Tract C-b quarterly report, 1975

U.S. DEPARTMENT OF THE INTERIOR
PROTOTYPE OIL SHALE LEASING PROGRAM

TRACT C-b

QUARTERLY REPORT #2

(Through February 28, 1975)

Submitted to:

Mr. Peter A. Rutledge
Area Oil Shale Supervisor
Conservation District
U. S. Geological Survey
Grand Junction, Colorado

By:

Ashland 0i1, Inc.
Atlantic Richfield Company, Operator
Shell 0i1 Company
The Oil Shale Corporation

APRIL 14, 1975

QUARTERLY REPORT #2

TABLE OF CONTENTS BY VOLUME NUMBER

Volume
Number Table of Contents
I I. PRE-EXPLORATION FA sea RECONNAISSANCE SURVEYS
A. Biological
B. Archaeological
II. ENVIRONMENTAL BASELINE MONITORING PROGRAMS
A. Surface Water
1. Streams
2. Springs and Seeps
B. Core Drilling and Associated Ground Water
1. Well Survey Plats
2. Completion Data
3. Drilling Water Production
4. Water Quality - Drilling
5. Water Quality - Baseline
6. Water Quality - Pump Tests
7. Aquifer Data - Jetting Tests
II 8. Aquifer Data - Drill Stem §& Multipacker Tests
III § IV a. Drei Stem Tests -"SG-17
V b. MPP Series 1 - SG-17
Cc. MBE Series 2 = SG-L7
VI d= MEP Series 3°- SG-17
é:. Driil Stem Tests -°SG=20
é f. Drill Stem Tests - SG-21
9. Aquifer Data - Pumping Tests
VII & VIII 10. Lithologic Logs
11. Geophysical Logs
12. Assays
13. Trace Element Analysis
14. Rock Mechanics
15. Gas Samples
IX C. Air Quality
1. Air Quality and Surface Meteorology
2. Low Altitude Meteorology
3. Upper Air Studies
4. Visibility
5. Atmospheric Diffusion Studies
XXL Gk 6. Radian AQ Data
‘iT? D. aaret

Terrestrial Wildlife Studies

Aquatic Studies

Terrestrial Vegetation Studies
Dendrochronology and Dendroclimatology
Soil Survey and Productivity Assessment

i oe tS

III. OTHER STUDIES
oe A. Fish and Wildlife Management Plan
B. Revegetation Program
C. Microenvironmental Program
D. Aerial Photographic Study
E. Archaeological Studies
I Scenic Values Program

Ree OO IANS

SSE rs Sy SE =X iad fd
> gas Ne ma oS bea LS a hte fed bed wns et

RC#100-056

QUARTERLY REPORT
AIR MONITORING FOR

C-b SHALE OIL PROJECT

- SEPTEMBER 1974 - NOVEMBER 1974

24. January 2975

Presented to:

C-b Shale: Oil Project
Suite 555, Iwo Park Central
1515 Arapahoe Street
Denver, Colorado 80202

Attn: Mr. Max Legatski

Prepared by:
Radian Staff

II C-688

8500 Shoal Creek Bivd. P.O. Box 939458/Austin, Texas 78765 /(512

FRABDIAN corrorarion

E.

LE.

iL Ee.

VI.

TABLE OF CONTENTS

Page

GENERAL DESCRIPTION OF AIR MONITORING PROGRAM...... II C-696
DESCRIPT LON; OF *"ENSTRUMENT SYSTEMS ios Oo otlhe cn nwrewie II C-698
A. Air Quality. Instrumenfation....... cei secicecees II C-698
B Calibration Preoeedrn Gp... ws. \lieiere desuate nk oo Win, bots II C-700
Gi “Data ‘Acquis it Lome S yet oil... dio eens donee raetes » ace, eons II C-702
DD.) Meteorological’ Instrumentation. wi sma’ saps sag oa wie II C-704
MICROMETEOROLOGICAL AND TERRAIN FEATURES........... II C-713
OPERATING ‘TIME VANALYSI Seis iets. + a\s0cx tap tes a So eo II C-719
METEOROLOG@GAL "SUMMARY. stints severe a eth dias ee ates wep ereiee LI: C-725
September Summary. «<2 t.<, ehesanie: ob ae Malo aun gee Sie ara sweeten II C-727
Oetober Summary %....02.g Pe cen sip a ee oe eee ow oes oe IisG-739
November . Summary &. oc, sicathss c,h! ae tees aw Pees eae iB 9 she
DATA PRESENTATION AND: SUMMARY 3... sts.0 ad olen ce bos ae LE Ga777
Quarter lye Swear Wir ok wiinedtor« ace he pies ee Dae + wl Ce II C-786
Particulate’ Concentration), Distributnom..... ...5 Sane II C-791
Daily Averace Concentrations. 7c a7... fete. «so eee II C-792
Concentration Versus Wind Direction

Cofrel at Leng. vidi tye. eS o's a ae ee cs oe Soe II C-804
otabilityawind Bose Das eames)... seuaeeeeee ccd. . ane Ii G-sst
Temporal Varlation.of Reeorded Parameters. ys) 2. II C-891

II. G-6659

ESS OS OES

i a a

3 EC

ey

ems

E2ADIEN conroration

INDEX TO DATA PRESENTATION TABLES

QUARTERLY STATISTICS

Site 020
Site 021
Site 022
Site 023
Site 024

DAILY AVERAGES

Nitrogen

ee ee a me)
ee a
ee er me |
ee ee ee |

oer eee ee eee een ete eer seerenne ees eeseeseer ec seeaseeevn ee see

ee oN chs sg ain ee ES ata a a eee

re ee i ee els ow SE os en Se ee oe

Nitrogen

Bu IRS pe 2 oe ger ge eo Oe Cie OE Ue eh |r ea .

Bitar Daye eas Ge se Ee, ee tis ww Shay: aiarie

eoecee eee eee eee eeeneeeseeeeeeeens see e ec ene ee ee

Nom-Metharie Hydrocarbons .< sil. a.65) cha ets oie so wpaeoat

Pa Ca Ae cs bie ab cia Slalle Oiwi Seen ee Fe on oie eee

ee ee

QUARTERLY CONCENTRATION DISTRIBUTIONS

Nitrogen
Site 020
Site 023

Oxides

|

xide

Nitric 0:

Site 020
Site 023

oS 8. 6 6°22 \8'S, 6 60-609 BO. 9 6 8 CTO OC A CS OC 4 BOTS Bae a a eer eT, YR

II C-690

II
II

id
II

II

iI

II
it
Et
a
‘ge
II
1 |
i
II
II
{I

II
II

IJ
ia

C752
C-793
C-794
C-795
C-796
C=797
C-798
G-7o9
C-800
C-801
C-802

C-803
C-804

C-805
C-806

S2 (MOU cornporarion

QUARTERLY CONCENTRATION DISTRIBUTIONS (Cont.)

Nitrogen Dioxide

Site: O20... oh sce ce olan at ee ee etc ames Sie
Ss te02 3. ook ee Dee be A Sa Sei are ee ee

Sulfur Dioxide

SEES 020... ods Ao ns ae ce Sa es
Site 021. (7.2.02 dr SRN eek) ot ck, COU Oe) ee
Site O22 66. 258 acct ee eee eee awe Calera Pera a es
Site: 023... i ee ee eee oe oe er
Site v024. ues AOL ME POR ae. Tok ot

Hydrogen Sulfide

Sie O20 |. tit ow een nape oe age cet « ueipe tle Stee mm RPS
Ste OZ os dks ace oe a mw here senees @ e's ea Gotekalaie ees reyes
Si £6 022 oso ow Bieta wad ale eee osu, alo ele aio ae es More
Site 023%. So hae cere a es Sie see nciene = emai
Site: O24. 5 13 ns Secale cei es ie ee re as rhe

Total Hydrocarbons

Site O20... ih gao ss demo ae ease eeu oles Shee ai
Site D Sieg a aes Oe ohn Aa tied es Hee eet ao) exer

Methane

Si fe O20... er ea ate 6: Sak eee seal elena ns) wun eaten
ST te O23 o w.6 See Keokerd a ohare AI CL Re cereus ee aoa ete ater enere

Non-Methane Hydrocarbons

Sime: O20. ko settee les Coneee teks ae eke rte aaa castes 6 re aertata
Si fey. O23 ooo kcal noe Sa Ce Reda 1 ara rate camer

Carbon Monoxide

Sipe ODO oo ee ns Se ee a pe ee ee. aes
Sete O8F0 ta os ele eee es ey, le eee

Ozone

Site, OZ OS eck... ox ce eee eae alo ree. a atant ae oe
Site O23. « 35. cee ae in ee a ces bers arenes

II C-691

Page

Il
II

II
i
II
II
II

II
II
Il

II
II

II
II

II
II

II
iG:

II
II

II
II

C-807
C-808

C-809
C-810
C-8it
C-812
C-8135

C-814
C-815
C-816
C-817
C-818

C-871S
C-820

C-821
C-822

C-823
C-824

C2325
C-826

C-&27
C-&28

Be OIS22) eorrorarion

WIND DISTRIBUTION BY STABILITY CLASS

September
October..

oeee eee ee eeseeeseeseee ere er eee eereewaeeeeee ee
eeeerereereereeeteeseeeseee eevee eeee tt tetse®eeeeeeeee
ore er ee eeeseeereeeeeereeeeeeeereeeseseseeeeeeeee

eoeeervreeeeereeeeeee ee eee ee eevee wee eeeeee ee

II C-692

Page

II C-834
II C-848
II C-862
II C-876

RADIAN corporariom

DIURNAL VARIATION OF RECORDED PARAMETERS

September

Nitrogen .Osides soe a sien oe Rintde, bastonoie
Nitric Oxide... :. pete. mess PO ee ar eee
Nitrogen: Deoxr1de Fe .2 «= soins os dale eeatarele
Sulfur Diozsde: .. ae. oe Dieta eM Yeo
Hydrogén Sultide.3 2s 2 Ue a oats oe sites
total. Hydroearbons 2.3 => + suai = + aeale ss
Methane v7 2 Pacis «Seis Saye Se ae, Se or a
Non-Methane Hydrocarbons.” .0..cu sens «
Carbon Monomide: .'. cise uote ashe aetna als, ose

Wind. Speed. 2.2. . é..5taee ese ates Sag Ree cies
Wind Direchvons . s<ceep tise ase ee ee a
Temperature s.4.. ot ccnce as eee aE eee
Relative Humidity 1... sss oe ees Bae Serene
PYeCipi labs Gn... docsa,s ees + ee ee
Solar Radiation s csetsys wae ee ae We Ce

PT.C-6395

Page
II c-891
II C-893
II C-895
II C-897
II €-902

II C-907

II C-909

Li-G-9it

TI C-915
BIG-945
IL G-8i7
TF G-925
it C355
II C-941
II C-949
II C-954

F2AAISILASY corpPorarvion

DIURNAL VARIATION OF RECORDED PARAMETERS

October

Meer OPeEr OxXTGesd os. ie:s oe aie ake ag tae oes eiia'e gedone ot ieeae
Ma ewe OK. GEG Mes. ie Susyatey aie ke arale aoapetals, araca ese ks
PEEL OREN (DELON SP) sy. Secu cs ape aw helt gone ke Soe auare
LIOR LGC. ain od. is x a aie is aqath rere ak aisles: a eats aoaee
Hy@rogen (oltre. fy. siete sails So stage a [ere eke 0 cate eelgrass! i
Peed, -HyYGEOCALD ORGS ..ctale s-s:0, cba) atauat eWay oc ai sae eae She ees
fy (ong 2 002 hg | RE Seme -o oe Cea NS mR Sm
Non-Methane Hydrocarbons « .. . 22 cccal seis ale Swine
Capon Monoxide. a2: boon eee ees ee

WING SPCC oi.G se eee shee ode She BROWS le acarie Rhein eet ates
WNaitie, DPE ESET ON eis: oo ah arele: «le Sp takeeinetidie ‘sas abel s caite
GID OE Cite ote elon. a <5, oa. sn Rd BA ches Sc eon a = ne. ie
ei we Tid Cd P< Gace nies» arabe te emis oma sys Suen ear ore
Lge alsy Dope stst ines oy ak Wf: Baek, Ser A A mene cmrameet Shr
Beh Rea Rae 1 OUR Mea ghee cw. 4) 4. +. 5, & eto eave olin Sh aw Uhaeure saat vs

IT C-694

E2EATSIZAPA corrorarion

DIURNAL VARIATION OF RECORDED PARAMETERS

November

Nitrogen: Giieiaa ee 2 oe eilalein<'s «5 5 aera a woe » ete eos
Wi tree Oneal es irene ais tare stat wysderainse aie winter es
Nitrogen a caeed es oi.) pasos etiale: sia eters (s.0 5 eee) 0:2 aileLdee
Siilivr: Da oscitaeer, 20. eee, seeks ices, 7 Sees Sickie MRP Reg (oar

Wind,..Speeds.o fot dis,« sx tacaneiemneeiers tes fo eeeraie Seer ae eae
Witid. DITESCLOM. « onc ules. San oS tae dikes ela D aibece
EEMPSTACULE Mase... . « «5S aeceeters SAO « Sen arete ee ole eee
Relative: Humads ty <. 4:2... sete eke ars ot eae es han
PREELDI ES ELONAG -. «. < ia, 5. <rcneteeieil ass a> win ae ar olene aah ee ate
SOPar -RAGEAELOM. «, ...\cls ce ene a wigs stata S46 che ache tel alaes's

BL C-695

| eure | ee: |

“2

ERAADIFAN corPorarion

2 i GENERAL DESCRIPTION OF AIR MONITORING PROGRAM

Radian Corporation is under contract to C-b Shale Oil
Project to provide ambient air quality monitoring.* Each site
measures and records the concentration of particulates, sulfur
dioxide, and hydrogen sulfide. In addition, two of the sites
record the amounts of nitrogen oxides, total hydrocarbon, methane,
ozone, and carbon monoxide. Selected meteorological parameters
such as wind speed, wind direction, temperature, and rainfall
are monitored at each station. A 200-foot meteorological
tower at one of the sites provides meteorological information
as a function of. height. Meteorological instrumentation is
planned at the 8, 30, 100 and 200-foot levels.

