~~ OP pent 7 - ‘ 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 Oil, Inc. Atlantic Richfield Company, Operator Shell 011 Company The 0il Shale Corporation APRIL 14, 1975 Pir eb rw! WHT Vv ili eon ay + ° MATIN OVAL | ad | | ae eA 3 ti. QUARTERLY REPORT #2 TABLE OF CONTENTS BY VOLUME NUMBER Volume Number Table of Contents I I. PRE-EXPLORATION ENVIRONMENTAL RECONNAISSANCE SURVEYS A. Biological B. Archaeological II. ENVIRONMENTAL BASELINE MONITORING PROGRAMS A. Surface Water 1. Streams 2. Springs and Seeps B. Core Drilling and Associated Ground Water I 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 Ee 8. Aquifer Data - Drill Stem § Multipacker Tests 1G thee tae 0.) a. .Detlistem Tests. -. SG-1y7 V D. MPT Series-1 --SG-17 ©. MPT Series .2':-.SG-17 VI d. MPT Series 3 - SG-17 é. Drill Stem Tests = SG-20 £. Drill Stem Tests -SG-21 9. Aquifer Data - Pumping Tests Vil &, ViuE 10. Lithologic Logs 11. Geophysical Logs 12. Assays 13. Trace Element Analysis 14. Rock Mechanics 15. Gas Samples IX C. Air Quality 1. Air Quality and Surface Meteorology 2. Low Altitude Meteorology 3. Upper Air Studies 4, WVasibility 5. Atmospheric Diffusion Studies x XE Geel 6. Radian AQ Data XTIE D. Biology B 1. Terrestrial Wildlife Studies 2. Aquatic Studies 3. Terrestrial Vegetation Studies 4. Dendrochronology and Dendroclimatology 5. Soil Survey and Productivity Assessment Pi. “OTHER STUDIES A. Fish and Wildlife Management Plan B. Revegetation Program Ce Microenvironmental Program D. Aerial Photographic Study E. Archaeological Studies . F. Scenic Values Program ‘ on eae ) a Li Ve zee. Ore) lo oidsT LATMAMEDATY: AUSIOAI ‘es AK egece [ 3360 Gyo) bats? sogeA Gre ani!! 27414% + i cami tothe? 301 obfiaad - vir: m ond Soheg + = Sf. quays. ele reat ee: - BI 08-02 - ester mare iti If-o2 7 aaah Ot tai s7eof Signs =< 2A) ee) as a > 4 lial ; ey . Le bec fi uh > i Aur oe 7 —. LL Eva oe tal4 aIS 4 oh, a ee os ’ ‘aii 7 ae Ue » WR) ) ae 4, vie 4uv e . IRAAOOAIN (ee ema, tear bd Sa ud » RC#100-056 AIR MONITORING REPORT FOR C-b SHALE OIL PROJECT DECEMBER 1974 Report No. 4 rt ) 4, March 1975 Presented to: C=b Shale. Oil Project Suite 555, Two Park Central 1515 Arapahoe Street Denver, Colorado 80202 Attn: Mr. Max Legatski Prepared by: 9 Radian Staff II C-464 8500 Shoa! Creek B!ivd./P.O. Box 9948/Austin, Texas 78766 /(512)454-4797 7 f A = | y ad ee soos eh Uae 7 t Ry - ar ™ a. ; = 2f 2 : “yy is = ra ; a o- m3t : : os oA 7 ‘ . * » : ir 7 ” — 7 a a 4 : M8) Sesh owl 222 2: Mlegbenh E12! _s —— a yy Shera! Sov3 26 ee reves FRAEDSIAALY corporariorns TABLE OF CONTENTS Page I. GENERAL DESCRIPTION OF AIR MONITORING PROGRAM,...II c-466 Ph. © DESCRIZ TON OFVENSTRUMENT SYSTEMS: 22.0. . a ee ee II Pgh ual ty nse rumentat hon. of alls. oe Ss cee Te Be. Ca librataonwmryrocdeduxes.i: {Pst ti Be oe os Jig C.. » Data, AcquismEwvon Systemes: . Pheer yee Se ree ee 0) De + Meteonolomiicalsjinctrumentationt to... eT r TT IIIT. MICROMETEOROLOGICAL AND TERRAIN FEATURES......... II IV... ‘OPERATING TIME ANALYSIS FOR EACH SITE. a6 23 ais e.cct i Vie -MONTHLY METEOROLOGICAL SUMMARY seni % Oes.cie ace comets an Ee A. NOfen, Ameri came SUMNATY cates ae waste osu Roaee a eee 1 B. Meteorological Statisties an Northwestern Colorado durzne. December: 3... ase a8 5 os oe a aes bE C. Summary of the Meteorological Conditions inthe Tract C-b during December... 2.5.53 66% DI VI. “DATA “PRESENTATION AND SUMMARY... oa... Secu ee eee APPENDIX A - STABILITY WIND ROSE DIAGRAMS. .....:. Bt II C-465 C-468 C-468 C-469 C=471 C-472 C-481 C-486 C-4593 C-493 C-495 C-500 C-505 C-630 7 - oo -_ 7 2 A “a = g ef 7 ‘oa ‘ ) 4Se> oi a a . é > ’ ° . wt, i ‘ 4 1 ro + r 7 : . 7? KR € » as) , = a = oo? ~ 4 - ae : ; : “ '- ™ 4 40) ’ 7 z an 7 z a +7 : : - ze «~ % > “Ve ; Ba.) ‘ : ° ~ od (oa ie ree 3 > a is < i _ : deo 7 vB oe ore s 4 7 a r =. Sar es a co I. rer +h " Ty A { ] 1 bos 11 «a» @ . » »- Gee 7A ALAA ia: va re. < du i ii : 7 ~ wees) tial el) ee Ha i * @ a -eeidlia iA AO’! ow ha é 2, *e em eof wee ts AA dl ApD Tito ais er i hh ee - om Snaige » Sit ith; obs" = 7 nod Ebaod i igaseaak erie. oe erm |, we il tad imaaoT gab < +) Saat on? Ab » + _ -_ 7 - —_ : : : _ _ = . ei a eo Waa en ats, wor 7 A Vs es i] (ATAG aie a” , wid 0 ¥ nea: a0 vas 7 Buh oy ae son ios TT TATZ. - A xis 1. = fea a ie (OLMOVANS conrPoRaTion E; GENERAL DESCRIPTION OF AIR MONITORING PROGRAM Radian Corporation is 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 hydrocarbons, methane, ozone, and carbon monoxide. Selected meteorological parameters such as wind specd, 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 C-466 —— a * ed " i 24 sg RS 08 | - Duar ) eam a rs SUL ~ 4 eal DRL steursn? cert te RON AO | RS rad | | LOSSEUANOD o/¥ t \ oe ee soos eee Boves weo 2 Re ree A er sw ane wren twee OA ER Ey Lae 4 Bere nds Be ee eens Ore ew ra tee 4 PO eee A PE os Oe Oe 8 ot Brae se IT C-467 a = a a (RSS aE EE Ea i es — — —— an 7 yi 7 _——— -_ -apeegaeae * feaa a FREAEORAAIN corrornearion If. DESCRIPTION OF INSTRUMENT SYSTEMS A. Air Quality Instrumentation Nitrogen oxides are measured with a Meloy Model NA520 analyzer. This dual-channel analyzer is based on the chemilu- minescent principle, and continuously monitors both NO. and NO. A subtraction circuit in the instrument provides a continuous NOprowtput, but isi not used” im Radiam's tsysitem.9)iNOn a's, eal 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 wNOe, output of the instrument. This instrument nas a minimum detectable sensitivity of 5 ppb (parts per billion), anda (limearity 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 scrubber. » The Model SAL&85 is a ,econtinuous andlyzer,; and, utilizes the flame photometric principle of operation. The minimum detect- ableusensitiyity isdsappb, and the Linearity is ye 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 sensitivitys Ue: 5\\ppbtand, the lincaritysais 17, 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. IT C-468 Samet mihive Ty | abt AeSsit obott nye. Pm BOs Ch ee P hs miye tireelan | ay wir i mig oo) & % » i! wi 40) , melt ae " >) me .conglens ay fi \ | zie te Mex BI5qo LG bat: Li) oe (Orc) Cre is ae [ of . sbos ane Bae k Yadisons f oct 4 # RTS > ae 2 Ma Tebott ee: ; a3 wr i a? sinned . - — jo. + J mae nhs= sg “Fr ie Se wn eis feta bg ha gAT —- & 4? oe if ath, b ao Piahirctot 3 F in ps gaa ee po hee ut : 1 i a a) 9 : ae ey 7 pis wth tet —- ate act FRAAESI LAE corPorarion The air sample is drawn in through a glass cane and manifold supplied by the Ace Glass Company. ‘The system has a 25mm dianeten., and a constant aio ilow thiaough the system is provided by an air pump rated at 60 cfm at 0" head pressure. The manitoldynas sampling ports, to .zhiel 7;) teflon lines, tothe instruments ase connected... All joints in ;the samplingwsystem are securcd by O-ring compression fittings. The manifold is contained in a heated (100°) chamber to prevent condensation of moisture. The teflon lines from the manifold to the instru- ments are insulated with 1/8" wall thickness rubber tubing. The trailer has four heavy duty high volume particulate samplers (li-Vols). Fiberglass filter paper is used Eor collec- tion of partrenmlate samples, and each filter is broeughe to 2 controlled humidity before weighing. Each Hi-Vol has a flow recorders to peumit wis ad “acon } hee: weaves heenss3ox't Lagi i T stl vd Be brim - mice Vd bet a : y : ae, : » saa tute so1 én: ieyilhcke) 4 5 a ae eee ® = Ss i ioe -P a - we ob tobe wen y. anh Sine S nallaieal is nl ; Du $8 \Buses wa ra ae id ‘ nal Loeiry «e ne iy = = - id has a 18h eh 7 7 a ne OL: 5 4 eae n a ia ie J asf a i) an RAE PAAR] corPoRATiIOo“‘s obtained 24 hours before, and if a drift “in’excess of 10pph' has occirsed, an excess zero drift light for the channel “mm quest ron is turned on on the System Status Panel. Next, span gas is supplied to cach channel and the computer decides when a stable span value has been seached. hrs Value is xecorded and compared) to the pxe- vious days value, An excess span drift light om the System Status Panel is turned en 1 a driftlexceeding LOppb oceurs. The instruments ake then returned to the monztor mode, and afttcr tve minutes the computer resumes data taking. The bottled NO gas used at each site was cbtained from Precision Gas Products. Pre-purified prade hydrogen "as used* ian the SO. analyzers. The SO, permeation tubes were manufactured by Metronics Association, Inc, “Their output has been verztied@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 pex molecule, thus S02 can be used to calibrate both the He2S and SO2 monitors The Model OA350 ozone analyzer has its own calibration system