 Our VOL aypossible LO0for 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-soui west of the Tract C-b, measured 1.18 inches of precipitation during November, which is .57 inches above normal for the month. Ge 27/2 IRREESEAAIN cerporarion 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 ‘termanglean Les Ausieim: tacelreres: 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 csidge in themWest.. ») 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 REARS EAARS corPorRaAtTION of the 24th. ihc an 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 hetghts 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... i Ca2 4 FRCAESEAREY ceorporatrion 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 katabatie circulation cell continued jtovexertena large influence on the meteorology of the Piceance Creek Valley during November, althouth the anabatic, or upslope, cireullatioen 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 Erom 0100 ‘to 0500 hours in the mommmme, When northwesterly gradient winds extended down into the valley, they were normally strongest at Trailer 021, at the western end of the valley monitoring network. Mt (S275 FReFAESEARRY corporariora 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 mites per hour at) Trailer 020¢enethe eth, §23 milessper hour ab iraiten 021 on the 28th) amdalé miles per hour at Trailer 022 on the 27th. 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 2lst. 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 ctronp, skies were cloudy, and precipitation fell, the strong radiational cooling did not develop and temperatures were rather uniform throughout the monitoring network, from the valley to the plateau. nie G=27 6 E2ERESIESDY ecrPcorar;rion Monthly average temperatures in the valley ranged from 26.7° at both Trailers 020 and 021 te 28.9 at tratleus022. 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 =i? B and -16 5. both occurring at Trailer 021, om Neowembere2Z3rn 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 te the extent that it aftected the valleye (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 pare ly, 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 tomeneutacnr that the synoptic-scale pressure gradient force winds which affect the plateau seldom extend into the valley because of the terrain constraints.) The tower site, in partreular. momocten LO O75) E2JAIDEAAN corpcratrion 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 dizection) 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 herenterabove: 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, T2278 RAES SAAN] corPorATION 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 lL 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 33212) athe highest daily average temperatures during the month, L1-22E to OD GAN occurred on November 21st. The coldest daily average temperatures on the plateau were recorded on November 29th, with the daily averages ranging from 13 .j6 Fete 1553 °Fewoiee 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 a fy at both the 8- and Z2Z00-foot level's on thesadth. Mate ene RARER corpcrarion 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 2lst 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. It G-z30 EFRAAES EASES corrpcrarion VE. DATA PRESENTATION AND SUMMARY This section includes summaries for various recorded data at the monitoring sites. The data presentations indicate the variability of pollutant concentrations and meteonolvorzreal paraneters with Loeation and time. © In addition, the presenta tions indicate the functional dependence of pollutant concentra- tion with wind direction. All data except suspended particulates (24-hour samples) are sampled once each second, but recorded as five-minute arithmetic averages of the one-second samples. This averaging technique tends to smooth instantaneous maximum values, and is especially evident when comparing wind EuSts to Local weather buseaw data. Inherent to any data acquisition system is random noise both from the recording instruments and quantization in the analog- to-digital conversion. The lower threshold for all analytical in- struments is twice the maximum noise level generated by the in- struments. This lower threshold is 5 ppb for all anstrumenes, except for the ozone analyzer for witeh tt as (02> ppb. sine retou, any values appearing in the data presentations that are less than 5 ppb indicate only a trace of pollutant in question and should not be construed to be absolute levels. In addition, when concentration levels drop below the lower threshold, the re- corded quantity is simply random noise and averages tend toward zero. Thus, when