Figure I shows a typical configuration of each monitoring
station. The station enclosure provides a sturdy and protective
covering for the monitoring equipment.

*Five monitoring sites are located in Northwest Colorado in
the Piceance Creek Basin on or near the Federal Oil Shale
Tract-C-D:

II C-696

wOSSaudkod
o/V.

GovdS WHOM
ie

|_/ Vauv INSNNULSNI

yananoo |<

ar |

’ 1 Sa CRS) IP SS » EE; GT 5

YOVYL AIXVI

HONG

Poa aterm |

SOVYOLS AYTZLLIVE

ee
nara

|
|
| KOOU FLL
|

a |

SAOUV O

aan
gala YIV OVSZ e

— ee eee eee

ST ShGRe.

alll

| BIV OYSZ

co

ee |

ee

IT C=697

ERA ISIAAN corrorarion

ti. DESCRIPTION OF INSTRUMENT SYSTEMS.

A. Air Quality Instrumentation

Nitrogen oxides are measured with a Meloy Model NA520
analyzer. This dual-channel analyzer is based on the chemilumi-
nescent principle, and continuously monitors both NO, and NO.

A subtraction circuit in the instrument provides a continuous
NO2 output, but is not used in Radian's system. NO»2 is cal-
culated once a second by the computer by subtracting the NO
value from the NO, value, thus avoiding any drift which might
occur in the NO. output of the instrument. This instrument has
a minimum detectable sensitivity of 5 ppb (parts per billion),
and 2a linearity of I7.

Both sulfur dioxide and hydrogen sulfide are measured
with Meloy Model SA185 sulfur analyzers. The hydrogen sulfide
analyzer uses a Meloy Model SO,-1 sulfur dioxide scrubber and the
sulfur dioxide analyzer uses a Meloy Model H,S-1 hydrogen sulfide
scrubber. The Model SA185 is a continuous analyzer, and utilizes
the flame photometric principle of operation. The minimum detect-

able sensitivity is 5 ppb, and the linearity is, +17:

Ozone is measured with a Meloy Model 0OA350 analyzer.
This instrument provides continuous measurement of ozone, and is
based on the chemiluminescent principle. The minimum detectable

sensitivity is. 0.5. ppb and the. linearity, ys 17.

Total hydrocarbons, methane, and carbon monoxide are
monitored with a Bendix Model 8200 gas chromatograph analyzer.
This instrument uses a flame ionization detector and has a minimum
detectable sensitivity of 5 ppb for all three components. The
Model 8200 works on a five-minute cycle, i.e., one air sample is
analyzed every five minutes, and the result is displayed for

five minutes via a sample and hold circuit.

IT C-698

F2ZAADISAM corporarion

The air sample is drawn in through a glass cane and
manifold supplied by the Ace Glass Company. The system has a
25mm diameter, and a constant air flow through the system is
provided by an air pump rated at 60 cfm at 0" head pressure.
The manifold has sampling ports to which %"' teflon lines to the
instruments are connected. All joints in the sampling system
are secured by O-ring (Viton-A) compression fittings. The
manifold is contianed in a heated (100°F) chamber to prevent
condensation of moisture. The teflon lines from the manifold
to the instruments are insulated with 1/8" wall thickness rubber
tubing.

The trailer has four heavy duty high volume particulate
samplers (Hi-Vols). Fiberglass filter paper is used for collec-
tion of particulate samples, and each filter is brought to a
controlled humidity before weighing. Each Hi-Vol has a flow
recorder to permit correction for changes in air flow as the
filter becomes loaded with particulates. Each Hi-Vol runs for
a 24-hour period (midnight to midnight), and is turned on and off
by the computer. The Hi-Vols were designed following guidelines
recommended by the Environmental Protection Agency and were
manufactured by Radian.

In addition to the normal Hi-Vol particulate samples, a
duplicate Hi-Vol sample is collected every sixth day on special
filter paper for trace element analysis. Once each quarter these
samples are composited and analyzed for gross radioactivity and

trace element content.

Tf (G-699

ERED IAIN corporatior

B. Calibration Procedures

Each trailer contains a Meloy Model RAD-1 calibration
unit. This instrument provides a zero air supply, SO2 span gas
from an SO2 permeation tube, and NO span gas obtained by pre-
cisely diluting bottled NO span gas. The calibration of all in-
struments is automatically performed once a day, and is controlled
by the computer. Each instrument is first switched to zero, and
the computer monitors the output of each channel and takes a new
zero reading after a stable zero signal has been reached. This
zero reading is compared by the computer to the zero reading
obtained 24 hours before, and if a drift in excess of l10ppb has
occurred, an excess zero drift light for the channel in question
is turned on on the System Status Panel. Next, the span gas is
supplied to each channel and the computer decides when a stable
span value has been reached. This value is recorded and compared
to the previous day's value. An excess span drift light on the
System Status Panel is turned on if a drift exceeding l10ppb occurs.
The instruments are then returned to the monitor mode, and after
two minutes the computer resumes data taking. If an excess drift
light is turned on, the operator will note this after entering
the trailer, and obtain the calibration data from the computer
via the printer. The operator decides whether the drift is
severe enough to warrant discarding the previous data, and he
then performs a manual calibration to determine if the

instrument requires servicing. If so, the instrument is repaired.

The SO. permeation tubes were manufactured by Metronics
Association, Inc. Their output has been verified by comparison
to the output of National Bureau of Standards tube 10-42. Both
SA185 analyzers in each trailer are calibrated with SO. from the
permeation tube. This instrument responds to the number of sulfur
atoms per molecule, thus SO2 can be used to calibrate both the

H2S and SO2 monitors. The zero air is obtained by passing ambient

IT C-700

RASIANM corporar4rion

air through an activated charcoal column. These columns are
replaced every three months.

The Model 0A350 ozone analyzer has its own calibration
system which provides a zero check and a span check. The zero
air is obtained by passing ambient air through an activated
charcoal column (replaced every three months). The span gas
is obtained by passing zero air through a calibrated UV source.
The ozone calibration system is verified by comparison to a
calibrated ozone generator maintained in Radian's laboratory
in Rifle.

The Model 8200 total hydrocarbon, methane, and carbon
monoxide analyzer is calibrated with undiluted span gas obtained
from AirCo's Rare and Specialty Gas Division. This span gas
contains methane and carbon monoxide in air, the methane being
used to calibrate both the total hydrocarbon channel and the
methane channel. This span gas-is checked against a bottle of
span gas which was calibrated at the National Bureau of
Standards. The Model 8200 is zeroed with air from a Bencix
Model 8834 zero air unit (a molecular sieve dryer plus catalytic
oxidizer). In addition, the instrument is electronically re-
zeroed at the start of every five-minute cycle.

Bottled NO span gas is used for calibration of the
nitrogen oxide analyzers. Bottles from three different manu-
facturers are used, and these agree with each other within 3%
(Precision Gas Company, Linde Specialty Gas, AirCo Specialty
Gas). The zero air is obtained by passing ambient air through
an ozone generator (to convert NO to NO.) and then passing it
through two charcoal filters (replaced every three months).
Bottled NO span gas has recently become available from the

National Bureau of Standards and a bottle has been ordered.

Hrec-70r

E2AAIDSAALDS eorPoRATION

The Hi-Vol particulate samplers were calibrated using
a Calibration Kit from General Metal Works.

IL Ce7Qz

RADIAN corperarion

C. Data Acquisition System

The basis of the data acquisition system is a Data
General NOVA 1200 minicomputer. The NOVA which has a basic cycle
time of 1.2 psec is equipped with automatic program load and power
fail/automatic restart features. The computer utilizes 16K 16-bit
words of core memory. Analog-to-digital conversion is accomplished
via an ADC built by Radian Corporation. The input/output unit for
the system is Texas Instrument's KSR 733 keyboard/printer. This
model teletype provides keyboard entry and hard copy printed out-
put. The data are also recorded on a cassette magnetic tape unit
with three drives. The cassette unit is utilized for program
storage and loading as well as recording. The power to the tele-
type and cassette units is turned on only when the unit(s) is to
- be used to reduce wear on mechanical parts. Several important
functions in the instruments as well as in the computer and the
trailer are monitored by means of lights on a System Status Panel.
These data lights are written onto cassette tape to monitor the
complete status of the system every five minutes. The Data
Acquisition System also monitors the presence of 110V power from
the power lines. In its absence, the computer, which is powered
by batteries, switches all trailer systems to battery-provided
power. If the line voltage is restored before the batteries are
discharged to a specified level, the trailer system is switched
back to line power.

IT C-703

FRAEIAR corrorRaArTIon

D. Meteorological Instrumentation

1. Ambient Air Monitoring Trailers -

Four of the ambient air monitoring trailers are equipped
with the following meteorological instrumentation: (1) dry bulb
temperature (outside), (2) relative humidity, (3) wind direction,
(4) wind speed, and (5) a tipping bucket, heated rain/snow gage.
The temperature probe and relative humidity sensor are mounted in-
side a motor aspirated radiation shield, the Model 186 Aspirated
Radiation Shield by Weather Measure, which gives an aspiration of
approximately 100 cfm. The wind instrumentation and temperature
and relative humidity apparatus (in the aspirated radiation shield)
are all mounted atop a 30-foot crank-up meteorological tower (the
WM-33, by Weather Measure) at each of the four trailer sites.

The wind instrumentation at the monitoring trailers
consists of the Model W103/3L Lightweight Cup Anemometer by
Weather Measure and the Model W104-2 Lightweight Vane by Weather
Measure. The anemometer is a high response, low threshold wind
system which offers the optimum in versatility and economy. For
low threshold applications, a unique frictionless tachometer
employing a high frequency oscillator and receiver is used to
measure precisely wind speed. The oscillator, transmitter, and
receiver are encapsulated in a small cube of epoxy for total
protection against the environment. The high frequency tachometer
embodies several distinct advantages over the commonly used light
chopper systems. There are no light bulbs or photocells to burn
out; power consumption is low; and the system is insensitive to
moisture condensation or dust deposition. The solid state tachomete!
is essentially free from maintenance with a life of well over five
years when operated continuously. The specifications of the W103

Cup Anemometer are as follows:

Il C-704

BE2LAIPIZAAM corPoRaArTion

Accuracy: + 1% or .15 mph, whichever
is greater.

Bearings: Sealed and shielded precision
stainless steel.

Threshold: 0.6 miles per hour

Distance Constant: 5 feet

The wind vane, the W104-2, is equipped with a 1000 ohn

low torque potentiometer and two wipers for o” to 540° operations.

The response characteristics of this vane are:

Dead Band: 0 degrees

Damping Ratio: 0.4

Distance Constant: 325 feet
DAresnold=e0. 75 ees per hour

Potentiometer Linearity: 0.5%

The thermistor probe used in the motor aspirated radia-
tion shields is the Model T621-TP18X Air Temperature Premium
Thermistor Probe by Weather Measure. This probe has a range of
-50°C to +50°C and an interchangeability of + 0.055°C. The out-
put signal accuracy is + 0.3°F.

The relative humidity sensor is the Model 2013 Remote

Reading Relative Humidity System by Texas Electronics. The sensor

assembly contains a newly-developed hygroscopic inorganic sensing

i Ur

RASTAN corpornr:on

element. Its expansion and contraction positions the suspended
core of a linear variable differential transformer (LVDT). The
absence of friction inducing linkages and wiping contacts minimizes
hysteresis and improves accuracy. The. LVDT output signal, when
processed, is directly prcportional to relative humidity. The.
specifications of this instrument are as follows:

« (“Rangevot Indication: “GZ (to 1007 RH

* Response: The sensor response time to
a step change of 10% in relative humidity
is less than 2 minutes with the sensor
exposed to moving air.

Pe ) Aecunacwe Sg bon RH; 2, 92-8
ie Plots 95% Riot 277 Re
95% -100% RH; + 3% RH

*— Solera... Output: Analog signal of -150 mv.
£0: 4150 mv. with electrical zero at 50%
RH Tse standare.

Each of the four monitoring trailers is equipped with
a Model P511-E Remote Recording Heated Snow Gage by Weather
Measure. In the case of this gage, the durability and reliability
of a tipping bucket gage are combined with heavy-duty electric
heaters to make this an all-purpose precipitation sensor. This
gage may be used to measure snowfall and rainfall. An insulating
cover of poly-vinyl chloride and a thermostatic control insure
the proper gage temperature. The thermostatic control is adjus-
table from 0 to 35°C. Snow falling into the inlet funnel is
melted. The resulting water (from rain or snow) drains into a
precision tipping bucket mechanism which activates a mercury

switch each time the bucket fills and tips. The gage is constructed

Il C-706

E2RZADIAN corporarion

@ of durable corrosion-resistant materials to provide many years of
service. The specifications of this gage are as follows:

¢ Orifice: 8 inches

: Callibeat ions 0.01 inch

- Accuracy: 0.5% (Calibrated at 0.5 in/hr).
- Sensor: Chrome plated tipping buckets

- Switch Mercury, “0.1 second closure

- Heat Control: Thermostat adjustment,

Oto 35°C.
@ 2. 200-Foot Meteorological Tower
The tower has instrumentation at four levels: feet,

30 feet, 100 feet, and +200 feetz VAtrall four levels, there ace:
wind speed, wind direction, and temperature and relative humidity
sensors in a power aspirated radiation shield. Temperature dif-
ference thermistors (also in power aspirated radiation shields)
and their associated circuitry take lapse rate measurements for
the 35-foot to 100-foot layer and the 30-foot to 200-foot layer.
in addition, this site has a Precision Spectral Pyranometer, a

barometer, and a tipping bucket rain/snow gage.