which provides a zero check and a span check. The ozone calibration system is verified by comparison to a calibratcd ozone generator maintaimed an Radian’s laboratory an’ Kittie. ihe Medel 8200 total hydrocarbon, “methane, and ‘carbon monoxide analyzer is calibrated with undiluted span gas obtained fron Airco s Rare: and Specialty Gas’ Division” This span ‘eas contains methane and carbon monoxide in air, the methane being used to calibrate both the total hydrocarbon channel and the methane channel. The Model 8200 is zeroed with air from a II C-470 a= a2. ——— va, Gp ter3 on 4% nsrtven Oa Mat bebhbsovy seed aaif. dig: y . (Os: 8-01 ny. tay abya! ‘ , V6 Ad | iy j , i _ - a LG ; eae oat VG. att ts “16 iret ; ' GQ if : copy irae £ ne sions! “i o2 ibnoqany seat a ati hia rit enge vera “a s< “etnitittes ea hoe od ‘nits p08 auis .ctosuben, 1 igs ssl 7 Se ; _ _ [= 7 i. ine ery a Bell Bete eo. ae 5 7 oe er iad Bierce SHENS-WEL AO Conor oat oe mqe: we bon | Soak weiss 6 a VET pak 7 a : - a ae tan satin, el / pas sg Bz « Awe Dots aa . ee “4108 } iat em ivy Phu: oy. bys 7 ra ihe " 10 PRP\ESEZARN corperarion Bendix Model 8834 zero air unit. In addition the instrument is electronmeally ve-zeroed at the start,of cvery five-minute cyele. The Hi-Vol particulate samplers were calibrated using a Calibratavon kive from Coneral, Metal Works. C. Data Acquisition. < oystem 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 sec is equipped with automatic program load and power fail/automatic restart features. The computer utilizes 16K, 26-bit words of core memory. Analog-to-digital conversion is accomplished via an ADC built by Radian Corporation. The input/output unit Lor 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 progam storage and loading as well as recording. The power to the tele- type and cassette upits is turned on only when the unit(s) isto 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 babheries, suubehes; all trailer systems to batterysprovided power. If the time Woltage is restored before the batteries jane discharged to a specified level, the trailer system is switched back to-line power. Tt @=471 —— - Bale fs . petazaveno | ywagumotarni\ . Porte y aha if J - ro\s PET TT ft is XK) {Te j ¥ (ond ie? P Hlg eropelwq gents C5. 127 ini er i BE mo3¢re’ ats petmisy ges bee! bon ¢25.10 br oae | anyse a. aya a6 = <{-4 ¢ may im. c al s = , : 7 ihe: ath oz Esha tt S73Ssecss7s A ov hi 4 Hae ww — Lh ete! ¥ » i ag a * 7 ¥ a : ; re] sok wows i 230 St JSHt sIUAaans. oct' ith iw Avie : mal = Pras tap Pate ‘it bre 9a SBD fo¥ Se grr! sod bias. oarae . aoe ee : . @s (e)2in ott noslw viiwo ra gases ans justia sai ins hes s age : O ic bai gti dsovet Patel (a bawartaan age 2A we suphilie = amas ait Ae 26 t [one = Bone Ue ee 2 r a: hae no ass gx! Sen wed har O74 tee - ae sg [2 AAR SAR corporaTrion D. Meteorological Instrumentation 1. Ambient Air Monitoring Trailers Four of the smbicnt ais monitoring trailers are equipped with the following metcorological instrumentation: (1) dry bulb temperature (outside), (2) relative humidity, (3) “wind: direction, (4) wind speed, and (5) a tipping bucket, heated raim/snow gage. The temperature probe and relative humidity sensor are mounted 10- side a moter 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 aspirate: radiation shield) are all mounted atop a 33-foot crank-up meteorological tower (the WM-33, by Weather Measure) at cach of the four trazler sites. The wind-anstrumentation 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 frietioniless 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 frequenvy.. tachometer embodies several distinct advantages over the commonly used light chopper systems. “There are no lipht. bulbs or photocells so. bimn out: power consumpttonsius low, and the system is insensitive Go moisture condensation on dust deposition. The solid state tachometer is essentially free Muommaintenance with a, life of weld, over five years when operated continuously. The specifications of the W103 Cup Anemometer are as follows: C= 4 7,2 : eS i eccei ae: P 7 ese ly P , anu lias aaltoidiview oii Le fet jenaeyriani heilw gut - TOosumemnA Qi tdgtwesily!! ME\COIW fool ade lo 4aétedo med aes da i? iy Ltenol ada bree pat! tora it mye f ,aarinye AT if shy ivi Sef tetornorsm et? ofwanoh a einaos lig @eoedaptase: 2 Ps wietyo or! «4 relic ft ty opdaye ‘- w et onde gai7% | eel mee oo ett wot ! ¢2 54 9.45997 ie solkg . BAG qomaL 2 gid » stigolqua aR EEL au r ‘gheona liekw yg is Lang peta bilian tem a 7 _ ve * int bo tol on AL aoe ses p20: > a eed » ails ae Ait iG: deni: awa at fap ¢ ovdhadne js ia ‘> 17 EQ FABDEAAIN corporation 7 enecunacy 1 2 1, or. >> mph, whichever 1S preater. - Bearings: Sealed and shielded precision stainless steel. 2 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 Oto ShO- operations. The response characteristics of this vane are: - Dead Band: 0O degrecs - Damping Ratio: 0.4 * Distanee Constant: 3.5 feet = Thresheld:- 0.75 miles. per hour « Potentsometer Lincarity= ©. 57 The thermistor probe used in the motor aspirated radia- tion shields is the Model T621-TP1L&X Air Temperature Premium Thermistox Probe by Weather Measuxe. This probe has a range of -50°C to +50°C and an interchangeability of + 0.055°C. he out- put signal accuracy is 4 0.3°F. the xeelative humidity sewsor is the Model 2013 Remote Reading KRelativemiumidiiy System by Texas Electronics. The sensor assembly contains a newly-developed hygroscopic inorganic sensing II C-473 -_ > — - sities ' - 2 ee 5 2 a a - : = 7 _ y ~ 7 * : i -_ > ap P a on - sit oh hae il ey Lwwo¢cimiod rye i andl “he n mi "ae oe a pht “ ana hs ef abl uk nd aden 8 nls Mt wt 7 - er oe . ry” 20 ai BS F Sides (phe Ah oie we . co. won 7 : —— ie a : FRALEY corrvorarion element. Les cxpangion and contractiom positions the suspended core of a Wimear vannable differential -transforner, (LVDT).:. The absence of friction inducing, linkoses and wiping contacts minimizes hysteresis and improves accuracy. The LVDT output signal, when processed, 15 dizechiy proportional te xelative humidity. The specifications,.Of semis anstyument are as tollows: = Range of Indication: 02 to LOO; Ri - Response: The sensor response time to a step enange of 107 im relative humidity Ls. less than 2 minutes with ative sensor exposed to moving air. “ - Aecuracys, O24 < 150 Ri; 2 37 RE LS 95%. Mis 2 25eRo 957, “LOO, 11; 3% RH }+ : Signal Output: Analog signal of -150 mv. to +150 nvs wet electrical zero at 507 RH is standard. . Each-of the four monitoring trailers is equipped with a Model P511-E Remote Recording Neated Snow Gage by Weather Measure, in the @ase of this gape, the durability and weliaba lat of a tipping bucket gage are combined with heavy-duty electric heaters to make this an all-purpose precipitation sensor, Ehius gage may be used to vmeasure snowfall amd rainfall. An insulating cover of poly-vinyl@ehloride and a themmostatie control insure the proper gage temperature. The thermostatic control is adjus- table from 0 to 35° G. Snow salling, inee tthe inlet funnel is nelted. Ehe sesultine water (from raingor snow) drains into 7a precision, Ci ppine bucke!: mechanisin whieh activates a mercury. switeh cach tinepeme bucket Mipis and taps. The gape is eonstmucted IT \6=4174 ornament edeereh OT Capt Tot ox apes eCn ame 9+ att qyere.th ‘eaair 03 ¢F133 nett ype! Vie 4 bl: Seainidta otanuen goi4t here amggreines Wihsubs! iv spaiie ve Tht of yambmse* °°: Meviantoz © lanobtaoqict | paoifot ar ou Hieomarttems 2): } we’ [ha aes uel tert, ii if 2! [ , 2 7 7 Wm POOL o2 * pokes tht Le. OMA { “a art Bite jAg 1 Rp sgetts Ie 6 . gid ool 63 hanagee iva v2ae r iv % ts t 4 1 critics lo Breas s~aoneten as | ‘sitet ise nage ERAAIDEAAN corporarion of durable corrosren-resistant materials "to; provide many year svor Scivices Whe speermucations Of “this eae ase as Lolhows: 7 Orittees .G) 11renes weCilipaatenon: O20. “nel = Accumaey=, — 0% 57, (Cae eed Aer... 5 inj) = Sensom. ‘Chrome placed tipping buckets - "Switche werciry, 0.1 "second iebosure : "Heat ‘Control? “Thermostat” adpustment ; 0 toms @ 2. 200-Foot Meteorological Tower The tovger Das. instrmucntation at four Levels: 8 feet, 30 feet, 100 Leeke@and 200 fect... Atv aki four levels. “there ane: 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 lepse rate measurements tox the 30-fLooe to L00=noor Tayer™and” the 30=foot to 200-Lfoot Layer. In addition, ‘thiswsite has) a Precision Spectsal Pyranomete:, .a barometer, and a tipping bucket rain/snow page. The winded@rection and speed apparatus used at ench measurement level of the tower is the Model 10/4-2 wind sensor by Metecoxroloriedienesearch, Ine. Ginl)..