concentrations are below the lower threshold of the analytical instruments they may appear as a zero entity in the data presentation which does not indicate absolute zero concentration. All pollutant data (except for particulate data is taken at the monitoring site im integer parts pex bilivon Cp) but is presented here in micrograms per cubic meter (jig/m-) ID C= 281 EFRERED IAA corPpGRATION assuming standard temperature and pressure of 25°C and 760 mmHg (Ome =2ymalilibarcs), respecrively the scale’ factors required to convert pg/m*? at standard conditions back to ppb for the various pollutants are given in the following table. TO CONVERT yg/m? AT. 25°C AND 760 mmHg TO ppb MULTIPLY BY POLLUTANT NO. i 534 NO 534 NO» . i - 534 S02 , | ey. SeSeyA oon | apap THC 1.536 CH, 3 1.536 ee) | S77 0; | 512 The units of the meteorological parameters are given in the table... It should be noted here that inside temperature is Monltored sand secorded as a Lunctional part of the system but is not presented in this report. Fable Wi displays the monthly statistics for each fomleconing, station for the month, Po insure, statistical sig- nitiucanee, and. to reduce the possibility of introducing’ a bias in the presentation, averages are computed only when at least 50 pereent of the Semples are present, except for relative hunidity and temperature, in which case 75 percent of the samples are required. If less than the required samples are present for a particular parameter, that entry will be blank. The number of Mie C2282 RADIAN coreoration samples present for a particular channel is defined) as) the totar possible number of five-minute samples for the averaging time less the computer downtime less the channel downtime less the channel calibration time. The averages in fable LIL ave arith metic averages with the following exceptions: Wind speed and wind direction are computed using a vector averaging technique where the wind speed is treated as the vector magnitude. Particulate averages are computed as the geometric mean. Table IV displays the daily averages. Again, 50 percent of the five-minute samples are required in order to compute an average except for the cases of relative humidity and temperature which require 7/5 percent. A blank entry indicates an imsuetreveme number of five-minute samples present for that day. Wind speed, wind direction, and particulate averages aré computed the same way as described in Table IIT. Table V presents the maximum daily five-minute average retained in the data base as well as the time of occurrence. A five-minute maximum average is printed if any samples are present for that day. Therefore, the maximum five-minute average for a channel which experienced considerable downtime or calibration time during the day in question may be misrepresentative of the maximum expected for that channel on that day. Table VI indicates the five largest averages for various averaging times. The table shows the period of time covered by the average. Maxima are chosen so that time segments IT C-283 FROELESELSEY ceorPoraricn are independent. The maximum averages reported are found using a ‘sliding average’ technique with the exception of the 24-hour particulate average which is computed from midnight to midnight and the 3-hour hydrocarbon average which is computed from 6:00 tow? 007a.m only.) For averaging weimes ess than or sequal to three hours, the sliding average is stepped one five-minute Samplevatvajtime. For longermsaveraging 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 preater than one hour require 90 percent. Whether or not a sliding average is computed is solely determined by the number of samples present in that averaging time and is independent of daily and monthly averaging criteria. To demonstrate the functional dependence of recorded parameters upon wind direction, Table VII shows pollutant con- centration displayed in a bi-variate distribution with wind direction. The tables display the total numper of five-minute samples occurring in each concentration and wind speed class. ihe mean concentration tor all sampkes occurring in each wind class are also shown. This distribution demonstrates the dependence of high pollutant concentrations upon wind direction. Appendix A contains stability-wind rose diagrams. The wind speed classifications used in Appendix A are based on the Beaufort wind scale classification system. This is a system of estimating and reporting wind speeds, invented in the early nineteenth’ century by Admiral Beaufort of the British havye phe was, Originally based on the effects of various wind Speeds once amount of canvas that a full-ripsed frigate of the pertod couldmecaxrry, but