The wind direction and speed apparatus used at each
measurement level of the tower is the Model 1074-2 wind sensor
by Meteorological Research, Inc. (MRI). This sensor has a 540°
potentiometer for wind direction and a light chopper for wind

@ speed. This sensor is rugged, with an all-weather coaxial cup and

II C-707

EPFL fild corPcRATIONn

damped vane assembly. The prototype model has been in operation
for years under the most demanding weather conditions, performing
continuously with the utmost reliability. All of the wind sensors
on the tower have been specially treated with a black paint which
will promote warming of the exposed surfaces of the sensor and
thereby reduce ice and snow accumulations on the moving parts of
the apparatus. The specifications on the Model 1074-2 are as
follows:

Wind Speed

+ Starting Threshold: 0.75 mph

- Response Distance: 18 feet (63% recovery)
- Flow Coefficient: 7.9 feet/Revolution

¢ Accuracy: + 0.4 mph or 1% (whichever
is greater)

* Range: 0-100 mph
Wind Direction
Startane Threshotd; 0.73 mph
Delay Distance: 4 feet (50% cu nee
Damping Ratio: 0.5 to 0.6
Accuracy (540° system): + 17%

Range: 0° to 540°

II C-708

FeAIDIANS CORPORATION

The relative humidity and temperature sensors are mounted
within a power aspirated radiation shield at each tower level.
All aspirators and sensors are of the Model 840 Series by MRI.
The aspirated shielded housing is designed to provide maximum
radiation protection to the sensor. Ambient air is drawn into
the shield and across the sensors at approximately 15 feet per
second. This intake air is essentially sampled from a hemispherical
space which is approximately 3-inch radius from the tube opening.
Speed of the incoming air at the periphery of this hemisphere is
approximately 1 mph.

The temperature sensor is comprised of a dual thermistor
and resistor network. This circuit provides a linear resistance
change with an air temperature change. The relative humidity
sensor is placed alongside the temperature elements inside the

‘shield where it is exposed to a constant flow of air. Circulation

to both sides of the sensing element produces accurate monitoring

with a good response time. The specifications on the sensing ele-
ments are as follows:

Temperature

- Accuracy: + 0.25°C

- Range: -50°C to +50°C

Humidity

-, Accuracy: 7253707. Ru

* Range: 0% to 100% Relative Humidity

Measurements of temperature difference are taken for two
layers,.the: 30-Loeet to 100-fcot dayer and’ the 30-foot, te 200=teot

ii C=708

E2PABDIAR corpcrarion

=

layer. The thermistors and circuitry used for these measurements
are separate from the thermistors measuring air temperature. The
use of separate thermistors and circuitry to measure AT allows

for much greater accuracy and resolution in the measurements, which
is necessary for stability assessments. Two AT thermistors are at
the 30-foot level, one is at the 100-foot level, and one is at the
200-foot level. All of these AT thermistors are mounted within
power aspirated radiation shields. The specifications on the AT
instrumentation are as follows:

= “mecuracy> + 0:1¢

- Range of AT Circuit
(Lower Level-Upper Level): +4°F to -8°F

All instrumentation, except at the ground level, is
mounted at the end of 12-foot retractable booms. These booms are
3-inch box beams which are on rollers and can be retracted to the

instrument platforms for instrument maintenance.

The meteorological tower itself is a 200-foot Rohn
Model 80 Guyed Tower, designed for 40 pounds per square foot wind
load with 4"" of radial ice per EIA Standard RS-222-B, to support
four levels of meteorological equipment. The material consists
of tower sections with a tapered base, three retractable booms
12-feet long, three outside work platforms, an inside ladder for
climbing, two base ground kits and one anchor ground kit. The
cable-type Safety Climbing Device consists of a cable and attach-
ment mechanisms with a locking sleeve and safety belt. The tower

is lighted and painted according to FAA specifications.

The signals from the tower instrumentation are fed from

multiple signal cables into transmitters mounted at the base of

Lr C-720

RADII CORPORATION

the tower. After signals have been converted to analog signals,
they are fed into a junction box, also at the tower base, where
they are assimilated into one coaxial cable. The signals are then
run underground within 3"' PVC conduit to the A-to-D assembly, where
they are processed. The transmitters are shielded and insulated
from the elements. The signal cable is run underground in PVC
conduit in order to minimize damage from the weather or various
rodents in the region.

The auxiliary equipment at the tower site consists of a
heated tipping bucket rain/snow gage, an analog barometer, and a
Precision Spectral Pyranometer. The rain/snow gage is the Model
P511-E unit by Weather Measure, with characteristics and specifi-
cations as described in Section 1. The barometer is the B242

Analog Output Barometer by Weather Measure. This barometer provides

an output voltage that is linearly proportional to pressure. The
Specifications on this instrument, which is mounted inside the
monitoring trailer at the site, are as follows:

*- Range: Specially designed for the 100
miliibar interval fromig25'imillibars te
825 millibacs .

Resolution. Infinite

Banéariew. = 0/5 milbiper, overethevres
millibar interval

The pyranometer at the site is the Eppley Precision
Spectral Pyranometer. This instrument is used for the measure-
ment of sun and sky radiation totally or in defined wavelength
bands. The pyranometer is levelled and mounted atop a wooden

stand 4% feet from the ground surface. Care has been taken to

It C=7ia

hh

nr?

FAIS corrornarion

eliminate the effects from all outside influences, such as
reflection or shadows, on the pyranometer. The instrument
characteristics are as follows:

- Sensitivity: 5S mv. per) cal/cm* /min
- Independence: 300 ohms

- Temperature dependence: Sensitivity constant
to within + 1 percent over the ambient tem-
perature range from -20 to +40°C

- Linearity: Response linear up to intensities
of 4 cal/cm?/min

- Response Time: 1 second (i/e signal)

All instrumentation is factory calibrated and is field-
calibrated at various intervals. Sling psychrometers are used to
calibrate the humidity sensors, known temperatures and/or resistances
are used to calibrate the thermistors, and an rpm calibrating
unit is used to calibrate the anemometers. The wind direction
instrumentation is aligned to true north (reference direction)

by means of a surveyor's transit.

II C-712

RADIAN CORPORATION

LEG MICROMETEOROLOGICAL AND TERRAIN FEATURES

The Piceance Creek Valley and C-b Oil Shale Tract
are situated such that many microscale meteorological pheno-
mena affect the region where the ambient air monitoring units
are located. In particular, the three units in the Piceance
Creek Valley (Trailers 020, 021, and 022) are heavily influenced
by a katabatic-anabatic flow regime. Trailer 023 and its
associated 200-foot meteorological tower are located atop a
plateau to the south of the valley, high enough to be affected
mostly by gradient flow conditions. Trailer 024, located half-
way between the valley and the meteorological tower, is affected
by a mixture of the gradient and mountain-valley flow regimes.

Elevations in the monitoring network range from about
6200 feet above sea level at Trailer 021, near the Rock Creek
Schcoi in the valley at the westernmost end of the monitoring
network, to 6940 feet at the meteorological tower site (Trailer
023) atop the plateau within the Tract C-b itself. The largest
gradients in elevation in this ares, of cotirse, occtr At joke
Piceance Creek Valley walls. However, the northern valley walls
are slightly steeper than those at the southern boundary of
the valley, which then slopes upward gradually toward the C-b
Tract. The Piceance Creek Valley decreases in elevation from
east to west in -this area, so that nighttime katabatic cold-
air drainage flows advect from east to west, or from Trailer 022
to Trailer. O20°to Draiser 22.

As mentioned at the outset of this discussion, the
terrain will have a large influence on the meteorology of this
region. Considering fLirst)Trailer 022, .at the eastem end of
the monitoring network, a nighttime katabatic (valley or down-

slope) flow will exert a tremendous influence on this site.

Le Nu Oe

RADIA corrorarion

Of the three monitoring locations in the Piceance Creek Valley,
this site has the steepest valley walls in its vicinity. As a
result, the nighttime katabatic flow is strongest here. That is,
the downslope winds are constrained or channelled at this point
such that the nighttime drainage winds often reach 15 miles per
nour.) In addition, the channelling effects of the Piceance Creek
Valley walls normally cause surface winds to flow from one of
two preferred directions. At night, the downslope winds
parallel the valley contours, generally coming from 115° (east-
southeast, referenced to true north). During the afternoon,

or whenever suitable pressure gradient conditions exist, the
winds generally come from the west-northwest because of the
boundary conditions and channelling caused by the valley. This
monitoring location has an elevation of approximately 6450 feet
above sea level and is at the mouth of Oldland Gulch.

Trailer 020, midway down the Piceance Creek Valley
near the Redd Ranch, at the mouth of Gardenhire Gulch, has an
elevation of about 6320 feet above sea level. Once again, the
valley walls are steeper to the north of this monitoring loca-
tion. The Piceance Creek Valley widens a little from Teailen
022 to Trailer 020, so that channelling effects are not quite
as great at this location. Nevertheless, a well-developed
katabatic-anabatic flow cycle affects this site, with the “after-
noon anabatic flow being fairly well-developed at this location.
The channelling effects of the valley walls cause two preferred
surface wind directions, southeast and northwest. However,
other wind directicns are experienced here, particularly during
the transition periods between downslope and upslope flows and
during periods when the surface pressure gradient dictates to

a large degree the surface wind direction.

IT C-714

FEAIDIAL CORPCRATION

Trailer 021, located near the Rock Creek School, has
the lowest elevation of the three valley trailers, 6200 feet.
At this point, the Piceance Creek Valley widens considerably
toward the east, so that nighttime katabatic winds are rather
light. Daytime anabatic winds are also rather light. However,
northwesterly surface winds caused by pressure gradient forces
are occasionally moderate in force because of the slight channel-
ling effects of the valley walls to the north and northwest.

Site 023, where the 200-foot meteorological tower is
located, is atop the plateau at an elevation of about 6940 feet
above sea level: It is approximately 2.5 miles south of the
Piceance Creek Valley. This location is relatively high compared
to its surroundings, with the nearest points having elevations
greater than 7000 feet being .5 miles to the south of the tower.
The tower itself is on the top of a small knoll located between
Scandard and Sorghum Gulches. Because of its location and the

irregularities of the surrounding terrain, meteorological patterns

are varied here.

Wind instrumentation is mounted at four levels of
the meteorological tower; 8 feet, 30 feet, 1C0 feet, and 200
feet. The top level of the tower generally remains in gradient
wind flow. That is, the winds at that level are normally
generated by synoptic-scale features and are usually separated
from terrain features and micrometeorological circulations.
Occasionally, a weak anabatic flow influence is experienced.
However, such is not the case with the three Lowest measurement
levels. To varying degrees, these levels are influenced by
both the katabatic and anabatic circulation cells. However, when
strong pressure gradient forces exist in the region and the
Synoptic-scale wind flow is strong, all four tower levels will
reflect a gradient wind flow, with the winds increasing in

strength with increasing height.

II C-715

F2eFAS IAN corrorarion

Trailer 024 is between the Piceance Creek Valley and
the meteorological tower location, about 1 mile south of the
valley itself. The elevation of this site is approximately 6740
feet. The terrain slopes downward to the west, north, and east,
and slopes upward toward the south, in the direction of the
meteorological tower. This site is in a transition zone between
the micrometeorological effects which prevail in the valley and
those meteorological phenomena affecting the tower site. Asa
result, the meteorological parameters measured at this location
are subject to rather rapid variations. The area is generally
affected by a weak katabatic (downslope) flow at night and a
weak anabatic (upslope) flow during the afternoon hours. However,
gradient wind flows generally take precedence over terrain-
induced flows at this location.

The terrain atop the plateau is generally barren and
fairly rugged, with a few scattered small trees. The topsoil
dries rapidly and is very fine, resulting in blowing dust when
dry, windy conditions exist. In the Piceance Creek Valley,
the terrain is fairly grassy and flat, with steep valley walls
on either side. Surface winds are normally rather light in this

valley unless channelling effects occur.

During clear nights with rather light pressure gradient-
induced winds, rapid radiational cooling will occur in the region
because of the barren nature of the terrain and the generally
@ry character of the giz in this perceion tot..the “country. ~ Asa
result, the diurnal range of temperatures will be extremely
large. Because of the katabatic flow in the valley, nighttime
temperatures will generally be lower in the valley than on the
plateau. During the winter, especially, temperatures in the
valley may be 20°F lower than they are on the plateau during
the early morning hours. In particular, the drainage effects

will be spectacular at Trailer 021, which will often experience

IT Ce fi6

E2fADIAAnN ecrrorarion

temperatures 10°F cooler than those at the other valley monitoring
locations during the early morning hours. This phenomenon results
from the pooling of cold air in the area of Trailer 021 because
of its relatively low elevation and the light nature of the winds
here during the night, which thus inhibits surface mixing and
promotes the strengthening of the nighttime pround-based inver-
sion. During periods of strong gradient winds and/or cloudy
skies, greater mixing of the air near the surface occurs and
meteorological conditions (particularly temperature and humidity)
are more uniform throughout the monitoring network. (on the
plateau and in the valley).

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E25, DIFA23 corPoraricn

IV. OPERATING TIME ANALYSIS

The amended Oil Shale Lease Environmental Stipulations
require monitoring air quality for sulfur dioxide (S02), hydrogen
sulfide (H2S), and suspended particulates on a continuous basis
(when applicable). In addition, hydrocarbons, oxides of nitrogen
and other pollutants will be continuously monitored as deemed
necessary by the Area Oil Shale Supervisor. Requirements for
meteorological monitoring include wind speed and direction at
three levels near the proposed plant site, one monitor at a
height of approximately 30 feet, one not less than 100 feet, and
one at an intermediate level. Temperature is to be monitored at
the 30-foot level and at a level at least 100 feet above the plant
site. Humidity is to be monitored at one level, height not
specified. All these meteorological parameters are to be monitored
at least 95 percent of the time over each lease year.