*"lhis sensor has a SHOn potentiometer fOmuind direction and alight choppers for iwand speed, Thas scnesonens rupecd, woth an all-weather coaxial eup and Tr .G-475 - = ‘ 7 ay bal,* yt , 7 '.< am Ae a bi oad y Oo 0 shaves 0 eitke. 54.0 II C-476 Bet: wi fyigunh uth Wat al 343 cebrl! eas: varaiin i ents gotsio2 54 0% poe aot Soha a rt ex pea ee ‘ or eaamesic oct) WEEH: CAM — te its. ~47!* iggiot Dcbieeets i, ee ipo Oy soatst = itviw hosted qiine hoa ‘ “mah? n ‘ys Se annecaeaeeae aanek es balla a ip #8284 a Cm sib ‘inane = Oa i econypaed is 4 8 ' neal - iat: A-BNGE Rabotrvos> i US es ait 0 (7 EAT 7 _ | ne BRO sbtodran” ~/iko tas? _ ow Dy sie ; oe - : : ’ | one Pr eae walt » - 7 7 ‘ ; : "40 © * yan tee d it ans aatg Ce : ea | _ AL . ie . 7 inte a | % peer is i Fe/2LSEAAIN] corroerarion The relative humidity and temperature sensors are mounted within a power aspirated radiation shield at each tower level. All aspirators and sensors are of the Model 840 Series by MRI. The aspirated shielded housing is designed to provide maximum radiation protection to the sensor. Ambient air is drawn into the shield and across the sensors at approximately 15 feet per second. This intake air is essentially sampled from a hemispherical space which is approximately 3-inch radius from the tube opening. Speed of the incoming air at the periphery of this hemisphere is approximately 1 mph. The temperature sensor is comprised of a dual thermistor and resistor network. This circuit provides a linear resistance change with an air temperature change. The relative humidity sensor is placed alongside the temperature elements inside the shield where, it is exposed to a constant flow of air. Cireulation @ to both sides of the sensing element produces accurate monitoring with a good response time. The specifications of the sensing ele- ments are as follows: Temperature Accuracy: + 0.25°C Range: -50°C to +50°C Humidity Necuraey? 213 107, RH Range: 0% to 100% Relative Humidity ® Measurements of temperature difference are taken for two layers, the 30-foot to 100-foot layer and the 30-foot to 200-foot If (G-477 Lon ee —_ . ale aoe use OMG Seamer y9 6368hse sre I091e: KOR NEM sviscl or ae? _ hovel tame? cas fa ‘tislin oo lveibay bevasiqva Ihe o Ali see Tew OO2 fabot afd Oe awa ietochs: bus agoseriqas 106 szizee gor Gerglend 22 yilivind babiisds beonsiqes alt Biche capidmA 8 apeGhe oui! ot colteadany) welteethes antna: Ja aan@s odd atease.Jline-bisahe ai “i Lekadaes a5-yin sipinh eset (beopde 2. agihes: Adgi-£ eloiimixotgge st Astw songs Paite 25 va gatioamt ot to beet E@/AESELALG corPorarion layer. The thermistors and circuitry used for these measurements are separate from the thermistors measuring air temperature. The use of separate thermistors and circuitry to measure AT allows for much greater accuracy and resolution in the measurements, which is necessary for stability assessments. Two AT thermistors are at the 30-foot level, one is at the 100-foot level, and one is at the 200-foot level. All of these AT thermistors are mounted within power aspirated radiation shields. The specifications on the AT instrumentation are as follows: fe) * Accuracy. .2 O21 C o. Rangerot AT Careuxt (Lower Level-Upper Level): + oP ieore 8 All instrumentation, except at .theseround level, is mounted at.the endef 12-foot. setractabhke booms... These. boons ied) 0 33-inch box. beams .whachn ace on solless mind can be setracted £o “Ehe 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 witly 3" of radtal ace per EIA Standard KS-222-2, to suppertus 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 g, twolbasespuound kits and one anchor ground kit. The cable-type Safety Cimmbing Device consists of a cable and attach- ment mechanisms*withwablocking si¢eve andesafcty beltisiic tewer ts lighted and paintedwaccording@toe FAA specifications The®sicnatic’ Grom the vower instrumentation areticd from multiple strenalycablcs ante Mxinsmitters mounted at the base of II C-478 . " — hp cgay ag ty oddige onedt semecd @fdasan tts ei-" Because of its location and the irrcgularities of the Surrounding terrain, meteorological patterns ave’ varied here. Wind instrumentation is mounted at four levels of the méteorolopical tower; $6 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 micrometcorological circulations. Occasionally, a weak anabatic flow influence is experienced. However, such as nok Yee case wrth the three Vowest measurement levels. To varying degrees, these levels are influenced by both ihe, Katabatse and anabatie erreulation cells. However, when SLSOne presere pradnene torceés exist" in the wer ior and ‘the synoptic-seale wind flew is'"strong, all four “tower levels wil) >? retileceta gradient windetilow: wath the winds ivercasing im Stren watch aiverecasine lie tet. TC - 465 4 4 win neddu ata Ser, ‘fam tezc.1aen af? * seribovowxus a te dive % i. oa ° uf iy <. ty ps w 1% GoOt mad od trosngnt ktond Wines & de gat Gi! no wh Mypest elias oof a9? YA S2ic4a8 mii T isf) ; Tt aa ais ijenial i fawit I gar hetite. Awe ort o 4 = a | _ on —s w=? i 7 - 7 _ - a fe? oii ay rae ani eenrese ala ar © ' sro 04 fas eats! Tare arts to Lovet a a = [RENOWN commomrrria a Trailer O24 as between the Piecanee Creck 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, moth, and east, and slopes upward toward the South, ingthe dasection of the metcorological tower. This site is ime transition zZoney berwcen the micrometecorological effects which prevail in the valley and those meteorological phenomena affecting the: tower SiLle. “VAS. a result, the meteorological parameters measured at thas 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. Howevei,; gradient wind flows generally take precedence over terrain- induced flows at this location. The terrain atop the plateau is generally barren and fairly rugged, with a few scattered small trees. The topsoil dries rapidly and is very fine, resulting in blowing dust when dry, windy conditions exist. In the Piceance Creck Valley, the terrain is fairly grassy and flat, with steep valley walls on either side. Strface winds ane normally rather Iaght am thas valley unless channelling effects occur. During clear nights with rather light pressure gi adLene. induced winds, rapid radiational cooling will occur in the secon because of the barren nature of the terrain and the generally dry character of the aix in this portion of the country. As a result, the diurnal range of temperatures will be extremely large. Because of the katabatic flow im the valley, wigsivetine temperatures will generally be lower in the valley ‘than om thie plateau. During thelwanter, especially, temperatures in the valley may be 20°F lower than they are on the platcau during the early morning hours. .In particular, the dsainaze effects will be spectacular at; Trailer 022, which will Of tC CxpcEVence II C-484 PINOUT enema mies 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 naphttame ground-based anver— 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 threughout the monitoring network (on the plateau and in the valley). II C-485 * ! 6. @ FRAO VAN corroRaArTion IV. 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 “DIGITIZING SYSTEM" indicates the entire data acquisition system and downtime hours appearing in this column and, therefore, means total loss of data. These instances inciude, fim addaitaon to computer downtime, power failures, no power available, and self-automated shutdown periods such as during air conditioner malfunctions. Calibration time is not considered to be downtime and is, therefore, not included in the downtime figures. The amount of time used in calibrating the instruments is given at the bottom of the downtime analysis table and is reported as total calibration hours for each channel for the entire month. As is evident in the calibration figures, channels can be calibrated independently of one another. No calibration time is given for particulate monitoring since Hi-Vol calibration occurs infre- quently and only during the off-duty cycle for each Hi-Vol while another Hi-Vol is taking data. II C-486 worturouges eee ELA IONS 99% SOMMIAEA dirry os zaseien andt3axeqo sna Riabes t07 nisses shay Hoes 472 pers ni 7oft0 dia Yo doh Ritloeq: 74% (675). eh) Sasa peded 7 aero ibak "yr POES times. tip . et piecsi! «inh Re Gayl Kqame 2 ShwOg 2a scveb: dogg Bol: Foy owoltule bot énospa- Sieg aise ot fee Bs scent 7 Ee a a “At dwal Hd Om eeee e a SD fay e¢eeeeeee e. GS 16 —OosS 850 8 9 2K wn SS eCererers e "> °a °0 °@ S¢cH “yc “bz Luvd LI3fOdd WO SIVHS 8-9 