hasi’since been modified and modernized. files presen. Lot LOr Interynattonal meteorological use ‘Lt equates) (a) Leautort ferce (or Veautore number); (b) wind speed; ie 284 REIDEAARY corPCRATION (c) descriptive term; and (d) visible effects upon land objects or the sea surface. One land adaptation is the NRM wind scale. The six basic wind speed classifications used in the report ares’ 1-3 knoes,) 4-6 knots, /-10) knots, 1-6 knots, 17-21 knots; and winds of greater than 21 knots: The follow: table is a complete description of the Beaufort Wind Scale, taken from Physical Climatology, by Helmut Landsberg, 1969. BEAUFORT WIND SCALE FOR OBSERVATIONS AT LAND STATIONS Corresponding Limits of Wind Speed ——————o = Explanatory at 10 meters ab. erd. - Force Title Specification for Use | ———_ & Mi/hr. IXnots Im /hr. M/sec. 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(ad) (NTC eo: oN Cad LN pol Ss ali, Mop (pal (ai > bh= fe= i= ¢ f= Q : $ Vv 3 vi {; ( " ¥ i Se Calo os mal 3 Da fh rata | | 0 G c ¢ y ) S v ¢ 2 t KOILYWBCAINSS ce 7741] Dive - a a DW NG XY a ON I on et Cre Ty Ca a TCO) YAU (OY: fafa fail (oy) GIG Guinta ™m™ © Ce LOO RNS Tok He « eis ier on Well. a elite a ON > <1 OD RANA esarcemnaticr APPENDIX A STABILITY WIND ROSE DIAGRAMS IT C-412 oe Vand gunk cart ie ahs PQA aE cerrawrnmon APPENDIX A © STABILITY WIND ROSE DIAGRAMS According to the data presented in AEC Safety Guide No. 23, the relationships between stability classes and Og are as follows (the values shown are averages for each stability classification...6, is the standard deviation of horizontal wind direction, Eluctuatrons)= Average Values Stability Pasquill 56 _ Classtivea tion Categories (degrees) Extremely Unstable A 25 30 Moderately Unstable B 20, 0 Slightly Unstable 6 5 se Neutral D LOMO Slachtly Stabie E pOe Moderately Stable F 25° os stability wind roses obtained at the treubers: meine monitoring network are displayed in the following tables. Because of the relatively low heights above the surface (9 meters) at which the wind data is taken, the stability distributions are skewed toward the unstable end of the spectrum. That is, the unstable classes (A, B, and C) have a much higher frequency of occurrence than would be obtained with the Pasquill method of stability categorization (or with instruments até higher levels), Table 1 depicts the frequency distribution of Pasquill Stability categories based on So from data collected by M. M. Pendergast and T. V. Crawford at the Savannah River Plant ("Actual Standard Deviations of Vertical and Horizontal Wind Direction Compared to Estimates from Other Measurements", Symposium on Atmospheric Diffusion and Air Pollution, September 3-13, 1974). “Three dieting t ranee pat tors ot stability lags PL Gra CELA COLLAR cerpornvior istributions were observed: low, mid, and high, according to the height at which the Og Measurements were taken. TABLE 1 Frequency distribution of Pasquill Stability Categorics Stability Categories based ono ck ere Re OS ee alg 6 A D E F G Hetgnes Og >23 18 = t ~~ ~ ” “ a be » 7 Zz c < > = = eee | x G y, = = % Fs b 200 5 oO a 0 (e) 5 10 {5 20 25 30 STANOARO OEVIATICN OF LATERAL WIND CIRECTICON Og (deo) - The vertical variation of the lateral wind- direction standard deviation (aq) for various stability regimes. The curves represent average or typical conditions with the exception of the two outer ‘‘very Stable’? lines, which represent extremes. The large surface values of ora for unstable conditions do not decrease very rapidly with height. very stable conditions, As in the case of the greatest lateral fluctuations during a very unstable thermal structure occur with very light winds. As a general rule, for a given insolation condition, increasing wind speeds are associated with profiles of o 0 that tend toward neutral stability. The majority of the trailers in the network recorded very light winds throughout the month. Therefore, the stabrilney distributions had a predominance of high ofa values and) ence, unstable classifications.) Ihosevtiraviers with thephagiest average winds (and fewest nearby obstacles to the flow) generally had the more reasonable and representative low-level stability Class dustraputrvonce TI Ge4 55 C-416 C% 60 th “Jeurt ~ JA0KY GalnuleiSldG Swlvd dO daueiin Tviud OCH FEROS OHHHEOESOSEHESHO HEHE SHEET ESTED EEE HEHEHE ETH OH HEHEHE HHH HEE HEHE EHH HES EEC HS EYES DEOE “4698 3 61. Oy €2 5 _Ghl Gbie Meh soll GUT) clCe Gre nee GGe 7 cGmerG e “ty : 1vicl T6000 sear ¢¢ 9S D6 g6 Te ZS “tt 6St 6tl eer wIS Bop Cy > 5 : ¢' JQ 196 tae g et ot Ve Cy oe Lie Lele Se. $66 Got eG 9 ég if : Z - ¢ gece § T v A S ve ot Vt Gd fa! 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