The lease stipulations in force at the time the air
monitoring network for Tract C-b was designed required
monitoring at four sites for S02, H2S and particulates; required
monitoring for hydrocarbons, oxides of nitrogen and other pol-
lutants as deemed necessary by the mining supervisor; and required
monitoring over at least 90 percent of each lease year. In order
to meet these requirements for 90 percent monitoring at four
stations the network design included a complete spare station to
be operated continuously so that even with a failure in one station,
four stations would still be monitoring. The met tower was designed
to monitor wind speed, wind direction, temperature, and relative
humidity at four levels: 200 feet, 100 feet, 30 feet and $ feet?

Since the lease stipulations have changed since the net-
work was designed, the operating time analysis will be presented
2as follows.

IT C-719

en"

F2FADDi fils corpernrion

(1) Air Quality Stations

Downtime will be reported as the number of channel-days
in the quarter that each channel in each station was not
taking data (Table I), and all five stations will be reported.
Calibration time will not be counted as downtime. A particular
channel will be marked as down on any day when it collects less
than half the available data points for that day.

The three stations along Piceance Creek had electrical
power prior to September 1 (020, 021,:022). Station 023 operated
on power from a diesel generator from September 4 to October 4.
Station 024 operated on power from a diesel generator from
September 27 to October 4. Electrical lines were available
at 023 and 024 after October 4.

Table II lists air quality data collection percentages
for each species for each month and for the quarter. The quarter-
ly average for gaseous species and for all species are also
given. For SO2, H2S, and particulates, the percentages were
obtained with an effective four station network from the four
stations plus one operating spare station (023). For the other
species the percentages were obtained with an effective one
station network from one station (020), plus one operating spare
station (023).

(2) Meteorological Tower

The channels which will be reported in the operating
time analysis include wind speed and wind direction at the 200,
100 and 30-foot levels; the temperature at the 200, 100 and 30-
foot levels; and the relative humidity at the 200, 100 and 30-
foot levels (Table III). Downtime will be reported as the number

of channel-days in each quarter that each of the above data

II C-720

FRAARSIAAN ecorrcraricn

TABLE I

OPERATING TIME ANALYSIS

AIR QUALITY STATIONS

The numbers represent the number of channel-days the

particular data channel in each station was not taking data.

STATION:
SO2

H.S
Particulates
NO

5

NO

03

Number of days of electrical power per site:

020

37

5

0)

020
021
022
023
024

Zn

(es,

I]

a8
oT
a2
88
64

022
41

29

84

023
mB

43

79

35

34

62

59

45

a9

024
28

19

60

E2EkSSisihdy corPporRAvAtion

S02
H2S

Particulates

DATA COLLECTION PERCENTAGES*

SEPT

70

TABLE II
AIR QUALITY

OCT

aL
a2
22
oF
oy
97
39
a2
13
71
100

NOV

99
100
18
100
100
100
73
73
73
83
97

Quarterly Average for Gaseous Species - 76%

Quarterly Average for All Species

*As defined in operating analysis discussion.

II C-722

- 627%

QUARTERLY

80
78
14
86
86
86
48
38
ae
tie.
96

FREADILAT corpoRrRarion

. TABLE III

OPERATING TIME ANALYSIS
METEOROLOGICAL TOWER

The numbers represent the number of channel-days the
particular channel was not taking data.

Channel-Days

SeDE ;) Oct. Nov.
Wind Speed
200-foot Zi 25 0
100-foot Zz. Sy 0
30-foot 24 18 0
Wind Direction
200-foot | 5 0
109-foot 22 5 0
30-foot 24 5 0
Temperature
200-foot 2b 7 0
100-foot g2 8 0
30-foot 22 | 0
Relative Humidity
200-foot 2a 5 0
100-foot Zi 5 0
30-foot 21 5 0
Percent met data collection this quarter = 64% (as described

in operating time analysis discussion).

Li C-12s

FRAAES IAAI corrorarion

channels were not taking data. A particular data channel will be
marked as down on any day when it collects less than half of

the available data points for that day. The percent monitoring
achieved will be calculated based on wind speed being taken

at the 200, 100 and 30-foot levels; wind direction being taken

at the 30-foot level and either. the 100 or 200-foot level; and
relative humidity being taken at the 200, 100 and 30-foot level.

II C-724

RADIAN conrorarion

re METEOROLOGICAL SUMMARY

The period from September through November brought
near normal average temperatures and precipitation to the Tract
C-b region of western Colorado. Temperatures were mild to
warm throughout the first half of the quarter, but became much
cooler during the second half of the period, particularly in
November. However, such a climatological sequence is normal
for the region. Although precipitation totals were near normal
for the quarter, the actual amounts received were light (about
two and one-half inches), since the area seldom measures more
than one inch of precipitation during any one month.

The western Colorado region had basically sunny
skies during the September to November quarter. For the entire
period under consideration, the area received about 75% of the
possible sunshine. The region had a total of 45 clear days,
20 partly cloudy days, and 26 cloudy days. Cloud coverage in
the Tract C-b region averaged 4.2 out of a possible 10 for the
sunrise to sunset time period and 3.8 out of a possible 10
for the entire quarter. September had an unusually large number
of clear days, while October was rather cloudy. November had
near normal amounts of cloudiness.

For the quarter, the mean upper flow showed a slight
ridging condition through the Intermountain Region and slight
troughing over the eastern United States. This ridging was
particularly well-developed and persistent during September.
The quarter was particularly noteworthy for the large number
of upper cyclonic circulations which separated from the main
portion of the upper flow and settled over the southwestern
United States. As a result, precipitation over New Mexico,
Arizona, Texas, and southern portions of Colorado was well

above normal during the quarter.

11 C-725

2

Adam |

| venwett: |

E2AAED ELAR corporation

Considering the Tract C-b, the stability wind rose
shows that winds on the plateau during the September to Novem-
ber quarter most commonly were southeasterly through south-
southwesterly and west-northwesterly to northwesterly. The
other frequencies of occurrence of wind direction showed a
bias toward the western half of the distribution. Winds from
the northeast quadrant were fairly uncommon during the quarter.
The strongest winds on the plateau, however, were almost always
south-southeasterly to south-southwesterly or northwesterly,
preceding and following the passage of a cold front, respectively.
Winds in the Piceance Creek Valley, which showed a very strong
katabatic-anabatic circulation dependency, were generally much
lighter than those winds on the plateau and were generally
east-southeasterly or west-northwesterly in direction.

Nighttime temperatures were normally lower in the
valley than on the plateau during the quarter because of the
strong radiational cooling which prevailed on clear nights
with light winds. Therefore, diurnal temperature ranges were
much greater in the valley. Trailer 021 normally achieved
nighttime minimum temperatures which were considerably colder
than temperatures at other monitoring locations when the well-

developed radiational cooling conditions existed.

Considering each month separately:

[I C-726

REID IAT corrorrrion

MONTHLY METEOROLOGICAL SUMMARY FOR SEPTEMBER

A. Summary of the Major Features of the

General Circulation Affecting Western
Colorado

The domination of the upper air flow pattern by merid-
ional characteristics which existed during August continued into
the month of September over the North American continent. The
- long-wave circulation alternated between meridional and zonal
flow throughout the month, with each regime lasting for a period
of about five days. However, the periods of large amplitude in
the long-waves were dominant in relation to the mean circulation
patter.

The mean position of the axis of the long-wave trough
during September was located through the central part of North
America as it was during the month of August. This circulation
pattern produced below normal temperatures and above normal pre-
cipitation from the Rocky Mountains eastward to the Appalachians.
Rainfall was slightly above normal and temperatures were slightly
below normal along the Atlantic Coast. Temperatures were above
normal and precipitation was below normal in western North
America because of the persistence of the upper ridge in that
region. However, the southwestern United States was an exception
to the generally dry conditions in the west because of a succes-
sion of cold-core low pressure areas aloft which cut off from the
main flow and settled over Arizona. These cutoff lows in com-
bination with an abundance of moist air at high altitudes off
the Pacific Ocean resulted in copious amounts of rainfall in
Arizona, New Mexico, and the western half of Texas during
September. El Paso, Texas, for instance, had measurable pre-
cipitation on 12 days during September, with 2 total rainfall for
the month of 6.68 inches, which is 5.52 inches above normal.

IVC -F27

RADIAN corporavrion | cs | |

September also produced two powerful hurricanes, Carmen |
and Fifi. Hurricane Carmen achieved landfall south of New Orleans,
Louisiana, during the evening of September 7th. Hurricane Fifi had |
a landfall near Belize in Central American on September 19th. How-
ever Fifi eventually meandered through Central American into the
Pacific Ocean, where it regenerated into Pacific Hurricane Orlene. |
Orlene then tracked northward toward the Baha Peninsula and was
eventually partly responsible for the heavy rains in the south-
western United States on September 22nd, 23rd, and 24th, as its
moisture became entrained in the subtropical jet stream which
traveled over the Pacific Ocean and then over Mexico, New Mexico,
and Texas.

Meteorological events on September lst centered on the
meridional flow enveloping North America. A strong blocking ridge
was centered off British Columbia, while a large amplitude trough
extended from Hudson's Bay to Oregon. A strong cold front, featur-
ing several surface waves, extended on a northwest-southeast line
through Colorado. The blocking ridge aloft began to weaken on
September 2nd and the entire long-wave trough began to move east-
ward rapidly as the next long-wave trough in the hemispherical flow
pattern dug southeastward at 150° W latitude. The surface continental
polar cold front strengthened at this time and pushed westward over
the Tract C-b region during the morning, bringing much cooler ten-
peratures to the area.

By September 3rd, the polar front jet stream had weakened
considerably and the long-wave trough axis had moved eastward to a
position at 90° W latitude. Correspondingly, the long-wave ridge
in western North America also weakened considerably. As a result,
the plateau region of Colorado had mild, fair weather and light

winds with a warming trend beginning to develop in the area.

IT G-728

RADIAN corporation

September 4th featured the weakening of all of the
prominent weather systems in North America. The long-wave trough,
which was still centered along 90° W, weakened further as did the
ridge in the west. Mild, fair weather and light winds continued at
Tract C-b because of the subsiding air aloft and the gradually
weakening surface pressure gradient. By September 5th, the upper
circulation showed definite zonal tendencies. However, a strong
short-wave in the northern Rockies was digging through what re-
mained of the long-wave ridge at this time. The maritime polar
cold front associated with this short-wave trough moved rapidly
through Colorado during the day, cooling temperatures slightly

and causing a few showers which were mostly orographic in nature.

On September 6th the short-wave began to dig into the
long-wave trough position over central North America after hav-
ing passed through the ridge position. The 500-millibar flow
was basically weak. A weak surface high pressure area was
centered over northern Arizona, causing warm temperatures, light
winds, and generally fair skies in western Colorado. September
7th brought little change in the meteorological conditions at
the Tract C-b. The weak surface high was now centered over
central Colorado and ridging aloft was building northward into
the state. Skies remained clear and temperatures were warm, much
above normal for the time of year. Because of the weak pressure
gradient, winds remained light and orographic wind systems (valley
and mountain circulations) were well developed.

On September 8th, a weak, zonal 500-millibar flow pre-
vailed over North America with slight ridging over the plateau
region. A surface high was again centered in Colorado. Tempera-
tures were well above normal with some orographic showers over
the Rocky Mountains to the east; winds were fairly trent.

September 9th was a continuation of the zonal pattern over North

Pi,C-729

RADAR Cesena

America. Temperatures were once again well above normal through-
out western Colorado. Scattered showers continued to dot the
region. A weak surface low began to develop in the vicinity of
Grand Junction.

September 10th signaled an end to the zonal flow of the
previous few days as a strong short-wave began to dig over the
northwestern coast of the United States. The developing surface
low of the previous day was stationary over western Colorado and
eastern Utah. A strong continental polar cold frontal system
began to organize in northern Montana. The extremely hot weather
continued over western Colorado, but the showers became more
mumerous and the surface winds increased in strength as the low
deepened.

September lith saw rapid changes occur in the long-wave
pattern. The short-wave continued to dig southward in the western
United States, as lee cyclogenesis took place in southeastern
Colorado. In conjunction with the digging trough, a long-wave
ridge began to build northward upstream around 130° W. The sur-
face low over western Colorado remained intact and was fairly
strong (996 millibars). The cold front over the northwestern
United States advanced steadily southeastward, passing through
the Tract C-b region during the late afternoon. This frontal
passage brought showers and thundershowers, a sharp drop in
temperatures, and strong winds to the area. By September 12th
the upper flow was strongly meridional, with the long-wave ridge
continuing to build in the Gulf of Alaska and the long-wave trough
amplifying over the plateau states. The cessation of positive
vorticity advection over the region during the early morning hours
resulted in clear skies during the remainder of the day, but tem-
peratures were nevertheless much lower than those of the preceding
day because of the continuing cold air advection. Winds diminished

in strength during the day.

iI C-730

RADIAN corPporaTion

On September 13th another short-wave trough dug south-
ward into the long-wave trough position over western North
America. However, the short-wave trough had the effect of tilt-
ing the mean long-wave trough axis to a southwest-northeast
line. Also, the vorticity from this system hung back over Nevada
and Utah as the rest of the long-wave moved eastward slightly.
The development was the beginning of the first of a series of
cold-core cutoff lows over the southwestern United States.
Cloudiness and a few showers also returned to western Colorado
‘because of this system. Temperatures on the 13th moderated some-
what from the cool temperatures of the preceding day. Winds were
generally light and variable.