HOS SYNOH JWILNMOG i) 2 310V4 » II C-487 UE SWIi NOLIVuaT WW ag on Lovet *y aw Gove t aan ia 6c7at ZT ou Ro/et we oa Lovet Si ° 4 Gerat ° a oe C2vet a "os ore. a) vie S27Gt mal eel COUN *4 e! laces *Y, oat neve t *¥ eu Oe F “it ge) Qik “ai mat ZUTEN a ca Giver "TT | Gi/ct “4 ae Palevacar a ay Wal ° A val Civ¢ “aah ot Divert seth sal! vt/set ree ea Cy a! my "A uw /ct *y a Let A ba 9 fot *y = Gayct 'e ~e p fet *¢ uy ©. ret ba, ak 2 /ét *0 *vu tA XON WALSAS 31v90 pe oo iii ig i\ ies & fas tua SND Zend “ge ea liver mer GD j% fern an *3 *4 *a wg ig Anil eNO i esar iva L ie t ie ® ; e Tevet *6 *¢ "4 a a a “1 oe 2 ei *y *v *Y t ag i ; oa 7 a, a) *y 2/2 Me “ ; ; . = a, aezg/ct *2 *Q "9g *G J a : a 6 en s ®*pe #4 Q te *” 1, %) rf) ; ro Oke *G ey *4 “A roc , ms ee e (a, baa, *o Ste He “¢ ‘ ip *y *A ay eve T mil pee "e *” “9 *Y pe =o ey sey | *g *aA *4 *% te “i a oe ) ba, “y *4 "5 v re i bs *¥ *v “4 *p "9 i one se e e La UG ‘ ‘ 2 a ‘Be *Y BG t ei7eat ; 2 e e + . ig *Q *v *y °¢ a aide wee e 6 ,; A s, ‘, + “3 - a ve Givet e e v : ea ‘5 *2 ea’, ba, a) vd vise ; , °Y °@ *a *y¢ ne Sa eon | ‘2 " é ; ‘4 *% “ve eimet *9 *2 *o *Y Q ) Ue hee *o *Q *9 "Vy *ozd *a HE ee e. 6 e baa, Mp , + : : o 3 ‘y “4 6 7c} , *y bal A ‘ 1 *9 tH “2 "v2 *2 vy ; AS a) *B *0 *A “ye 2 a i ‘ is a wigs Marl “9 % Of Ye : y : . *¢ “A st Cevet ‘4 th : os a) aot 5) Ve iG e A w& ; : *y 7, "3 A *) : : Aa. 6 é *y *a Pie °*g ute ‘ : *¢ Le T i “als es : a = : ae WAHLSAS 34Vd ; Luvd zos ! i se a = SONI Zi itt tou) Gaally ew L34afr0uUd WO JIVHS ee. 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AS » _% $ es » §4 > gi¢ et a *2 “a *2 *¢ *2 ‘a *” *¢ is *@ 8H ‘4 *o 9 *a *A baa, ba ry *9 *2 *Q *y *2 *¢Z *2 ° 4 *Y ot sa 9 ‘Go ‘4 * “9 *H *0 at *Q *4 *0 gai aa) *a *4 *@ *Q mn, *2 *a *Q ‘A “2 a *a *9 *9 *¢ *4 *G *6 *9 *2 *9 "9 *4 *2 *A *0 a) oat) “2 *2 ot a) *A *¢ a on *% a”) *9 #9 *y 59 ‘A ‘4 *g yy 7, eat "A *9 *@ “2 *9 “A *4 mat "9 *Q *9 *g ‘a *9 *2 *( °4 *8 *Y “4 *g *Q *2 "4 ‘9g “0 *a *Q *2 *Q ‘9 *Y ‘A °a *0 *0 *¢ *2 *y “A ‘yj *u *y i! *2 *2 *2 *@ “4 *Y “a *% a) “2 *” a”, “A ‘a *y *Q “Yu “a bal? ®4 *¢ *4 *g “Y * *a *¢4, 4 a *9 *2 *a *g sy “4 oT *¢ *q *A *9 ‘a aa “Gg *9 “2 *Q et *A *A *a “9 *O St °g *9 "2 *2 “0 *Q ‘a ‘0 “Qa "pt “0 *% *Q eat et *Y *Y *Q ar *Q *4 “4 ‘a a *a “4 “4 =< “oT a) *0 a) *2 *p *y “0 *2A “vz *9 ‘9 °9 coe mit *2 *B *u *b we at emp me *¢ *g *2 *2 *9 mi *Q ont *g *Q *9 “2 *4 ‘9 7) *g 7) *4 “7 -T “9 9g *a *4 aa mat mt *Y i ' *Q *0 *2 *9 *g *0 *4 *o *Q *4 *. *A *9 *¥ “A bare, *A “A *9 *” TLQ 0 odW3aL HY OM Sh dw Ha QM SM memwwmwone | 4ahijoeeerees sewn menne | dei omnanae ban saa 4 *A e a T “A *Q *y *¢ *g ba *Q "a °i4 a * i é e T 4) *¢g *g *Q "a “4 ey *4 *g 0, “1 a é if ) *Q “a bat “a *o *g “0 * “¢ “a *9 “2 *¢ “2 ‘a A “i *0 *” “1 “3 or *¢ *Y *Q aa a ' “A “0 “A” *9 *g a *2 dwat Hd G ay, * i) *¢ *G Cm (Ga os °a SwIh NOLLVaeId “0 “vi Tova *2 v2 ag/é “0 | 66/7¢ on: Set ge/2 °@ “vie LOE "a “Vig Go/e *” eee Ge/e ma itr ve/le *¢, yal SELG °6 a) GOle *2 * 44 Te/2 “a =a Wo/? a) i! 61/2 a) 7% 8 hAe a, out Le *g “vie Q1/) °Q “UG Gt/e m7) aC I vive a) a SUHAs °a A Zuse °id : lol °O baa) vtlsS™S *¢ sa ' 5K /ed * wa o 72 *@ fe, Lode *y ot G9 Fe *@ wa Ge *2 ‘a b Ze “a at € /2¢ *¢ oot 2 72 “0 ‘ot I 72] Sid WALSAS 3140 Sint 2 ee LISLOUd WIO SIWWHS gd=3 HYOd SYNOH SWILNMOG ° Tigi iavi Ged Hd veL ia a a *2 *¢ *¢ +A *9 baa) *Q *Q “y *a *a *A "4g “9 *4 * *¢ “4 i) *¢ *9 *Y *Q *Q “a *¢ “9 *¥ *y *9 Lr, *a $a *” *2 “4 *2 +g *y *6 *o #1) *9 *3 bat) mt ‘a “9 *Q *Q “9 *¢ *9 *¢ *4 *g “4 9 *g *% “9 *Q =O ‘oO “9 “a 9 ‘9 “4 ar.) aay, 4 *Q *a@ *g *9 A 9 *9 *9 Yj *” 4 *Y *O *g “6 “4 *Y *y *9 *4 *@ HY aM Sx gt *g *9 “Gt °G werk *” “A *g *g a) om *0 ur “4 ec “be a) “be "A © ie “py *y *bt *G baa, *A *0 wee ae) *” aA ipa *y “pia *g *@ ray * i °g *pe Gas “oe ve aed * i She “y “pe *B “tg *g *y a °9 *g “oe *9 “0 “9g “pie *Q * SoH Lavd 5 Oak SuIL NOLivssetiy3 *Q “A Lorn "2 *yj uosel *2 *g 62/2et *Y *4 —ee/et “J = L2/at *y "2 ad/cdt *Y *G Gere} | “Ge ve/ct Sarat eat Reset “tt *u eovet “ot “4 Tevet pt ra ge/et +4 3 6t/et a, ks al/et °a "2 LUKE a) “2 Ot/ét “Yj “a Gt fet ba) *y piel oi *u SL /et °9 “a ohne F sey! a Tine. *g oe Ub/et *g a) 6 et C “A Piayieia| *6t *4 2 Fer at *2 9 /et *g ey S /et a”, 4 AL *9 “¢ So fet *Y *a & /et ‘% ban) te Her rAD RS WALSAS divu ONG LLC LOALOXd WIA SIWHS gd 804s SHNOH JWHILN«AO0 adv i oot Nd ROCHR SERS on Py r 2 Sia Bo FE eng | \ rs a & we yey es ilvad II C-492 74 oe eae. ‘de> 864 ewie a LOE JEP SJkMe G=> 495 aNUON ketene - : : ; > oe a a _ = SS tas ci “are EOE. ESEZARY cerPporarion V. MONTHLY METEOROLOGICAL SUMMARY A. North American Summary The month of December brought rather mild temperatures to much of the United States. Upper ridging prevailed over the western portion of the country during the first 21 days,.of December as the mean long wave trough position was established through the Mississippi Valley. During »the lastiten days..of the month, the southwestern United States was dominated by a persis- tent upper cyclonic circulation, which brought heavy snowfalls to much of the region. Zonal flow prevailed over the United States from December lst through the 6th, from the 10th through the 14th, from the 18th through the. 21st, ~nd»fromsthe 25th through.the 29th. Meridional flow was dominant from December 7th through the 9th, from the 15th’ through the 17th, from the 22nd through the 24th, and on the SGlst. Split flow prevailed on the 30th. A large closed low at upper levels dominated the eastern third of the nation on December lst and 2nd, causing the formation of an intense surface cyclone off the Atlantic coast. This low brought very heavy snows to the Northeast and Atlantic seaboard states. Upper level cutoff lows dominated the southwestern United States from December 8th through the llth, from the 23rd through the 26th, and from the 28th through the first two days of January. In general, average temperatures in the United States during December were above normal, except for the southwestern portion of the country, where cloudiness prevailed during much of the month. Precipitation amounts across the country deviated Pi iG-493 ‘ » 4 — bes - { ig 8 ‘ | To 7 ’ ae) J, atl #075 5 ii 3oro iie Qo! 902 eff dau OL ads wovk .1t8 Hd! tulle a9) a Gaees fae. Sd) eo? ede Sed S Siz dquetii PHL wt ott geared fat Sets sa); GOT? tiagimol ac.) r Fanoihirem .s5hf i 9 eis ova .fat! att sewn 720. eds 7? cf 22 ada! i faz belteve-< voll giiat : ate ge bee. . ys? eds © 7 —_ és » ’ - : a # besenimot ejevos tigi? ae wal, terals inlA ch y no mite Jel tefasont qe notian.< iveto & at tisiess 3 ‘Yo dnd sue suanie. gedasi? ng ‘quite: po ald ae Suh ai eumel q seu or trond wot cidl 4200 > ae * | 1236 Bisodsap 2S Mie. ar ae she hat x paloma sit aS jot: outt net ’ att =! 56 i ery ex » se RADIAN corporarion little from monthly normals. Specifically, the Northeast had average temperatures which were much higher than normal and precipitation totals which were slightly above normal. for the month. The Atlantic seaboard states experienced above normal temperatures and precipitation during December, while the South- east had above normal temperatures and slightly below normal precipitation. The northern tier of states also had above normal average temperatures during December, while experiencing slight- ly above normal precipitation. The central portion of the United States was affected by above normal temperatures and below normal precipitation. Both the Rocky Mountains and the Southwest (in- cluding Texas) generally experienced below normal average tem- peratures and slightly below normal precipitation. The western United States had above normal average temperatures and near normal precipitation. No major (extremely cold) outbreaks of continental polar arr occurred in ‘the United States during December. II C-494 - J , Merete om = ' ° 7 alk ale liad : nm - cc . ‘w FREES IAARY corporarion B. Meteorological Statistics in Northwestern Colorado During December The month of December brought below normal temperatures and slightly below normal precipitation to northwestern Colorado. Seven maritime polar cold fronts passed through the region during the month (eécember 5, 13,.417, 19, 22, 28, and 30). The cold front of the 22nd was exceptionally strong... Im addition, an occluded front passed through the area on the 7th. The last ten days of December were much colder than normal in this region, and heavy snowfalls occurred on the 29th and 30th. Grand: Jametron received 2 total of 0232 inch of precipitation during December, which is 0.23 inch below normal for the month. The area received snow on twelve days of December (December Sth, 7th; Jith, 13th, 15th. iGth, iyth. 20th, 22nd, 29th. 30th wand 3ist)., The heaviest snowtalls in Grand Junction _oceurred on,the 5&h and 29th. Heavy fog, which 1 reduced horizontal visibilities to below % mile, occurred on the 6th. The area in general had twelve clear days, five partly cloudy days, and fourteen cloudy days. Sky cover by cloudiness averaged 5.6 out of a possible 10 during the period from sunrise to sunset and 5.4 out of a possible 10 during the entixe 24-heuz midnight to midnight period. The area received 56% of the possible sunshine during the month. Northwestern portions of Colorado experienced some periods of poor dispersion and air stagnation during December. The valleys were particularly vulnerable to these stagnation conditions because of cold air which became entrenched in them, thus enhancing poor ventilation and trapping conditions. The Piece -495 -_é - sobmer $ wnied oD Sead iiic se : a , goku si reals tucaea hae Jersrse oi seta aT = nites “st myers Ke. ae EMbuotS 1s $7102 bis 1 Sen “iuoty ag a. == beled ¢ mls | ; aoe Oy er bbaas: ee 20°" 2 Bagn ze: ; oe eerece =o ee pany ibe if ade a to awe ‘ ra bree aa sar’ 08, ov ey ein av Sieg. +t ‘eit JL OF aH . a 7 Bitton ila su i F2EREDALAEY corPorarion following official National Weather Service FKUS Air Stagnation Narratives pertain to northwestern Colorado during the month of December: December 1: ''Morning dispersion conditions . will be poor over a large area of Utah and Colorado southeastward to Texas on the morn- ine o£ the: 2nd: " December 2: "The stagnation area over the central and southern Rocky Mountain States today will be depressed southwestward on December 3rd and 4th as a surface frontal system moves across the top of the upper ridge. High surface pressure gradients in- - dicated on the latest prog package suggest improvement in dispersion conditions over eastern Colorado by late on the 3rd. However, locally poor dispersion is apt to persist in the valleys of New Mexico and western Colo- rado through Wednesday morning due to con- tinued light winds and the trapping of cold ais" December 3: "Stagnation conditions to dimi- nish during the next 24 hours through the Rockies and southwestern United States as the ridge is forced southeastward. The upper ridge will continue to cause light winds through the 4th so would expect re- stricted night and morning dispersion con- ditions in that region into early on the 5th. Increased circulation through the Rockies should provide improved dispersion Condi rions am most of Colorado ven the 4th." IL €=496 thos oc ’ stth "Ba ~ ats fo Steal yd! nlesey as Igy t noe xaiie! qs < 5 745 ba baste xe wos nage oe pbs) ihm Paes he ? Ghana pike ree Ee RIDE LARN corPoRATION December 8: "Expected deteriorating night and morning dispersion conditions in Utah tonight and eastern Colorado late tomorrow as the upper ridge moves eastward into the Rockies...Conditions in Colorado will improve tomorrow night as the front moves through the central Rockies." December 11: "Poor dispersion will prevail at night and in the early morning hours un- der the surface high crossing the Great Basin for the next several days, but the movement of the high and forecasted positive vorticity advection should restrict periods of poor dispersion only to short periods in any one place." December 17: "An area of negative vorticity, associated with an upper ridge, builds into Utah and western Colorado by the morning of the 19th as a vorticity minimum shifts into that region with associated light winds. Dispersion will be restricted mainly during the morning and nighttime hours and mostly in valley locations. December 23: "A cold air mass moving south through the northern Rockies will cause locally restricted dispersion in portions of northern Utah and western Colorado as winds diminish and cold air becomes trapped in valleys." EI G=407 tislmiev wv )say, ara Oi" eamnd ABE Land aah hs IS4q0 0 ; ® gate Gat 6: 1 ad whe Salo? ims : ab aside machetes. Edy ht -_ abs tw tee! Des dafouane oat: 4A pads: A aaa be, ore 2207 Gt 1; izren2ta }: boa “ —— a ha rs Tem au si4 ee VS< <>! iz . mets dT ma st5 cig J" 5 i” ©@ 4a ew 9 Aes a F2AARSILALY corPorarion December 24: "The ridge in the far western United States is forecast to break down during the next 36 hours allowing increas- ingawinds»and»circulation in)the Pacific Northwest and flushing out any cold air that may have been trapped in the valleys of the northern Rockies. Area of restricted night and morning dispersion to move south into the Great Basin and portions of Cali- fornia, byntheanight, of: the] 25th. December 31: ''The ridge building into the far western United States will spread an atbea Of stagnation and locally restricted dispersion through Oregon, central Cali- fornia, Nevada, northern Utah, Wyoming, and Colorado. Stagnation will persist in the Great Basin and central California into the morning of January 2nd, with the trend toward deteriorating night and morn- ing dispersion continuing through the en- tire region." In addition to being subjected to periods of air stagnation during December, northwestern Colorado also experi- enced several winter storms and some extremely cold weather during the month. Travelers Advisories were issued for heavy snowfalls in northwestern Colorado on December 4th, 5th, 3th, 21st, 22nd and 29th. Heavy snow warnings were issued for the region on these same days. As much as ten inches of snow fell in portions of western Colorado on the 4th and 5th. Selected portions of the ABUS National Weather Summaries for December are as follows: 1G yC-498 Bmoisss (URI Sapgwe vat wit nb nah be Ge GEE actos Be ovat 92 Zhao TR RE dee ED thos bit rch ACswoERS axel BY GRep ind? got yp x at ai fot ni nate: bam. bate -orek «3 ~ :siclA ois sad pesto athe J0¢ oo 7 2-9 Jone erde Gaeis ascw eyed om ylveiggiyre, .apee o:' nl ofdeesgeee Sera! Str am: Yo favel 200%-6 mgs Lap S20 10: url. SEiiaoeee aaive:! ea? ei: oie: syaod Jesteld oAy bei! +! Looe See ; “Ye <(bniw Fo Joh .vbeel. ait pei oe “ A Whtalet bos coguttinteyeis Gmitsdat> wal Caer eee eds J a. ue saliew 2143 400 Yaldsst. 48 > -yIe7aGNe aoe iy roe¥Pads pt wanes Siuthvantes leanrwik aratsomy ¢ ete 1G 3-4 sl Ae « 7 7 _ 7 = > > a : ; uy i ‘ “oe 7~ ae a c 7 7 _ READIAN corporation temperature difference between these two levels was often positive (inversion) during the daytime and negative at night. Because of the frequent snowfalls during the month, the monthly average relative humidities were rather high, both at the valley sites and on the plateau. The monthly average relative humidities in the valley ranged from 71.9% at Trailer 020 to 74°4% at Trailer 021: “On the plateau, Trailer 024 averaged 68.67 relative humidity, while the four tower levels ranged from 67.3%. to 71.6%. December 7th, 29th, 30th, and 31st were the most humid days o£ the month in’ the-fzact €-b region, while@the first four days of the month were the driest in this region, particularly so on the plateau (some relatively moist air was trapped in the valley during this period, im addition to the fact that the, lower nighe— time temperatures in the valley on these days resulted in higher daily average relative humidities at the valley sites). Due to the generally cloudy conditions which prevailed inthe Tract: C=b regiom-durine the month, “in addition to the fact that solar elevations were’ low @inter solstice), solar radiation totals were relatively low during December. On a clear day in December, about 165 langleys should be received. The only December day when the maximum possible solar radiation was received was the- 9th (downtime, especially on the 3rd, prohibits a complete eva- luation of “the month)> “The 5th and 7th of the month received only minimal amounts of solar radiation because of excessive cloud cover. The highest hourly radiation total received during the month was 36 langleys on the 3rd and 9th, from 1200 to 1300 hours, the normal period of maximum solar radiation. Daily averages of the barometric pressure (limited data) ranged from’/53"3' miltibars “on “the 29th to 79122 millibars, on the 30th at the meteorological tower. The standard station ii C=502 aero oo eV evizieoay negig any sieval o@1 sea piswiad wanes? ) 16 © 1 2sariqeey Augie os Gvidhush Uifmmitvah, Adz 2c: wh Cebtereweds ed: , ¢tate ede galouh ‘Rf niwona ‘giipe®? afz to -3unGee ets me Mo uetie: szav a.0fEbtow! s¥iscts: ogres efAsgee | oe ethos ori't F -~ste af go oni wade qed pee ibe £9) gn ‘* yadiev >¢3 mk telpehiaal masts Gado} ~I50 s2hhext Sa-Gee ame = oe } needs - f of? alia OC hou ebra teas | w oe paste (As tedwaned (Foi Soey | ala