By September 14th, a cold low aloft had formed over
northeastern Nevada. As a result, cloudiness and showers were
widespread over the western half of Colorado and all of Utah.
Temperatures were mild and the winds were light and variable.
On the 15th of September the 500-millibar low was over northern

Arizona. Widespread rains continued over Colorado, as temperatures

varied little from those of the 14th and light winds prevailed
because of a weak surface pressure gradient.

By September 16th the low aloft had moved northeastward
to the vicinity of Grand Junction and had filled slightly. There-

fore, the rains and cloudiness decreased somewhat in western

Colorado, although showers and thundershowers were still scattered
around the region during the afternoon. Temperatures remained mild
and winds remained Puen. ‘On September 17th, the upper ridge which
had extended from California to British Columbia during the pre-
ceding three days weakened as a short-wave pushed over it and be-
gan to drop into the central part of North America. The weak
cyclonic circulation aloft remained over the southwestern United

States, centered over central Arizona. A few cumulonimbus clouds

nad C-751

RADIA corPpcrRaArTrIONn | . |

were scattered over the area during the afternoon. A warming trend |

|

the long-wave ridge and dug into Alberta, Canada. The weak cutoff |

began to effect the region, although winds were still rather light.
On September 18th another strong short-wave pushed through

low circulation retrograded slightly to southwestern Arizona.
Temperatures continued their warming trend and cloudiness decreased |
somewhat over the Tract C-b region. The cutoff remained stationary
over Arizona on the 19th, but the upper flow pattern became more
meridional as a ridge built northward in the Gulf of Alaska and

a strong short-wave trough dug southward just east of the Rockies.
Although a small surface low developed in eastern Utah, skies were
clear throughout northwestern and west central Colorado. Winds were
generally light. |

On September 20th the strong meridional flow pattern
continued, with a ridge in the Gulf of Alaska and a long-wave
trough through central North America. The now strengthening
stationary cold low aloft was centered over extreme southwestern
Arizona. A cold front eased through the area from the east dur-
ing the late afternoon but affected temperatures only minimally;
the main effects of the front being a drying of the air and a
shifting of the winds to a northerly direction. Skies remained
clear throughout the day. The low aloft over the southwestern
United States drifted southward into Mexico and filled slightly
on the 2lst and the meridional nature of the upper circulation
over North America continued on this day. Western Colorado was
clear and warm because of the subsiding air from the upper ridge
to the west. Local circulations (anabatic and katabatic flows)
were well developed on the 21st.

On September 22nd the cold cutoff low over southwestern

Arizona strengthened once again as cold air was advected into it.

LD. Ceygae

PeADIAR CORPORATION

Meridional flow continued over North America as the long-wave
trough axis progressed eastward to a position through the Ohio
River Valley. Meanwhile, the remains of Atlantic Hurricane Fifi,
which had slammed into Belize in Central America three days
earlier, reorganized into Pacific Hurricane Orlene and moved
northward toward the Baja Peninsula. Generally, partly cloudy
skies prevailed over western Colorado on this day, with warm
temperatures, light winds, and a few showers scattered over the
region.

The generally meridional long-wave pattern progressed
slightly eastward on September 23rd. The low aloft remained
stationary over southwestern Arizona and a small surface low and
weak lee trough began to develop over northeastern Colorado.
This troughing action shifted the winds to a northwesterly
direction during the afternoon, in western Colorado, but the
wind speeds remained low. Skies were clear throughout the area
except for a few orographic showers and temperatures were mild
at. the Tract C-—b-

Several large-scale changes occurred on September 24th.
The cutoff low over Arizona weakened, as did the entire meridional
pattern over North America. However, a strong short-wave in the
Gulf of Alaska began to work its way through the long-wave ridge
off the western coast of Canada. Scattered cloudiness and a
few showers returned to western Colorado, but temperatures re-
mained warm. Winds increased in speed somewhat. By September
25th the long-wave pattern became zonal across the United States.
However, the strong short-wave continued its southeastward pro-
gression through British Columbia. Scattered cloudiness, a few
showers, mild temperatures, and generally light winds prevailed

Over western Colorado.

RRADIAT corrorRaArion

_ A zonal flow pattern existed over North American on
September 26th. The cold low aloft which had persisted over the.
southwestern United States for the past twelve days was finally
ejected northeastward into Oklahoma by the strong short-wave in
the northwest, which had reached the Washington coast. A strong
maritime polar cold front organized along the northwestern United
States-Canada border. Meteorological conditions in the Tract C-b
region changed little from those of the previous day, with partly
cloudy skies, scattered afternoon showers, light winds, and mild
temperatures in the area.

Rapid changes occurred on September 27th. The strong
short-wave dug southward over the west central United States
as a strong maritime polar cold front rushed through the Inter-
mountain region of the western United States. The cold front
_passed through the Tract C-b region during the late morning,
causing scattered showers, strong northwesterly winds, some
blowing dust, and much cooler temperatures. Skies cleared by
sunset. By September 28th the short-wave and cold frontal system
had continued to move southeastward rapidly and had reached the
central section of North America. Surface and upper ridging
affected western Colorado, causing freezing temperatures (during

the night), clear skies, and diminishing northwesterly winds.

A broad long-wave troughing pattern enveloped North

American on September 29th with several strong short-waves en-
trenched in the flow. The jet stream and its baroclinicity re-
treated northward to a Montana-South Dakota line. Subsiding air
continued to affect western Colorado, causing clear skies, moderat-
ing temperatures, light winds, and extremely dry conditions. The
long-wave pattern became more zonal on September 30th as fast polar
jet stream westerlies affected the northern sections of the United

States. Meteorological conditions in the Tract C-b area changed

IT C-734

RADIAN corPoRATION

little from those of the previous day, with continuing clear skies,

light winds, mild temperatures, and very dry air.

B. Micrometeorology of the Tract C-b Region

The Piceance Creek Basin is subject to local circula-
tions (anabatic and katabatic winds) of varying intensities through-
out the year. These flows are best organized when clear skies and
a weak pressure gradient prevail over the area, conditions which
are rather common in western Colorado. During the night the higher
elevations cool more rapidly than the valley floor, causing cold,
dense air to collect and flow toward lower elevations. During the
day the opposite effect occurs, in that the higher elevations re-
ceive more direct insolation earlier in the day, causing them to
warm more rapidly. The resultant density difference between the
valley tops and valley floor causes an anabatic flow, with winds
blowing up the valley floor and walls.

Considering the Piceance Creek Basin and the three monitor-
ing trailers located in this valley, the valley-mountain flow regime
is very evident. Trailer 022 has the most eastern location of the
three trailers in this valley and has the highest elevation above:
mean sea level. Trailer 021 is located at the western end of the
valley and has the lowest elevation above mean sea level. Trailer
020 is intermediate in both location and elevation. These loca-
tion and elevation differences cause micrometeorological effects
to appear in the data as a result of the dominent anabatic-katabatic
flow regime in the valley.

For instance, considering the diurnal variations of wind
speeds at these three trailers, winds are strongest (6 mph) on the

average at Trailer 022 which has the highest elevation. Winds were

Be -C- 735

i |

RADIA corPORATION

lightest on the average during September at Trailer 021, which

is at the lower end of the valley. The diurnal wind speed distri-
bution for these three trailers indicates that the katabatic
(downslope) wind is strongest at Trailer 022 and weakest at
Trailer 021. Conversely, the anabatic (upslope) wind is most
strongly developed at Trailer 020 and equal in intensity at the
other two trailers. That is, nighttime winds are strongest at
Trailer 022 and weakest at Trailer 021. Daytime winds are
strongest at Trailer 020.

These winds have a profound influence on the temperatures
experienced in all three locations. Trailer 022 has the highest
mean temperatures. It is warmest at night because radiational
cooling is inhibited by the relatively strong winds. Conversely,
Trailer 021 has the lowest mean temperatures. This is because
nighttime winds are lightest at this location, allowing excellent
radiational cooling. Also, cool air from the eastern portions of
the Piceance Creek valley drains into this area and settles, caus-.
ing colder nighttime readings. Moreover, daytime high temperatures
are highest at Trailer 022 and lowest at Trailer 021. Temperatures
in the valley during September generally averaged 53.5°F, with an
average maximum temperature of 71°F and an average minimum of
37°F. The highest maximum temperature for September was 93°F at
Trailer 020 on the 9th and the minimum was 14°F for the 30th at
Frazier 02%;

Relative humidities during September averaged 50% in the
valley. On a diurnal basis the average maximum relative humidity
values of 75% occurred at 0800 hours. The average minimum values,
about 28%, occurred at 1800 hours. The highest mean humidities
occurred at Trailer 022 and the lowest mean humidities were at
Trailer 021. Humidities of less than 15% were common at Trailer
021 during the last half of September.

II C-756

RADIAN coRPORATION

The existence of a local circulation cell in this valley
(anabatic-katabatic) is evident upon inspection of the wind
direction data. Winds are generally east-southeasterly at all
valley trailers during the night when the katabatic flow dominates
and west-northwesterly during the day when the anabatic circula-
tion takes effect. On days during September with well developed
upslope-downslope flow characteristics winds were easterly
(90° to 110°) and downslope during the nighttime period from
1900 hours to 800 hours. The winds then went through a transition
period for the next two hours, backing into the north and then
into the west-northwest (300°) by 1000 hours. These anabatic
winds usually prevailed until approximately 1800 hours, at which
time they would abruptly veer to a northerly direction and then
settle into an easterly direction, usually by 1900 hours, as the
katabatic flow again took over. |

Conditions at the Tract C-b itself, up on the plateau,
were somewhat different. In particular, the anabatic-katabatic
circulation cell is not as well developed on the plateau. Also,
the cooler air generally drains into the valley from the plateau,
causing two main effects: (1) the depth of the ground-based
radiation inversion is rather shallow (averaging slightly more
than 100 feet in depth during September), and (2) temperatures
at night are not as low during radiational cooling nights as they
are in the valley.

Because the upslope-downslope flow does not effect the
tract to the extent that it does the valley, wind directions on
the plateau have a high frequency from the southwestern quadrant,
in connection with the geostrophic flow (large-scale flow related
to pressure gradients). In particular, the 200-foot level of the
tower has a very high frequency of southwesterly winds, even at
night when the lower tower levels are enveloped by a ground-based

radiation inversion and drainage flow.

Il C-737

FPALLAN eccrrPornv7icn

Winds can be rather strong on the plateau and around the
tower site. The highest hourly average wind speed recorded during
September was 24 miles per hour on September 27th, as a strong cold
front passed the area. Winds increased in speed with height dur-
ing September, as was to be expected. The average wind speed at
the 100-foot level for the month was 9 mph, higher than in the
valley. .

The air was much drier on the plateau than in the valley
(moisture occasionally becomes trapped in the valleys) during»
September. Humidities for the month averaged in the low 30's.

Mean temperatures for the month of September were slightly
higher on the plateau than the valley. Daytime temperatures
averaged about 2 degrees lower at the tower site then in the valley,
but nighttime temperatures were about bere higher, with an average
minimum temperature of 42°F and an average maximum of 69°F. The
average temperature at 200 feet was 55°F, but the diurnal range

of temperatures was smaller than at the lower tower levels.

lI C~738

E2ZAD IFAT corrornation

MONTHLY METEOROLOGICAL SUMMARY FOR OCTOBER

A. Summary of the Major Features of the Upper
Flow Over North America

. North America during October alternated between periods
of zonal and meridional flow, with two sequences of split upper
level flow. The upper flow was basically zonal (or west-east)
over the United States on October 2,4, 7, 225°13, 22; 23,7288.
The flow was generally meridional (north-south) on October 2-3,
5-6, 9, 14-21, and 25-26. Split upper level flow prevailed on
October 8, 10-11, and 27-31. The net results of these cir-
culation patterns for the month of October were: much below
normal temperatures and below normal precipitation over the north-
eastern United States; below normal temperatures and much below
normal precipitation over the Atlantic seaboard states; near
normal temperatures and precipitation over tke Central United
States; below normal temperatures and slightly below normal pre-
cipitation in the South; much below normal temperatures and below
normal precipitation in the north central United States; below
normal temperatures and above normal precipitation in the South-
western United States; slightly above normal temperatures and near
normal precipitation in the Rocky Mountain regions; and penerally
above normal temperatures and below normal precipitation in the
West.

October began with a mean long wave ridge axis extending
from western Canada to northern California. A rather deep long
wave trough was positioned through the eastern United States.
Precipitation was confined to the far northeastern portion of
the United States. A stationary cold front extended from Montana
through Wyoming to southern Nebraska. By October 2nd, the long

wave pattern had amplified so that a well defined long wave trough

mite 7152

FRADE AN corPORATION

extended from the Great Lakes to Florida. A strong upper ridge
extended from Utah to north central Canada and a deepening upper
trough was approaching the Pacific coast. A weak upper low was

off the California coast. On the surface, a large, cold high pressure
system was centered over Illinois. A warm front extended southward
along the Rocky Mountains from Canada, while a strong maritime polar
cold front came inland along the Washington coast. Precipitation

was confined to California, Washington, and the northeastern United
States.

On October 3rd, all of the major features of the circula-
tion over North America moved eastward. The long wave trough along
the Atlantic seaboard moved eastward slightly and amplified. The
upper ridge also moved eastward to a position from Kansas to
Minnesota and then northward into Canada. The upper trough in
western North America also moved eastward and flattened somewhat.
On the surface, the large surface high was still centered near the
Great Lakes region, while a cold front advanced across the Great _

Basin. Precipitation was widespread across the Intermountain Region.

By October 4th, the cold front had pushed completely
through Colorado into the Midwest. The large surface high moved
southeastward to a position along the Atlantic seaboard. At upper
levels, strong short waves were located off the ccast of the
eastern United States, along the Rocky Mountains, and along the
west coast. Precipitation, mostly light, was scattered throughout
the western two-thirds of the United States. On October 5th, the
general positioning of circulation systems remained about the same.
The long wave in the western United States amplified slightly.
Precipitation was moderate from the Great Lakes to Montana and

south from there to Kansas.