iat dirom oat te oyah ni a . ae ERASERS ILARY corPcrarion pressure at the altitude at which this barometer is mounted is 784 millibars, using the standard atmosphere as reference. Winds in the Tract C-b region generally followed the same pattern during December that they had followed during the preceding months. The katabatic/anabatic circulation cell dominated the flow in the Piceance Creek Valley, while the plateau remained in gradient flow with far fewer mesoscale effects superimposed. Actually, the katabatic (downslope) circulation was much more dominant than the anabatic cell in the valley on cloudless days with weak pressure gradients be- cause of the low solar elevations and resultant lack of insola- tion to power the anabatic cell. Resultant wind directions in the valley, therefore, were east and east-southeasterly, generally following the contours of the basin. Resultant speeds ranged from 0.6 miles per hour at Trailer 021, where nighttime winds are generally rather light, co, 3.1 miles per hour at Trailer 022, where the katabatic flow is strongest. Scalar wind speeds ranged from 3 miles per hous at Trailer 0207 to 5 miles per hour at Trailer 022, On the plateau, the resultant wind directions on the meteorological tower ranged from 239 degrees at 30 feet to 249.9 degrees at 200 feet. The general wind flow, then, was west-southwesterly with a general veering in direction with height, as would be expected. Wind speeds, both resultant and scalar, increased with increasing height, also a normal occurrence. Resultant speeds ranged from 2.6 miles per hour at 8 feet to 4.7 miles per hour at 200 feet. Scalar speeds ranged from 5 miles per hour at the 8-foot level to 9 miles pex hour at’ 100 feet and 200 feet. Trailer 024, between the meteorological tower and valley sites, demonstrated an intermediate wind behavior. The resultant wind direction at this site was 177.5 degrees. The resultant wind speed was 1.1 miles per hour, with a scalar average speed of 3 miles per hour. PIV C-503 >=. ; pea 7 : ‘Ss 4 7 - | padleseas vei layw-@43 qi enoidseudb baie tras ‘root a qiis ph "?<. «¥Yloeode 4 d t-7 iti) 7e0S hognas bbe qa Soasiine. ikesd ots Ye _" smi Itgin 1¥ arly ‘£0. 4a] 2677 26 port 247 16 THOT howd lim I £62 ,gAgt! bate ai a tre et wold Srandescat - 7 7 - et a8 re a, oo OFD “iabiar? wa> y : 1 bo ats me v0 = par» Pitadege ss 27 , Onere 7 oe or a6 30 CS @usl bag BA waew yo asy besa atic Ol : we +o a} girkao: bese i a atiw i ae 7 SnitwW vias de ine te iiss fd sen abi ahoeei » OG, 2 maori 1396 t FRAAESEAAIN corporanorn The 2lst had the highest daily average winds, particularly on the plateau; while the 9th, 29th; 90th and 3st had the lightest winds. Winds were generally light to moderate on the plateau during the month and were very light in the valley, low enough to cause impaired dispersion and ventilation on occasion. The strongest winds experienced in the Tract C-b area during December occurred during the evening of the 21st, in advance of an intense winter storm. Sustained winds of 40 miles per hour or higher were record- ed at 100 feet and 200 feet for a period of about seven hours during this episode. The maximum five-minute average wind velocity record- ed during this storm, and also during the entire month, was 52 miles per hour at 2005 hours on the 21st at the 200-foot level. II C-504 PATA corPoRATION Vix 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 conversiom., The lower threshold £or all Analytical jan struments is twice the maximum noise level generated by the in- struments. “This tower threshold" 1s") ppb tor allinstruments: except for the ozone analyzer for which it is 0.5 ppb. Therefore: 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 entry in the data presentation which does not indicate absolute zero concentration. 7 ALL pellutame data €except for particulate data as taken at the monitoring site im integer parts per billion (ppb) but is presented here in micrograms per cubic meter (pg/m?) PH €-505 Wao ws Oh HoCeT aa ATA panel eae Sea “03 spitsesmwvs Q260eisat watdes: «):19 eoeetg S22) 347 peetde andic: ines wale da ated P baw teotiox: conges; Sendyliég ‘io ysiliddiiay aay (npko ahha at . sae ba pmijacc! (yl ageyenrrag To Po, aaireorsqult, Peroisorwt 242 osavttigk anos wm ; stab £EA ettneslh balw Adlw ants crane i rear nism (29 lq Sied-de) if . is ta oitomls ira epiele-ay lt Ot sles suptadadd golgersen E2VAROVAIY corPORDYION assuming standard temperature and pressure of 25°C and 760 mmHg @O13s. 2 millibars) , respectively. The scale factors required to convert wg/m*? at standard conditions back to ppb for the various pollutants are given in the following table. POLLUTANT TO CONVERT yg/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 not presented in this report. Table Til displays the monthly Statistics for each monitoring station for the month. To insure statistical sig- nifveance, and to reduce the possibility Of introducine a bias in the presentation, averages are computed only when at least 50 percent of the samples are present, except for relative humidity and temperature, in which case 75 percent of the samples are required. If less than the required samples are present for a particular parameter, that entry will be blank. The number of LE C500 3 oarrR etait ‘ a In stini oy 7 ees , —_ ie fe ete? tio rte ad. SIuor 3 sta f isd: aut: ; 2h, i: ian Dav odhox ba S 2s708 fiom : - 7 a0 78 = ehlt nc 8 ta +6 _ . = - B sol Hits not r {* & ae Tak al ot & eae nak Pl Barros: a ore ci ie 74) ERO DAAIM corPoORDYTION 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 pexcent. A blank entry indicates an insutliesent 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 sepments Me C=507 Fagot yi 4 >’ faves ofee berlin! wi Meicuito eke bes ey 6 a 7 FG /T §>aQtae wus BAlgcm-v:. wiz ttt esiemp RUinlncnum In » ie “G £161 9400 et: gel saldennt: lerneaa asia See ats Hol do trqeo: eee seat ~Aiae gee Gif eeidaT 4:3 hui 2nVE6 sil? OPE] i245 259h ( Lae. \ it sy bregeeinn Geos Iqno%e PRM ST deo sty 36.7002 @iijem Caw ettessib bade Bas baegs inst Srigaxove FOI OEY Sr aeiety bod uqmny a2 baaqa Spiw gay wrote aipinioay i frgem sosssy sils 2s Losses bedaqwes sxe segetevn 222!islerd HR SPY Joie 3 st Be a? avelyzib ¥rigtdar 5 aalqnaz 2 Unie tp te t agi ats Oe 7799k9 2 SA gebtsaisg 2 han qT eolgtee savidat- tapes 2 Late Side ania ‘Ai vise a FRISIAN corporation are independent. The maximum averages reported are found using a ‘sliding average’ technique with the exception of the 24-hour particulate average which is computed from midnight to midnight and the 3-hour hydrocarbon average which is computed from 6:00 to 9:00 a.m: conly for averaging) tamess less, than;or: equal te 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 hot a Sliding averaze 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 a full-rigged frigate of the period could carry, but has since been modified and modernized. | In its present form for international meteorological use it equates: (a) Beaufort force (or Beaufort number); (b) wind speed; bE C-508 Ste we*iudsa a y= ; - iam < ee but tORNR ©: on Manisa oY nha shel aaa ‘i gee te yosugnas ca lsc GpAnnens § 4%) {s- -—jgeie & bes JsAiolia me 2h ier? 22 iaihe 39 ei eae ac iees ern ‘boteqers : Sta favecnodaectt il saod-f @e2 ae —aiep wo-asrs ecko at: Saheeeey G1 Est ni é Ube og ‘eele-S0i2 goo beeqaue «| agedevA- geibil: si) sven game , -ulereege ads 2aitls ineveve Sago! Fo nid 6°28 orcas A omitiaeet coalu. gitkgacevy G9. .toaGsero tO 2s iqaseyuvisws jade Gahbtus stenineag!t oft Bq adeossq. 00! 1: l- aso) OF Ganga eucls, sothere ¢2Gls paigerovA§ .aQ@aevR 18 HIuqoD OB GnesoTG od Og Is 7h grtbrin * 30m tO Yeddor)! sere tam OS Siupes sti ute dias 3 2¢ eqdgase io oda odd &i bermtferscisol yYfoloa et baluetine es “iting Gee efisb Io Grohesqahet st bos smis oi gers judd nd Lsagtao grigetsve a4 Si fsnottaged and auwssercoebh at ba TRV cid pmottes stb bri images couric esp ts patth ede geretto nf boystqeeb ndlideanse i igs sft eapegeal nolday oft, .nomsgsiih as Tao ilo Ra, ot gabetioik> Se gh 0 io sean pi = 7 312. vate “quote, eae | PRIATDUAA corPporRATION (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 Lepore ave: io EnOtS, 4-6 knots, 7-10 knots, V-1G knots. l7=2) knots}; -andiwinds* of greater than ZL knots. The following table is a complete description of the Beaufort Wind Scale, taken from Physical Climatology, by Helmut Landsberg, 1969. BEAUFORT WIND SCALE FOR OBSERVATIONS AT LAND STATIONS < Explanatory Force Title Specification for Use 0 Calnts an e.creisicterene Smolcemmises viegeicalliyseerereeeeieineiee eet 1 Wighttcaitpere)crret-telers Direction of wind shown by smoke drift, buginot by windevancse « sceeeei cre cies 2 Light breeze...... Wind felt on face: Icaves rustle; ordinary TWAIN Inienwerel NOW iNelG 66 Go onaoooodoKds 3 Gentle breeze..... Leaves and small twigs in constant mo- tion; wind extends hight flag.......... 4 Moderate brceze...