On October 6th, the northern half of the long wave which

had been over the western United States was reinforced and moved

II C-740

RADIAT corPORATION

eastward, thus causing the southern half of this wave to be sheared
off, forming a cutoff low aloft over California. The cold front
which had been across the Midwest was reinforced by the deepening
of the northern half of the short wave and moved southward as a
result. Cloudiness and precipitation were widespread in a band
from Arizona and New Mexico to Minnesota and the Great Lakes on

the 6th, but decreased throughout western Colorado.

By October 7th, the western two-thirds of the nation
was under the influence of a large dome of high pressure. The
short wave that had been over the Midwest on the 6th moved

eastward rapidly, to a position over the Great Lakes. The cold
front associated with this short wave extended southwestward
from Maine through Tennessee to central Texas. The low aloft
over California persisted, causing precipitation over southern
California and Nevada. Precipitation also extended along the
front from Texas to New York. Skies were clear to partly cloudy
over western Colorado. The upper flow pattern was split in the
western United States on October 8th, as the upper low persisted.
The cold front and short wave in the eastern United States con-
tinued to push eastward to a position off the coast. Most of the
nation was under the influence of a large, weak high pressure

system. Precipitation was confined to California and Nevada.

By October 9th, a short wave approaching the western
coast of the United States caused the upper low to be ejected
northeastward to a position over Nevada. A weak cold front
extended from the Great Lakes to Nebraska but no other significant
weather systems affected the United States. Temperatures were
cool in the Northeast but seasonable elsewhere. A weak surface
high pressure area affected most of the United States, resulting
in many areas of light winds and stagnation. Precipitation in the

United States was confined to the Great Basin area. October 10th

PG: /4

RADLAM ccorrPorRarTion

saw a split upper level flow regime return to the western United
States. A short wave trough was located from Idaho to southern
California. Showers and a few thundershowers were scattered
throughout the Intermountain Region and the western slopes of
the Rockies. A few showers fell in the Tract C-b area.

‘The split flow regime continued in the western United
States on October llth. The short wave from Idaho to California
stayed nearly stationary. A cold front extended southwestward
from a low pressure system on the Minnesota-Canada border through
Nebraska to northern New Mexico. A secondary cold front extended
westward to Montana, also from this low. Precipitation was wide-
spread throughout the western half of the nation on the 11th,
with showers and thundershowers again dotting western Colorado.

By October 12th, the two cold fronts through the northern Plains
States had organized into one strong frontal system which extended
from the Great Lakes southwestward to the Texas Panhandle. The
short wave trough which had been stationary over the western |
United States for the two previous days finally formed a weak

low pressure circulation aloft over western Arizona. Precipitation
covered a large portion of the United States extending from Arizona
northeastward in a broad band to the Great Lakes region. A large
cold high pressure system dominated the weather in the western
half of the United States behind the cold front. Considerable
cloudiness and a few showers persisted in western portions of
Colorado.

By October 13th, another in a series of upper level short
waves moving rapidly into the northwestern United States from
British Columbia caused the upper low center over the southwestern
United States to move slowly eastward. This approaching short wave
had associated with it a moderate polar maritime cold front, which

was located across central North Dakota and Montana on the morning

II C-742

PADIAAI corPORATICN

of the 13th: Precipitation was widespread across the middle of
the United States on the 13th, extending from New Mexico to the
Great Lakes in a very broad, nearly solid band. Skies cleared
over western Colorado on the 13th as the upper low was forced

eastward.

The short wave amplified rapidly on the 14th, causing
the cold front to move southward rapidly. The front passed through .
western Colorado during the morning of the 14th, causing cooler
temperatures and a continuance of clear skies. Precipitation once
again occurred in a broad band across the central part of the
United States because of the strong short wave and cold front.
The short wave and cold front continued to move eastward rapidly
on October 15th, thus forcing the precipitation area eastward with
it. A large upper ridge and surface high covered the western half
of the United States on the 15th, thus causing a continuance of
fair, dry conditions.in western Colorado on this day.

October 16th and 17th were very similar with regard to
the upper flow patterns which prevailed over North America on these
two days. A large surface high pressure cell dominated most of the
United States during the period. Precipitation was confined to the
eastern fourth of the country. A large upper ridge prevailed over
California, Nevada, Utah, Idaho, Wyoming, and Coiorado on these two
days, while a large amplitude upper trough extended from the Great
Lakes region to the Gulf of Mexico. Fair and mild weather prevailed
over western Colorado on these days.

The same basic meridional flow pattern persisted over the
United States on October 18th and 19th. A strong upper ridge
dominated the flow in the western United States on both days, with
a deep upper trough along the Atlantic seaboard. The systems pro-

gressed eastward very slowly, so that another long wave trough

reC-745

RADIAN COoRPORRTION

began to approach the Pacific northwest by October 19th. Pre-
cipitation was minimal across the United States on both the 18th
and 19th. A weak cold front progressed southward through the
eastern half of the nation on the 18th and 19th, but did not
affect Colorado at all. Meteorological conditions remained fair
and unseasonably warm throughout western Colorado on both of these

days.

The upper flow began to change on October 20th. The
upper ridge and trough progressed eastward slowly, but a strong
short wave began to dig southward along the west coast of the
United States. A cold front associated with the short wave
extended southward from eastern Washington into northwestern
Nevada and northern California. Precipitation was confined to
the northwestern and northeastern portions of the United States.

Fair and warm conditions continued in western Colorado.

The short wave in the Northwest continued its easterly
movement on October 21st, forming a closed upper low circulation
in the process. The polar maritime cold front continued its
eastward movement, passing through western Colorado during the
afternoon of the 2lst. Because of the upper low and its associated
moisture and positive vorticity advection, cloudiness and scattered
rainfall returned to western Colorado on this day. Actually, pre-
cipitation was scattered throughout the entire length of the
Rockies. Precipitation and considerable cloudiness continued in
western Colorado on October 22nd as the upper Low strengthened
Slightly and remained stationary over northern Nevada and northern
Utah. The upper flow became fairly zonal on this day, with the
jet stream located along the United States-Canada border. The
polar maritime cold front moved eastward through the northern
Plains States but did not advance southward because of the zonal

nature of the upper flow, the northern position of the jet stream,

II C-744

RADIAN corPorRarion

and a blocking high pressure cell in the southeastern United States.
Precipitation was widespread throughout the southwestern United
States on this day.

The upper level flow over northern Nevada strengthened
further by the morning of October 23rd, causing the broad area of
precipitation to persist over the Plateau region and southwestern
United States. Temperatures were cooler and cloudiness and pre-
cipitation were widespread throughout western Colorado on this day.
The zonal character of the upper level flow and the northward
retreat of the polar front jet stream into Canada caused the
maritime polar cold front through the central part of the United
States to become stationary. Precipitation was scattered along
this front from Texas to New York. Rains continued in western
Colorado during the morning of the 24th but began to diminish
in areal coverage later in the day as the upper low over northern
Nevada began to fill gradually. A short wave moving south from
Canada into the northern Great Plains brought with it a weak
cold front which extended into northern Wyoming during the morn-
ing. Precipitation was heavy in Texas and Oklahoma on this day.
Clearing took place in western Colorado during the night of the
24th as the cold front passed through the region and a high pres-
sure ridge built southward into the area.

The upper flow once again had meridicnal characteristics
by October 25th, although the flow was beginnirg to show splitting
tendencies once again in the western United States. An upper ridge
extended northward from Colorado through Montama and into Alberta,
Canada. A long wave trough extended southeastward from Hudson's
Bay into New England and a short wave and upper closed low came
onshore in the Pacific northwest. Precipitation occurred in
Wasnington and Oregon and through the center of the nation, along
a cold front which extended from Texas to the Great Lakes. Mild

temperatures and clear skies prevailed in western Colorado.

DY (C=745

P2ADIAM corRPORATION

Cloudiness returned to western Colorado as the short
wave moved eastward from the Pacific coast on the 26th. Pre-
cipitation was restricted to the Pacific Northwest, the Southwest,
and the Midwest as an upper ridge which extended from Florida to
Alberta, Canada brought fair weather to most of the nation. The
upper flow became split in the southwestern United States on
the 27th, as a cold pool of air at upper levels became cutoff
from the longwave circulation and formed a closed low over western
Arizona. This low caused scattered light precipitation throughout
the Southwest on this day. Cloudiness increased throughout western
Colorado as the day progressed and light precipitation was ex-

perienced in the area during the evening hours.

~ An approaching short wave from the Pacific caused this
upper low to be ejected northeastward by October 28th, resulting
-in continued cloudiness and scattered precipitation in western
Colorado. This approaching short wave caused the generation of
@ strong surface low pressure area (cyclogenesis) in Oregon, from
which trailed a polar maritime cold front into California. The
split flow characteristics and broad upper level troughing which
prevailed in the western two-thirds of the United States caused
this entire region of the nation to be covered by cloudiness and
precipitation.

The split flow in the polar front jet stream continued
on October 29th, with a strong upper low forming over Nevada.
A strong surface low was centered over western Utah during the
morning of the 29th, with a moderately strong maritime polar cold
front trailing southward. Cloudiness and precipitation continued
in western Colorado, as the storm produced the first widespread
snow of the season in the Intermountain Region. These cloudy and
snowy conditions persisted in western Colorado on October 30th,

as the upper low intensified and moved northeastward to a position

IL C=746

RADIAN corPcrRarTion

over central Utah. The surface low had meanwhile moved to eastern
Colorado and weakened somewhat. Cold frontal passage occurred late
on the 29th in western Colorado. By the morning of the 30th, it
was located on a line from eastern Colorado southward to western
Texas. Much of the nation received precipitation on this day due
to the amplitude of the upper level troughing over the western
United States.

Cloudiness and snows continued in western Colorado on
October 3lst as the intensifying upper low was pushed northeast-
ward by an approaching short wave just off the northwestern coast
of the United States. On the morning of the 31st, this upper low
was located over central Wyoming. The split in the upper flow
over the western United States continued, however, with a broad
upper trough continuing to affect the western two-thirds of the
United States. A surface low was located in Wyoming by the morn-
ing of the 3lst, while a maritime polar cold front extended from
Idaho into central California. Precipitation was widespread through-
- out the western and central portions of the nation.

B. Summary of Meteorological Conditions in the
Tract C-b Region

——— es

Precipitation totals and temperatures were near normal
in the Tract C-b region of western Colorado during the month of
October. The area experienced seven cold frontal passages during
the month. (October 3°55, 10,14, 209.24. "and 79). .Theistroncese
of these fronts was the one which passed through the region on
October 29th. Precipitation was experienced in the area on twelve
days of October (October ‘3, 5,10, G.822 23, 26°27, 28, 27942
31), but most of the daily totals were low. Snow was experienced
in the area of the Tract C-b on October 29th, 30th, and 3lst, but

TE a747

RZADIANM corrcoragrion

snow amounts were rather light and melting occurred within a few
days. Temperatures were below normal during the periods from
October 3rd through the 7th and October 11th through the 15th.
Temperatures were much below normal on October 29th, 30th, and
31st. Temperatures were above normal on the other days of the
month, but were much above normal during the period from October
17th through the 22nd. : ;

The area received 62 percent of the possible sunshine.
during the month. Sky coverage by cloudiness in the general area
totalled 5.3 out of a possible 10 during the period from sunrise
to sunset during October, and 4.9 out of a possible 10 for all
possible observations during the month. The region experienced
10 clear days, 9 partly cloudy days, and 12 cloudy days during
October. Thunderstorms were in the area on two October days
(October 10th and llth). Grand Junction, Colorado, about 75 miles
te the southwest of ‘the Tract C-b,;, meceived 72 anch of precipi ta—

tion during October, which is .21 inch below normal for the month.

Poor dispersion or air stagnation conditions occurred
occasionally in western Colorado during October. .The period dur-
ing which dispersion conditions were worst in the Tract C-b region
was from October 17th through the 20th. During this interval, the
region was influenced by a large persistent upper ridge over the
western portions of the United States. This ridge brought clear
skies to the Tract C-b area but also brought rather low mixing
heights and subsidence aloft. The weak surface anticyclone
associated with this upper ridge further compounded the problem
by causing very light surface winds throughout the area. The net
result was an extended (3 or 4 days) period of locally poor dis-

persion conditions.

The following is a summary of all air stagnation messages

fiom the National Weather Service pertaining to western Colorado

II C-748

Fe ADaIsaAzd corrPoRATION |

during the month of October. The messages were received in
Radian's facilities via the Service "C" Weather Teletype Circuit
from the National Weather Service, a cable service to which Radian
subscribes. These Air Stagnation Narratives are coded as "FKUS"

messages.

* October 2nd: “In the western United States,
the ridge moving through the Intermountain
Regions of the Rockies is supporting the
development of stagnation in portions of
Colorado, Arizona, New Mexico, and West
Texas...The stagnation will diminish as the

ridge moves eastward."

* October 9th: "The stagnation through the
Rockies this morning will diminish during
. the day as the trough moves into the

Intermountain Region."

* October 16th: “Deteriorating local disper-
sion conditions over much of the United
States west of the Rockies during the
next 24 hours.”

)’ October. 1/th: “Stagnation ‘conditions are
persisting over the western and south-
western United States as a result of little
movement of the upper ridge over the Pacific
Northwest and no movement of the flat sur-

face high pressure area."