} Raises dust and loose paper; small bran- chesjane movedterr eee eieineeic ce 5 | Fresh breeze. ..... Small trees in leaf begin to sway; wave- Jets formed on inland waters.......... 6 | Strong breeze..... Large branches in motion; whistling heard in telegraph wires; umbrellas used with Cistieuillty’ sh seyerecerarcteyeoistee: «ches el creteyetensiale @ NOMighinvitnds.). ws. Whole trees in motion; inconvenience felt when walking against wind........... Solieineshigalesrccre:-tel- Breaks twigs off trees: generally impedes PROLRESS « oxcic epaislsrerevavs, s.sieicias sls eters wet 9 Strongigalej ee. Slight structural damage occurs (chimney pots and slates removed)............. 10 Whole gale....... Seldom experienced inland; trees uprooted; considerable structural damage occurs.. M1 SHiclitiboasudsoocos Very rarely experienced; accompanied by Wides preacidamage a1) inicio 12 jp uarricatie sy ciisisccucill yersvoqcsreccrsyos ersteiteretayetors ores nai aero vacloerers 3: sh Ssisre sierevearaic sceuceersee llerseveras QAO G00 NU DU COOO OO DON BEOGOO OOS MAE Il, ciateveravorcreveraxercueyscoretellt catatefeters elev sreroreteteteleteterere aicrerers\evelelstekepsieveral ere YS) |) cacwiateidtarararvinreveretaseaseille oxevene wiacumy sapere otteterelalelsielavareuersaravacieisisiaveye NG? il) Slerereoias are tcarevoreyeraretalll rovalanetere: oi s/sisvorayereteieslereicceis:sfeisioiecieierarcrerarctels | {f / SBee re oete On| eR Ateneo foo 00 AoC ore Ice cr Source: Table 36(p. 119) in R. J. List (1951); Smithsonian Meteorological Tables; Smithsonian Miscell. Coll. Vol. 114. i E2509 Corresponding Limits of Wind Speed at 10 meters ab. erd. ——_—_—$—$—————_ —————————————_ ————e—eSEeEeSSSESESFSSSSSSSSSSSSFSSFSFe Mi/hr. oe OD OO 6*°6pre2 C°2pe . 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PERDOOCL2A/ 177246590) 42733474) - 21 TRAILER NO, HAUR 24 MEAN 23 £6 «7 aS 219 g20: 221 15 14 ica NAY 18 15 18 19 SK~VNO TWMOORDOAQGA A wt ot mM = vw - nwo - = 4 @ ~ } = 18° 6 36 16S 20 24 nH -_~ S Ou ot Om ON cay) ine) Ce wv Ne) fan ™ aw (eo) ra - Lap) ° MEAN RVATIONS E NUMBER OF OBS laureate NTU OE LEC TABLE ITM y | OF THE INSTRUMENT 9] 24 ERT Lah be SAMP DERE S. VAN eV Alleah) t Wy Geome 7 e *, as . 21 22 23 24 MEAN 20 {5 1s e SULFUR DIOXIDE (UG/M*¥#3) BeRvOUGray L778 TO 1275177 43 HOUR DIURNAL VARTATION NF TRAILER NQ, rm 1) on Coho Sal Luk ad Nad 7 . PAF a Bad Wok bate CS ba accd se KR RR RHR KR KRRKRE KR SRR RHR KR RHR RHR ESE x x ee R Ke HR KEKE KKK Ke FRR KEKE KR HK KK x * eK eR RRR KR RK KK a a =" * KR KEK KER KH KR ER EK eee eR E * x REx k x a a ee es xe eke * xneK x * KeRR KERR RK KK KKK * a a a KKREK KE X eee RH KR KE KR EK KEK eK KK Ke KK KEE ee eK EK KK wk * KX * Ke KR RHEE x KK KR ee ey ee ee Ke RR KK eR KEK KR KK * KR KKK SE eR KKK XK KR ee RK Ke ke RK OK + KR RR RR KKK KEKE KK KR eR HR KE * xe KK & * eR RR KKK RK KE ee RK KE ke eRKK & * a Kee Ke KK KKK K + KKK KKH HR KE RK EK ERR eR KR KR KKK ST * KK RK wR KR RRR HK KX EEK KM Rw KRRK KER * KR RR KK He Kw X xe KR HK RK KK KH * a a a ange KKM RK KEK + MRR KR KR RK Kw RR KE KE KR LT MRR Kw KR KK OF * (au KR RR RRR RK RR KK HK * +O ee xe KK RK OR * > < HNGTOWON@OAGHVMTOONR TOV AMTNIONDAA DBD ) e MEAN DETECTABLE LIMIT OF THE INSTRUMENT = 7796 BELOW THE MINIMUM OBSERVATIONS OF SAMPLE VALID TOTAL NUMBER A 3 * DENOTE EAN —— ee TO — we ee eS Ge ee ar © © ” 2 » nad - a S *« *s& ¢ « * «= eee eer 8262 8988 46 & © *«4 a » > = * © see ese 2#© @ 7 8 @ ** «28 ee @m@e@ese ee oo & “3 s =& +s¢é ee @-e 7 e¢@es 8 6 '>e © ee 2 O's. @ © & eo + @ @ " 2 ‘ oe «« @- @aea@eac#se#wee@G@eae 2 ee @ @ ee ae @ eevee ~ a * = «e* =f eesee ee # @ @ es e+ @eie ew edeen a #G 2 g wa @ SS ©8©@. © 8B e+e teenena eee ewene @ eevee eae ® $ 3 s: > “<< S@eeeeweeeeee@ee *se@eeentereewerstses & w@ & e * 7 id > * *e @e ee weseeenweeevew® - 4 ee +s © #8 48 w 6 €.8 - —_ s ~* eo e@ *e® © @# @ © @-@ © 2 @ a Le! Sette nee te wees a . Fests eneenees a _ pee : _ 7 a : 7 ms a ia Sees wae an we by : - Suber ee phew Be) Geer TeX fe. bh teoataeces br hy ee «08 0+ Cowen ne : sede ++ anal e ed 3 a eo on ee . i 4 * Ww LNOWNSLSNI SHL 30 LIWID 379V193150 WHhINIW SHd MOVSH -SIdwV¥S GLIVA ¥ SAlLONS0-* a °9 es NVGW €GEG = SNOILVANSSHU 40 Y34nNN WVLOL "Bl *6 7 *g 9 Sc we '¢ “CG Tt i a “1G ae *y *p CMa *p *y Lie is eal *é6 *@Q NW 2H Spe NO -8e “fe 6) Shae % * % ap @¢ Ge G2 TE @e Ge Ze ve Ge US Se Go Se UNE T¢ S71) GO 82 pe Wo Vis * % * BE "21 a a et. CF Cl “er s » Gy « * * * * r Py % * * * * Py 6zZ SG. & * * et 6% @e 6) 6f Si ny BZ LG vo Ct “2h Set eto * * * PY * r rn Ps * *¢¢ bet 60 Ge 2c @o Be. Gk cen de Ge Tee GE ecm Moa Ge te Gt ed 92 Ye Ge ce be €e 6% Gt « « * % x * * * U6. 2a EY Ste ig “ge OS @y -* * % % * » * % % + * * % 4 *4 5 s r % ry * s % * * * * * * * * Pi * % % * * * *g * a ry ry * * » * Ma s Py ia) 0 * * PY % % a 8 Pa 4 *2 r » * s 4 * * rn s * * * » % * * 4 ® s % * * % * LN r * * * * » * * * * » * * * * * ” * * ” * * % a *8 r Pi rt * s a a » * % * * * * * * a # * % * * Py °@ a * ® * * cy a * * * * * & * * * * be % + * + * *2 Py » s * ry * * % * * * * * * » * PY * * * 6 be, % * * * * s * % % * * % % * % is % * % * % * ry *9 * * a » * * * * a * * * * * * % % % % * * * 4 * *g * Py s e PY * r * * * * % * * * r * % * ¥ % &% & 4 are * Pm * * % * » ¥ * Fry % * “ * * * * % * * 4 * vals) s * % * ry * * a * * * * a * & * * % % * * * * +6 % * a Py a % * * * * a * * a s * 4 * Pa % *g & * * ¥ 4 * » & * * * * * * * * * 4 % + # 9 a a ry r a ry * * * Negu ge “Ce 22 ‘Fe “Se T6T GOY £20 GOT G51 wbl eCl set ytt get |G 8 Z 9 c v e Z t Yyfi0QH (pi/te/et OL past /etyauluad 2 = “ON 4alivad @e (Qe4W/9N) SOIXOIOG ana Tis 4O NOLLVIYVA TvNuntd Pe ero | : r Pr PY A ey ES iN ess SS wad % = —_—— > = Cf eS Ttwyi vr _*” z. ty rm gn es of - x <=. a. « “4 é . + & ® ~ ae cd Pere if ek ec tod awe. lat“ bill * R OIOXTDE (UG/Me*3) UJ al SU PERODIGAys TWH7.42 TO 127.317.7749 DIURNAL VARIATION OF 24 TRAILER NO, HOUR 24 MEAN We ey teh As 63S Gh AP 18a Sy Sy OS 10 DAY zee & BEE zs £ eee eK zs tt x*ertk & kD = * ee etexex« zs «© * Ke RR Oe ae Se a ze xin rae KK ER EK EN eR aK * £0 ron RRR ETE FRO wt Sm) RR RK K x + KKK eK K xe * ae “8 tk e eK Tt = ee Fe KE KR KH = & ~*~ e & eh we we & * +# ANMVMOR DOL wo wn 14 14 14 14 4 15 %4 15 15 15 ie, ts 26 a7 8 2 2 3 32 x 31 MEAN = as MEAN 7167 OF OBSERVATIONS = TOTAL NUMBER SAMPLE BELOW THE MINIMUM DETECTABLE LIMIT OF THE INSTRUMENT A VALTD DENOTES * i C3575 — —_ a a a _ — = i 7 i” ee TO we ; . e- oe 8 ee@-e « o * **e ©@ae ones se 464268 4 = a swe f « ® e era scree «©? S- * 4 4 @ @*s = “se teen e@~- + @ « + *ees ee @ **« eee «+ es * — * ; - ee@eeeeee * eee se Mme e046 *-. *e ee «+ «5% 7 : A ee 7 oe * ese es @ @ 8 ** “e¢ ¢ © 8 re } “e¢0e8 6 . eT ee ee *« *“<«e ec « @& @ e - et) s . oon sos ® *-* ee = ‘ 4 °. | - “se eeee *°s *« ere e080 8¢ e+ «aes : 4 & . * * ewrieee ae -* ee @ **« is") ° - —_ ; - *« . ,.0e0 PW eee er, = 2 « ae fi _ ~ ~ > Pets 6 + “se #7 © + oe z = Pa oe 2 2 wa see ®. 0) 8, 04. **e2¢88 : aa ye setae bene pets ee E eee - ad = @ DIURNAL VARTATION OF HYDRNG (nd Oe dmc buen” fed Laer vedh :/ =" = / k. EN SULFIDE CUG/M*#3) PERTOOCL2/ £774 TO 12731774) 20 TRAILER NQ, HOUR 24 MEAN 20° 24.22 .23 19 ro > < OQ 0. Oe BO. D- @. G4 Be 1. Q. ee -T tt 12 13 14 i) 16 We 18 * B. 31 Be Be TOTAL NUMBER OF OBSERVATIONS DETECTABLE LIMIT OF THE INSTRUMENT SAMPLE BELOW THE MINIMUM A VALID * DENOTES II €-580 Ta ia F 7, ; _ . a ° _ eS. # D : . ‘ — oo om ie. a iM s. ‘one a ee oy 7" 2 a : os coeee ‘ee , id ln ak 2 a ” .__~ ae ; eer \ led Cored a ave —) ACh ones A Oe Bee es bn yf, ace SULFIDE (UG/M¥e3) PERIONCL2/ 1/74 TU 12/31/74) DIURNAL VARIATION OF HY = 21 TRAILER NO, HOUR at 24 MEAN iS “94 39 6 17 38 +49 20 21 @2 2g 12 [on DAY SWUM VMNONR OM 23 24 25 26 27 28 29 32 31 MEAN MEAN OBSERVATIONS TOTAL NUMBER QF BELOW THE MINIMUM DETECTABLE LIMIT OF THE INSTRUMENT SAMPLE DENOTES A WALID * LEG Sil . e ‘ * ° - - es » . a 7 * « ° « ° s e * = - ° ° dl * > ° . . ° - . « .- * J > e * 4 e % « cs e e ® a ee _ e * @ * e a , . a a - ys _ —_ 7 ° ° ' « ’ * * . ff * ° ° ® >.> * 7 7 Ve ° ° 7 * * » ss _ a -* 7 - _ 7 . : / =. i -_—% 7 hee es a. e ° .. * *s - ) a i - 9 * . >| . - ] 4 i : 4 - eo ° ° ~- a7 * ‘ ‘ oe 7 : Tey ' ge? ta. 79 ™" Laden SULFIDE (UG/Me #3) PER EOOCLOA LA7'4 TO: £2/3477-4) > = ie ow ra z Ser Le 3 ke e a oo) mz ox ul = ~_t rH a< Fe (oe a = — ey oO > So aol ‘ é belie tack ieee acl as, Ty, f A vara hus t, Cu HOUR 24 MEAN 19 28 21 22 23 18 > z oO mo « ~VNMTMWOM OD 12 11 12 13 14 15 16 17 18 ng 22 A\ 22 2 * 7 ete RK ES + cece eK KE eH + = eer ee ERS Bad 5 i i a * an ek SC Ke * xe rxraxree * exckeseerste * 5 i i Se a * xx ee &£ ee 3 24 25 26 an 23 29 38 31 MEAN 1. MEAN 7966 QF OBSERVATIONS TOTAL NUMBER LUW TRE MINIMUM DETECTABLE LIMIT OF THE INSTRUMENT BE * DENOTES A VAETO SAMPLE’ : — —*§ . oy « : am eo 4 . ‘ 7 Pye 7 » _ a > 7 — 7 _ ve - 2 ei ‘ ° 7: ' ® st at: ot. of, + ot el es ; — i eee i ° ei y= an a ray 42 } ‘pe a i °# 1 J i ra i. ip he Ky q a’ 345 @ i _ _ re _ a, —.* - ANAWNSLSNI GHL 43O LIWIT 31SVL93L39G WOWINTW 3HL MONTAG AldwWVS GIIVA ¥ S3LUNGG « : o ae = WNV4W 9ESG = SNULLVAYN3S@O 40 Y3NWnN AWLOL = Sc &6 ®*p 8p ®p *» *p vg 1G “9 *p =a 7 “9 ae) "G *c "Gc Ns “6 “¢ Le) “9 “¢ NV dW nek: 2) Gl “Ol cf. 2 & ww Oo ae Oo - — a * e = = & es ¢ * = £ * * e¢ & e = = 2 * “* I + = * = + * a & * = * x * * «x & * & & * x * * * * * * e * = + * AYN AV =a WAN OS 23 24 29 26 27 LQ eo i8y 29 58 31. MEAN 3 a, MEAN 6898 OBSERVATIONS TOTAL NUMBER OF « DENOTES A VaEITD SANPER BELOW THE MINIMUM DETECTABLE LIMIT OF THE INSTRUMENT Il ¢€-5o4 oa vee , , - 7 a ene ee ree@es en ao z — - _ ; a —— 7 i : ‘ i dnd ‘ee « a) > 05 “At = NVIW 998S = SNOILVAYSSHO JG YSuHnNW Wid0l "et “et et “at “ate tat “Ot Yer Ser Sige = Seb e SiGe Vigee “Gee Ere aie Ole Wile “one (Ole tle Ole Wile une ini T¢ we 62 82 92 Cé eve Te Get Saer wie ve Re '6 6 6 6 6 6 6 6 6 6 6 6 6 6 G 6 Ze *6 6 6 6 6: 6 6 6 6 6 6 6 6 6 6 6 6 6 6 6 6 6 6 6 te *6 6 6 6 6 6 6 6 6 6 6 6 <6 6 6 6 Ot wut 6 Ot et 6 6 6 Be mor Ot “ot ob wt Ob OT “IS Gt OF OF Gt ‘Ot OT “Gt Et =“ “Git so tT i Sie Se te 63 a th Sh eh oes |CCCt. ST UTE COT g - @ "8 46 TT OS et Qt "6 6 6 6 6 6 g g g g g g v g 6 6 6 6 6 ob OF Ob at 6 Z1 eek 6 6 Ol sat 6 6 6 6 6 6 6 6 6 Ot 2% wet the cet. th She WS eee: Qt SGie JO Ot Ob 6 6 6 wt 6 6 Ot Gt Gt Gb Ot Ol Gl @t wat 6 6 6 é 6 6 Gi “6 6 6 6 6 ) 6 6 6 6 6 6 ) 6 6 re Sh OF Wh We 6 6 8 6 6 yt ~6 6 6 6 6 6 6 6 6 6 6 6 6 6 6 6 6 6 6 6 6 6 6 6 a a! Cl. Oh. “t- OF bic bl Ot "6 6 6 6 6 6 6 at OT “at ate FT THe FO Siete Fee Sat Zt Fiesta ath. at: RE Ch. TO 6 6 6 6 6 6 Ot Ot OUT 4a STA Ot SIS "Ue [ete rene Scie siel TT oka) be eS ae Ch Sem TAS SU at A. Se At 7 Z 8 8 ) 6 g 6 6 6 e 6 an 6 bt 6 ot bt 6 6 g s) 8 g Z Z g Z 6 6 6 mie Sete Sy 6 SC Oeeeiioeelte Ch et. Gt. tt. os ‘Ot Ot “OY Tt sty OT Bt "ee St se Mee Die Me Se Sty g ont Gch eh. 6 6 6 6 6 6 6 6 6 6 6 6 OT Ot “OT GT “ot % 6 @t° 6 v4 Z Wiesel of Cf “et ‘St ‘OT Th 6 6 6 6 6 Cy OT Uh "OF "2 “Bh She HOIe “eRe Stee ae 9 ou Gk Gh OF CL Ot tt 6 6 "66 6 6 yt 6 6 ot “Ol Gt Gt "Oh %G 6 6 6 ¢ *6 6 at 6 6 6 6 6 8 g 8 g 8 6 6 ) g 8 g g g 8 6 g Y =6 g 8 g ) 6 g 6 9g 8 8 g 8 B g g 8 8 8 g 3) g 6 5 6 € *g 8 @ 8 6 6 6 6 6 9 Z 9 Z 9 9 9 9 9 9 Gg Z *¢ 9 9 9 Z 9 9 9 9 ¢ 9 9 9 fe) 9 9 9 9 9 9 9 9 9 9 g t AVQ NyaWebo Co eo te Ue 6t “8t “Zt “St “Si “oT “81 “et Tl "Bt 6 eg Z g S v ¢ 2 1 &noud (pz/te/]et OL vZ/t /2t)OUTNad @2 = “ON UatIVEL e (c=eeat xX pide tie ieick lle is WilOlL 40 NOILVIaVA IWNSNTO Levene em aac hae a ate PT IN AG Ene? he > cue S bist ew toed ens aw _ams s ones *SE5"5> a an. OE ot cca = - — = "shzg NV3W 994¥ = SNOTLVAYSSAO JO S3GNNN WLOL “pes ete°*sSts* aac’ cue’ Z6t"pct aot *cuc*est*ste*ece* yee co ve Le vZe ¥S9 cGe cet ter2 Bed Cue ES2 eo? Selsey raed SA eee) 69t Z6t 9ct 6et ve 2 ve Le 96 pZe ¥G9 Gee LZ Cue pSe Ted eve po? 682 aS2 6¢ 5 Zut vpt 6gt Tet eet ce Be ve BE 92 ple TS9 Tre 66 cS2 tc2 622 ¥92 L¥2 p82 992 ect pee vot Tot gcd 822 oe be "4 God Lo 92¢ 1S9 ate 62 b6™S 292 E92 TAG Zst Lye Ove evt Sve vet Tue “9T Cie te a2 G2 62 Ge eZe 1S9 coe vG 9G2 Cu? ple toe vel Vv? Ved? dyt C6? cut Loe ust oted Ye 22 “Ke 6¢ Le Zee 1S9 bce £6 Vue Got Loe ee 69t 602 eve pet 6re ott eGt £Zt Tet 6t Te te 8c 8c fue 9et Gud 86t bS2e tee pst ¥32 ay pot cyt 36s Bt CpLZ/te/set OL p4/t /2et)auldad Lt Zt Re ve Toe 91 et Ze ce Gov Tat ZLt 9¢2 Got Aupy vu? B12 Sere Sct vot 66¢ 91 (2aeat X Cean/ oe ue 9¢ 8d Tét LL} AS + vate ¥Ge2 Eve 8ZT ert art Gt "COM Nee oye LSU LSU Cee Loe i este abed - ek cf <2 ce cf ef ae ce ce < Cc a & ~ 2 ~ ee 272 av » 4 7 a4 i _ a ft — al -. - _ 7 4 > a 258 36.9 up z ® 6€ & fe & & a ul co On OOD je <= [an Or 10 ota oO; 12 12 12 S 14 11 12 KNOT ONONOAD _ PO, Oe eT ee 10 10 11 ~~ —_ 12 12 vi | 12 i 9 12 8 9 NmMT WN ot wt wt ree 10 18 ote it 6k ie 6 6Th Ui 1” rp! 14 tt Los) 7 12 1” © se) 28 few 22 23 24 25 - 18 25 18 Zo 26 Af 28 29 3Y 31 9, 90 9» MEAN MEAN 5867 TOTAL NUMBER OF OBSERVATIONS LEN E2587 = « oe ; - Cal > oo ® e >= @ 7) >o d eo &) saw @ @ ts rie ry 5) a ai we Ce aBaLeASecrxnev 2 of o & t were a 6 PSee eee eurcweca es Pam S oo re Pal GHeoetqoaeoacomact & aa o ac @ = eFncanaec oon Aned oe a - ~~ e wa2A@ a2nPRGee2eCo2 wereaoc 2 & e- ~ ore geragvea Pn eonac o Vo . COte2Ot« Sate tOtelate rot = 6is-< Ot © ™ —_ Om e o ADDDADDOMDWADD CO O NV3W bo fe at Bt 6% 63 et Onn Amnwowmowooovooonondn Dd at ot 61 61 Bt om oO ADTODADDAGEWDWAAD A DO is] N at Qt 64 64 gt AwmDvenomoomnwsowdona ~~ N nt vit 64 64 et HOmpmema nmnonvnonoacvon a S ON at at 64 &t 64 ADODDDODANDNOBADWADAA DO Le.) —_ ( in iC Sat = WNV3W 62Z6v = SNOITLVAN3S#0 40 YS8wNAN TWibs oye 8 tte totwteh Ute lOtakG O66 wmeCleeC lesa cutee lalG #06: an 6o ee Olen) NV SW 6 Ot Ov ef OF OL Ot oO Gh wh at sur oper eel wn oom oat Te 6 Ot OF OF Bl Al Gt Gt Bh Ot Ut 1) ot wh @) =e) at sat ae 61 6h 42 Be 82 eg 6t -6t 8% “61 6h “Gh et “St “61. Wet 40 66 of =O geo ae. pe) yes cee S 8 6 +6 aot «8 of GO: G6 CO LO 5 goon) crete S g @. in®- G oO ap@ eG: oO BG 2S" a0 Geers ci nce mcamEc y @ @ i Oo [Ge 58 O20) ae Cdn ae) 0 epee ¢ Gr 2G 9, a 26 6.7 36 «ee z 6 6 6 @t | 1 AY Ot 23 oS oSt oil oft oct vit . Bt 26 ) Z 9 G 4 ¢ A if yYNOH Cpz/te/et OL p2/t /etjadiusd ¢2 = *ON sdTIvys (2 a —-NMO TWN OR DADA et 12 if Ws 13 14 i) 16 17 18 a S he ro S wu Q 2 fa) te 9g Y 4) 9] 7) N © ® Nn 2) 2a 21 & g ” v 22 z3 24 20 26 27 28 29 32 31 Q. 0, = tT. MEAN 58465 OF QBSERVATIONS = TOTAL NUNBER ne easing "ETS°EOS* SOS LET * VET LAT HOT AST CET ad duc cle*Gee Tis aus Lue aus*gus*ats*euc* pas ou ate*uue Gce Tyo ece £6 AT 6t2 562 ve? 6c2% Tue f£6t Zgt Te72 Bot Zt Lit gat 4 Zt 6 | ts) rs et Z Z cce 9¢et Tyo Teg QTE eee 69 6 £62 92 Gre ere ole U2e Qv2 ece2 Zee Lb?) 842 ple Toe £62 Oct tet 96¢ Gee Tet 9et est ect eect vce Lt The fo 22 ad nO Oo DH Ze Zr9 rae BZ 922 ec2 GG2 912 Lvl O¢2 BL? cet £62 cect Zot Tot cue te “| BY at 9 6S¢e ov9g C66 GP? Qr2 f6t C92 ZG cit UES ete Bet pea ect 612 T2t AN? a? at at 6 Z ¢ge cpg ove G8 c62 6e8t 622 a4 6Gt Bed bee cht we? gut bet 691 colt 61 (cmeeat X C##W/ON)ISNOGHVIOUGAR SNVHLAWN=NON 40 NOTLVIYvA TvNanta *2u2 = NVW4W 292Zy © SNOILVAN3SSSU 4O NY3dWAN AVAGL tt 2 S 6? te ke te te be te be ie Ve se te ke 0 4 ¢ Gl te te We te -le We We Set te le ie oe 6 8 1S ee: ee eft 6 6 Z 8 | iL 8 et 6 S G 8 6 vce OLE TEE Bdp £46 M60 c6e@ Gc tee Guc eee 442 Bue ete Coe 9ct oe | T62 6IE Bue HI wee SUE Bre Bcl 2242 V6t SGT @Zt e8l tcc Ge tee Sec OIe Gad ic gle Gile gee wid Mec £Z£1 vot B89T BOT SGe2 H9F TSE SSE 642 BUE AB BYE GEE Bwyd GOS Coe 9242 ele 962 eoGSb 6240 GH CBS GLC 6G2 BE Sle bbe Gle L422 Tle eet OTe ETE GTE ZTE OFF vie Tle Tie Sue Ete Tue vo! eve 162 cSb Gov Muy bev BCE Cee LES vod ECL HOE GIE He L422 Sve £0 Bee ece Wie ZTE Que YY WIS LEP HLS 692 GEt Bce BET fue GGSe GSe2 Tye Tet ext @24 BSE 6ST GUT “GT WOT TET STY Sot 66t Spt Ge Lue Gul @9e cud Tle 9G2 G22 SYS 9G2 Bee Cte ol2 Tod Be 68S LES SLE G92 Mys ve? 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Wey Wb. ae a6 y rh ‘ye © Z P b cj 6t eC ve ga ry ey Or cb Ge Se 61 S&T We St Wi i wha at Foz 2t wt @t 8 ef Wl ve cy -2S 486 ve 8 ve 6te. 6 6 Poe Oc ate IR 36 yt 8@ C2 SS wr ab be Cy ey wy cE We © ot at Gt gt Gh wt en g TS Se | | SA 0 2 A ) 72) 2 i <2 be 6G 6 Se Z bee ge we “i eh Oe ¢e 3% $e erp £¢ ev ev be te Ot & Z vy 6 et Ch. 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O a) *g ) “a7 9 “oT Ft “et G2 *g az2 NVSW 2 ~~ T 8e¢es DONW a v > VERY UNSTABLE | HEIGHT (f1) rn Lo) Le) UONERATLY NEUTRAL MOOERATLY UNSTABLE 9) o Co) 5 ite) 15 20 25 30 STANOARO DEVIATION OF LATERAL WINO CIRECTION Og (deo) ._+ The vertical variation of the lateral wind- direction standard deviation (¢,) for various stability regimes. The curves represent average or typical conditions with the exception of the two outer ‘very Btable’’ lines, which represent extremes. The large surface values of To 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 oecur*with very Light winds;. As a general rule, for a given anseolation condition, imereasing 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. 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