Ii C-749

RADIAN corRPoORRTION

- October 19th: "Large-scale stagnation exists
over the western United States from extreme
West Texas through New Mexico to western
Montana. An ASA (Air Stagnation Advisory)

is in atfect for much of this area. i

C. Meteorological Discussion of. Tract. C-band
the Piceance Creek Valley

Meteorological conditions often varied considerably from
the Piceance Creek Valley to the Tract C-b itself during the month
of October. Anabatic and katabatic circulations were much better
organized in the valley at Trailers 020, 021, and 022 than on the
plateau at Trailers 023 and 024. Nighttime temperatures were much
-colder in the valley than on the plateau during nights when radia-
tional cooling occurred and the downslope flow became organized.
The diurnal range of temperatures was much greater at the Valley
Trailers (020, 021, and 022) because of the mountain and valley
circulations, with daily temperature ranges of 35° common at these
trailers during October.

Trailer 021 generally had the largest diurnal range of
temperature, mostly because of its location. At this location,
the katabatic winds were fairly light at night because of the
widening of the valley just upstream to the southeast. As a
result, the mixing of the air was diminished during the’night and
cold air from higher elevations was allowed to collect in this
relatively low area of the valley. Thus, radiational cooling was
allowed to proceed uninhibited and temperatures fell rapidly dur-
ing the night. Nighttime minimum temperatures were generally at
least 5°F colder at this trailer than at the other two trailers
in the valley and at least 10°F colder than minimum temperatures
at Trailer 023 on the plateau, where the katabatic circulation cell

was not developed so as to abet rapid cooling.

It C-/30

IRAADEAAM corPpoRaATION

On the majority of the nights in October, Trailer 021
had the lowest minimum temperatures, followed by 020, 022, and
023. Temperatures were higher at Trailers 020 and 022 during
the night because of increased wind speeds from the katabatic
circulation, which mixed the air near the surface to the extent

that the ground-based radiation inversions that formed near these

trailers were not so intense as the inversion (coldest at the lowest

level) at Trailer 021. During the afternoons, temperatures were
much more uniform at all trailers because of increased vertical
mixing from convection and the anabatic (upslope) flow. Daytime
maximum temperatures during October were generally highest at
Trailer 023, followed closely by Trailers 022, 021, and 020, in
that order.

Relative humidities were generally rather uniform in the
Piceance Creek Valley during the month, averaging about 62 percent.
Humidities were a little lower on the plateau (because of slightly
drier air and higher average temperatures), averaging about 53 per-
cent at the 30-foot level of the meteorological tower.

Winds were generally much lower in the valley than on
the plateau during the month. Winds generated by pressure gradient
forces were normally decreased in strength substantially from the
plateau to the valley. While the strongest winds during the month
were generally the result of synoptic-scale developments on the
plateau at the meteorological tower, the strongest winds in the
valley were often the result of katabatic or anabatic circulations.

Winds at Trailers 020, 021, and 022 exhibited marked
channelling effects because of the steep valley walls in the
vicinity. Winds at Trailer 022 were normally either east-southeast
or west-northwest while winds at Trailers 021 and 020 were normally
either northwesterly or southeasterly because of the katabatic-

anabatic circulation cycle. However, during transition periods

TI Gaol

BEDI corporarion

between upslope and downslope flow, or vice versa, the wind

direction was rather variable at these locations. In addition,
on occasions when the surface pressure gradient was weak and an
anabatic or katabatic circulation cell was not developed, the |

winds were often calm or variable in direction.

At Trailer 023, winds did not exhibit as much of a
terrain or micrometeorological dependence. Pressure gradient
forces for the most part controlled the wind directions and speeds
at the meteorological tower. Both the mode and mean of the dis-
tribution of wind directions at the tower were south-southwesterly
or southwesterly, depending on the level of the tower under con-
sideration, which is a reflection of the pressure gradient forces
which existed in the Tract C-b region during October. Winds
generally veered in direction (clockwise progression) and increased

in speed with increasing height at the meteorological tower.

Average temperatures in the monitoring network for the
month of October ranged from 39.4°F at Trailer 021 in the valley
to 47.3°F at the 30-foot level of the meteorological tower at
Trailer 023. The average temperature at Trailer 020 was 41.3°F,
two degrees higher than at Trailer 021. At the meteorological
tower, average temperatures were fairly uniform, ranging from
45.7°F at the 8-foot level to 47.3°F at the 30-foot level, with
the 100-foot and 200-foot levels registering intermediate values.
However, the average temperatures do not reflect the diurnal
variation of vertical temperature structure which occurred at
the tower. During cloudy, wet days, near-isothermal conditions
prevailed at the four tower levels. However, on clear or partly
cloudy days, the normal thermal pattern was: (1) inversion to
100 feet, with unstable lapse rates above that during the night,
and (2) unstable lapse rates to 100 feet with an inversion above

that during the day. The layer above 100 feet seems to have been

LI -C- 7352

ER.ADTAR corporation

decoupled from the layer below that level much of the time. How-
ever, during extremely windy or cloudy conditions, there was more
uniformity in the vertical temperature structure.

The highest daily average humidity reading in the valley
during October was 93.9 percent at Trailer 022 on October 29th.
October 5th also had average relative humidities above 80 percent.
Likewise, on the plateau, October 5th and 29th had the highest
average relative humidities. October lst and 2nd were the driest
days of the month, both in the valley and on the plateau, with
daily average humidities in the twenties.

The highest daily average temperature in the region for
October occurred on October lst. The average temperature this
day at the 30-foot level of the meteorological tower was 61.0°F.
Meanwhile, in the valley, the average temperatures ranged from
46.0°F to 48.1°F. The much lower average temperatures in the
valley were due to much lower temperatures from strong radiational

cooling during the night. The lowest daily average temperatures

in the network during October were recorded on October 30th, a snowy

day, when temperatures ranged from 27.6°F.to 29.9°F in the valley
and from 29.8°F to 31.0°F at the four meteorological tower levels.

The highest maximum temperature recorded in the valley during

October was 73°F at Trailers 020 and 021 on October 2nd. The highest

temperatures recorded at the meteorological tower during the month
occurred on October Ist, 2nd, and 15th. The lowest temperature re-
corded in the valley during October was 14°F at Trailer 021 on

October 15th. The lowest temperature recorded on the plateau was
24°F on October 30th.

Considering the valley stations, winds were strongest at
Trailer 022 during the month, averaging 5 miles per hour. Winds

at Trailer 021 averaged 3 miles per hour and winds at Trailer 020

ba ay Pet

Pes eo a or ae

: enemas. |

| pies |

Fe CARI AT coRrPpoRATION

averaged 2 miles per hour. The highest daily average winds
occurred on October 3rd and 21st. On a diurnal basis, the strongest
winds occurred from 1300 to 1500 hours at Trailer 020, from 1500

to 1800 hours at Trailer 021, and from 0100 hours to 0200 hours
(katabatic winds) at Trailer 022.

At the meteorological tower, wind speeds averaged 2 miles
per hour for the month at the 8-foot level, 7 miles per hour at the
30-foot level, 6 miles per hour at the 100-foot level, and 9 miles
per hour at the 200-foot level. The windiest days of the month on
the plateau were October 21st and 3lst. On a diurnal basis, winds
were strongest on the plateau during the period from 1300 to 1500
hours. Winds were lightest from 0800 to 0900 hours. The highest
5-minute average wind speed recorded in the valley during October
was 23 miles per hour at Trailer 021 on October 3rd. The highest
-5-minute average wind speed recorded at the meteorological tower
site during October was 35 miles per hour, at the 100-foot level,
on October 21st.

FRAUD EAAIN corrPoraricn

MONTHLY METEOROLOGICAL SUMMARY FOR NOVEMBER

A. Summary of the Major Features of the

General Circulation over North America

During the month of November, the general circulation
over the United States was fairly normal. That is, in general,
the various sections of the country did not experience prolonged
periods of abnormally extreme cold or heat. In addition, most’
sections of the nation did not deviate appreciably from monthly
precipitation norms. The long wave circulation in the upper
atmosphere generally alternated between periods of zonal and
meridional flow during the month. Split flow dominated the
upper flow from November lst through November 6th. Otherwise,
meridional or zonal flow regimes prevailed. Zonal flow, or
west-to-east flow which promotes rapid variations of a rather
weak nature in the meteorological conditions in a region,
occurred in the United States from November 7th through the
9th, the 16th through the 23rd, and on November 30th. Meri-
dional flow, or north-south flow which causes rather extreme
meteorological conditions (hot or cold, depending on relative
location in the circulation pattern) of a rather persistent
nature, existed from November 19th through the 15th and from
November 24th through the 29th. |

The results of these circulation patterns over the
various sections of the country during November were fairly
uniform. In general, much of the nation had temperatures which
were above normal for the month and monthly precipitation
totals which were also slightly above normal. Specifically,
the north central portion of the country, including the upper
Midwest and Ohio Valley, had temperatures and monthly precipi-
tation totals which were slightly above normal. The North-
east had near normal temperatures but below normal precipita-

tion. The Atlantic seaboard region had temperatures and

Pi C=755

ea.

2 2A 339 ee -

precipitation totals which were slightly above normal for the
month, while the South had near normal temperatures and slight-
ly above normal precipitation. The central portion of the
United States had above normal temperatures and slightly above
normal precipitation during the month. Meanwhile, the Rocky
Mountain region and Intermountain Region had slightly below
normal temperatures and precipitation totals which were slightly
above normal. The Southwest also had temperatures which averaged
slightly below normal, but had above average precipitation.
Finally, the West and Pacific coast areas had temperatures
which were much higher than monthly normals and precipitation
totals which were above normal.

No extremely cold Arctic air masses advected south of
the Canadian border during the month. The mean position of
the long wave trough over North America was through the west
central United States during November, while a weak mean ridge
was situated on a north-south line through the eastern portion
of the nation.

November began with a broad upper troughing pattern
over the western United States, with ridging over the Atlantic
seaboard. The split flow conditions caused one large upper
low pressure area over northeastern Wyoming and another over
northern California. A stationary front extended from the
Great Lakes to southern Texas and a cold front extended south-
ward from a surface low over eastern Nevada, Precipitation
was scattered throughout the western half of the nation and also
along the stationary front from Texas to Indiana. Skies were
overcast in western Colorado in the vicinity of Tract C-b on
the lst and rain and snow showers were widespread throughout

the area,

E2AADIAN corPornarion

November 2nd was much the same. The upper low in
Wyoming moved northeastward to the North Dakota-Canada border
and the upper low in the Southwest strengthened slightly and moved
southward to southern California. A surface high pressure region
began to build (anticyclogenesis) over the western portion of
the nation. The stationary front through Texas moved northward
as a warm front to a position along the Red River Valley, while
the low over Nevada moved to southern Arizona. Precipitation
was widespread across the western three-fourths of the nation.
Cloudiness decreased somewhat in western Colorado, but scattered
rainshowers still persisted in the region.

On November 3rd, the upper low in the Southwest
moved to northwestern Arizona and filled slightly. Meanwhile,
an upper ridge began to build into the Pacific Northwest.
A stationary front extended from the Great Lakes to southwestern
Texas. Precipitation, much of it heavy, covered the entire
midsection of the country. High pressure continued to build
into the western portion of the nation. Colder air advected
into western Colorado, with rain, snow, and fog persisting
throughout the area of the Tract C-b during the day.

The split flow regime continued on November 4th,
as the upper ridge in the Northwest continued to strengthen.
Weak upper lows were centered over western Kansas and western
Utah. A cold front extended from New York to a low over
Arkansas and then southwestward to southern Texas. Precipitation
was heavy in a broad band from southern Texas northeastward to
the Great Lakes, with many precipitation totals exceeding one
inch. Western Colorado continued under a moderate high pressure
regime at the surface, although a very weak surface low was
centered over southeastern Utah. Middle cloudiness and a few

light showers were scattered throughout the area of the Tract
C-b. .

ka C=¥S%

RADIAN corrcernarion

The split flow pattern began to break somewhat by
November 5th. A strong upper low was centered over Iowa and
a very weak upper low was over southwestern Utah. An upper
ridge extended from Oregon to Montana, A strong long wave
trough began to deepen at about 150°W longitude. At the sur-
face, a weak cold front extended southward from a low pressure
center over the Great Lakes to Alabama and then into the Gulf
of Mexico. An occluded front made its way onto the Washing-
ton coast. Precipitation was confined to the eastern third
of the nation and to the Pacific Northwest. Weak high pressure
at the surface covered the eastern two-thirds of the country.
Skies cleared in western Colorado with only a few scattered
middle clouds dotting the sky.

November 6th marked the end of the split flow regime
over the western portion of the United States as zonal flow
began to establish itself. Upper lows were centered over
Illinois and the Arizona-Utah border, while an upper ridge
extended from Nebraska to Minnesota. Precipitation occurred
in Texas, along the Gulf Coast, in the Northeast, and in the
Pacific Northwest. On the surface, the cold front moved off
the Atlantic coast, while the occlusion in the Northwest re-
mained essentially stationary. A weak surface high centered
in Kansas dominated the circulation throughout the nation.
Generally fair weather prevailed in western Colorado, with
some scattered middle cloudiness in the area during the

morning.

A zonal circulation prevailed on November 7th, with
a strong upper low in the East and a weak upper cyclonic
circulation centered in southern Colorado. A weak upper ridge
extended northward from Mississippi to Wisconsin. A short

wave moved onto the Pacific coast. A large weak anticyclone

[I C-/58

RADIAN corPorRaAricon

was over eastern Missouri at the surface. A maritime polar
cold front extended through Washington and a weak continental
polar front dropped southward into Montana. Precipitation ©
was widespread in the Pacific Northwest, Texas and its ad-
joining states, and in the Great Lakes region. Skies were
clear in western Colorado, with a very small high pressure
cell centered over central Colorado.

By November 8th, an upper level short wave had
advanced rapidly eastward to an Idaho-southerm California
line. Upper lows were located over Missouri and off the
Atlantic seaboard. A cold front extended southward from a

low in Alberta,Canada, to Nevada. Precipitation was widespread

throughout the Gulf coast states, Texas, and the Intermoun-
tain Region. The cold front passed through the Tract C-b
region around noon. Cloudiness increased during the day
and a steady rain began to fall during the evening.

The short wave moved eastward and dug southward
on November 9th as the upper circulation began to exhibit
some meridional flow characteristics. An upper ridge extended
from southeast Texas to an upper high over the Great Lakes,
while the upper trough was located on a Montana-Arizona axis.
A cold front extended through the northern Plains states and
another weak maritime polar cold front came onshore in Wash-
ington. Weak high pressure dominated the eastern half of the
nation. Precipitation occurred in Florida, the Pacific North-
west, and over a large section of the nation's midsection
extending from Texas to Minnesota and from eastern Utah to
Missouri. Cloudiness covered western Colorado during most of
the 9th and light rain fell during the morning hours.

The upper flow became meridional by November 10th,

as the long wave trough dug southward along a Montana-west

LisC-759

res

Lei,

be ee ee ee te he ee ee ee

Texas axis. Long wave ridges were located along the Pacific
and Atlantic coasts of the United States. The cold front
continued its eastern advance through the Midwest, extending
along a Minnesota-Central Texas line during the morning.

The cold front in the Northwest began to undergo frontolysis
(decay) because of decreasing upper level support. A warm
front moved northward from the Gulf of Mexico into south-
eastern Texas. Precipitation was scattered through the
Pacific Northwest end the Intermountain Region. Precipitation
was also concentrated along the cold front in a broad band
from Texas to the western Great Lakes. In westerm Colorado,
skies were overcast during the morning and some snow flurries
occurred, but skies began to break by the afternoon as high
pressure built into the area.

The meridional pattern amplified on the llth, with
a major trough through the center of the United States and
strong upper ridges in the West and East. A strong cold front
extended southward from a low over the westerm Great Lakes
region through the Mississippi Valley to a low in southern
Alabama, from which a cold front extended southward into the
Gulf of Mexico. Precipitation extended northward along this
front in a rather wide band. A large high pressure cell dominated
the western half of the nation, bringing clear skies and light
winds. Western Colorado likewise had clear skies and mild

temperatures on this day.

This meridional pattern changed little on November
12th. The long wave trough and western ridge retained their
amplitude and moved eastward slowly. High pressure continued
to dominate the western two-thirds of the country and precipi-
tation was confined to the Atlantic seaboard, Great Lakes,
aad Ohio Valley regions. However, a strong short wave began
to dig southeastward through the upper ridge in British

Columbia, portending a strong continental polar outbreak.

EY C-780

RADIAT corPporRaArion

Skies were generally fair (high cloudiness) and temperatures
were mild in the Tract C-b region.

The meridional long wave pattern amplified on the
13th as the short wave dug southeastward swiftly on the up-

stream side of the trough. Cold continental polar air streamed

southward down the lee side of the Rockies behind a cold front
extending from a low in Kansas to Colorado and then northwest-
ward to Washington. Precipitaion covered the northern
portions of the country. The cold front passed through the
Tract C-b region during the afternoon, lowering temperatures
slightly. Skies remained fair.

The meridional pattern continued on November 14th,

although the amplitude of the circulation was somewhat reduced.

An upper ridge dominated the West while a major trough covered
the eastern half of the nation with cloudiness and precipita-
tion. The continental polar cold front continued its south-
ward march, pushing into the Atlantic Ocean and Gulf of
Mexico by nightfall. A weak maritime polar cold front moved
into the Pacific Northwest. The moderate continental polar
cold front retreated eastward out of the Tract C-b region
during the day. Broken middle and high cloudiness advected
over the area throughout the day. Temperatures were mild.

The meridional circulation pattern of the five
preceding days began a transformation into a zonal flow
on the 15th, as the ridge in the West flattened and the
eastern trough began to lose amplitude. A weak cool front
extended westward from a small low pressure center in Wyoming.
High pressure covered most of the nation. Precipitation was

confined to the Northeast. Middle and high cloudiness covered

western Colorado as mild temperatures continued in that region.

i..G- 70d

TRADIAAI corRPoORATION

Zonal flow re-established itself over the United States on
November 16th. A short wave, located ona Minnesota-New
Mexico axis during the morning, moved through the center of
the nation, causing widespread precipitation throughout the
western half of the country. High pressure and light winds
covered most of the country. Mild, fair weather prevailed in
the vicinity of Tract C-b.

Zonal flow continued on the 17th as numerous short
waves progressed eastward across the country. Short waves
were located in the Ohio Valley (a rather strong system),
Texas, the northern Plains, and the Northwest. A weak con-
tinental polar cold front was in the northern Plains and a
maritime polar cold front moved eastward onto the Washington
coast on this day. Precipitation covered the easterm third
of the nation as well as the Pacific Northwest.

The short waves continued their eastward progression
on the 18th. The strongest of these waves was located in the
Northwest. The weak continental polar cold front in the north-
ern Plains remained fairly stationary, while the maritime polar
cold front progressed eastward to a Montana-central California
line. Precipitation was scattered through all areas of the
country except the Southwest. Cloudiness increased throughout
the day in westerm Colorado. The maritime polar cold front
passed through the Tract C-b during the evening, bringing
scattered showers and a few thundershowers tc the region.

The upper flow became a bit more organized on the
19th, with a long wave trough through the center of the United
States and minor ridges along the West and East coasts.

The maritime polar cold front extended southward from Minnesota

to Kansas and then curved into the Texas Panhandle and New

II C-762

ER SASS YAR CORPORATION

Mexico. High pressure began to build in the West behind the
front. Precipitation occurred throughout the eastern half
of the nation, in the Northwest, and in the Intermountain
Region. After some snow pellets during the early morning

in western Colorado, skies cleared gradually during the day,
becoming virtually clear during the evening.

The short wave trough moved eastward to a Minnesota-

Louisiana axis by November 20th as an upper ridge built
northward over the Intermountain Region. On the surface,

a cold front extended southward from a low over the Great
Lakes region to Louisiana and then to the southern tip of
Texas. A high pressure system, centered in western Colorado,
affected the western half of the United States with its
circulation. Precipitation amounts were large throughout
the eastern third of the country. The Pacific Northwest also
had precipitation. Skies were fair in western Colorado, but
temperatures were rather cool.

‘The short wave troughs and ridges continued their
eastward progression and by the 2lst, short wave troughs were
‘located off the Atlantic and Pacific coasts while a ridge
extended northward from Texas to North Dakote. A cold front
and low pressure system were located just off the coast of
northern California. Precipitation was confined to the
Northeast and the West. High pressure dominzeted most of
the nation. The Tract C-b region had mostly fair skies on
the 21st, with some scattered to broken middie and high
cloudiness over the area.

The zonal upper flow pattern continued its eastward
progression on the 22nd, as the Pacific short wave system
advanced inland to an Idaho-southern Califorria axis. The

maritime polar cold front associated with this short wave

It C-763

Ss SS Eo

ae |

RADIAN corrporarion

extended from southeastern Montana to southern California by
the morning of the 22nd. Another cold front, a continental
polar front, dipped into Montana and North Dakota from Canada.
Precipitation covered the western third of the nation and the
Northeast. Cloudiness increased throughout the day in western
Colorado and the cold front passed the Tract C-b region late
in the afternoon. A few scattered showers fell during the
evening.

The upper flow began to change from zonal to meri-
dional characteristics on the 23rd. A strong short wave
trough dug southward over the Intermountain Region on this
day while upper ridges built northward over the eastern and
western portions of the nation. On the surface, a maritime
polar front extended southward into Texas from a low in Kansas.
In addition, a relatively strong continental polar cold front
rushed southward through the central Plains states. High
pressure dominated the East and the West. Precipitation
fell in the Pacific Northwest, the Rockies, and throughout
the central portion of the nation. Some snow and rain fell
during the early morning in western Colorado, but skies cleared
during the late morning hours and remained clear for the rest
of the 23rd.

The upper circulation became meridional on the 24th
as the troughs and ridges amplified rapidly. Long wave ridges
were located along the Atlantic coast and in the western
United States while long wave troughs dug southward through
the central United States and near 140°W longitude. The mari-
time and continental polar cold fronts of the 23rd merged into
one cold front which extended from the Great Lakes to southern
Texas. A weak high pressure system dominated the western
half of the country. Precipitation on this day was confined
to the Pacific Northwest and along the length of the cold front.

II C-764

RADIAN corporarion

Western Colorado enjoyed fair skies and cool temperatures be-
cause of the high pressure system centered in northwestern
Colorado.

Meteorological systems moved rapidly on November 25th,
as the long wave trough through the central United States
moved eastward, as did the upstream ridge and trough. As a
result, a strong short wave pushed eastward to a position from
Washington to southern California by the morning of the 25th.
The surface maritime polar cold front accompanying this short
wave extended from Idaho to central California at this time
‘and was moving eastward rapidly. High pressure dominated the
central portion of the United States as precipitation was
confined to the Atlantic seaboard, the Northwest, and the
Pacific Northwest. Western Colorado remained fair throughout
the day, with some high cloudiness advecting over the area
during the morning. Skies were clear during the remainder
of the day. The maritime polar cold front passed through the
Tract C-b region during the evening of the 25th, lowering
temperatures somewhat.

The eastward progression of the long wave systems
continued on the 26th of November. Large amplitude troughs were
located in New England and on an Alberta, Canada, to Texas
axis, while sharp ridges extended from Missouri to Minnesota
and northward into Canada and also long the Pacific coast,
northward into British Columbia. A cold front extended
southward from Canada into Minnesota and from there into
Oklahoma, at which point it curved westward into New Mexico.
High pressure cells dominated the Ohio and Mississippi Valley
regions and also the western third of the country. Precipi-
tation was scattered throughout the northern third of the
nation. Clear skies and cool temperatures prevailed in the
Tract C-b area.

It C-765

Thee os RR Oa RE ORS

| imate: |

E25A DIAM corrPorRation

Short waves and upper level lows moving eastward in
the meridional long wave troughing pattern were the major
meteorological forces on November 27th. Upper lows were
centered just north of Maine, just north of Minnesota, and
in southern Washington on the morning of the 27th. One cold
front extended from the Great Lakes to Tennessee and southwest-
ward into central Texas on this day while another maritime
polar cold front extended from Oregon southwestward into
northern California. A weak high pressure system dominated
the Plains states and the Intermountain Region. Precipitation
was confined to the Great Lakes region, New England, and the
Pacific Northwest. High cloudiness increased throughout the
day in western Colorado in advance of the approaching upper
low and surface cold front. A middle overcast covered the
Tract C-b area by evening; temperatures remained cool.

Rapid changes took place on November 28th. The upper
low in Washington moved to a position over northern Utah and
strengthened, while the other two upper lows over North
America also strengthened but remained stationary. Meanwhile,
the upper ridge over the Pacific Northwest amplified dramatically,
which caused surface anticyclogenesis in southern Canada and
the northwestern portion of the United States. The development
of this large cold continental polar high cell caused a new
frontal system to form from the Texas Panhandle westward to
northern Arizona. Cold air streamed southward over the north-
western half of the United States. Precipitation, mainly in
the form of snow, occurred in the Great Lakes region and in
the central Rockies and Intermountain Region. Western Colorado
was cloudy throughout the 28th, with intermittent snow showers.
Rather cold air advected into the area during the day. Clearing

took place in western Colorado during the evening.

II C-766

Fe Zi D324 coRPORATION

The deep long wave trough and strong upper ridge
progressed eastward during the 29th as a transition to zonal
flow over the United States began. The upper trough extended

from Minnesota to New Mexico while the upper ridge extended
“northward from California to Alberta, Canada. The upper low
over Utah filled as the trough was propelled eastward. A
cold front extended from Tennessee to Arkansas and then into
southern Texas. A large cold high cell centered just north
of North Dakota dominated the weather over the western two-
thirds of the nation. Precipitation, much of it in the form
of snow, occurred from the Rockies eastward to the Mississippi
Valley and southward to the Gulf of Mexico, and snow flurries
occurred in the lee of the Great Lakes. Skies were clear
throughout the day in the Tract C-b region, but very cold air
continued to affect the area.

By November 30th, the upper circulation had changed
to a basically zonal pattern. An intense upper low was center-
ed over northern Missouri with a strong upper ridge over the
Intermountain Region. On the surface, a large, complex low
system was beginning to organize over the Southeast while a
strong ridge of high pressure extended from North Dakota to
southern Texas. Cold continental polar air and high pressures
dominated the western two-thirds of the United States. The
eastern half of the United States was covered by cloudiness
and precipitation. Snows occurred in the Rockies. Heavy snow
fell in Missouri, Illinois, and Iowa. Skies were fair through-
out the day in western Colorado but very cold air persisted in
the Tract C-b region.

II C-767

IRADIAAN corporation

B. Summary of Meteorological Statistics in
Western Colorado during November

The area of western Colorado in the vicinity of the
Tract C-b had below normal temperatures and above normal
precipitation during the month of November. The area ex-
perienced five cold frontal passages during November (Novem-
ber 6, 13, 18, 22, and 25). In addition, ‘the passace of an
upper trough on November 28th brought extremely cold air into
the region. Precipitation fell in the area on twelve separate
days of November (November 1, 2, 3, 4, 8, 9, 10, 18, 19, 22,
23, and 28). Of these precipitation occurrences, five involved
snowfall in the area of the Tract C-b (November 1, 3, 19, 23,
and 28).

In general, the first twelve days of November had
slightly below normal temperatures. From the 13th through the
26th, temperatures were generally near to slightly above normal.
From the 28th through the 30th of November, the Tract C-b
‘experienced temperatures well below normal.

The region experienced about 75 percent of the
possible insolution during the month. Cloud cover (all types,
but mostly high clouds) averaged 5.1 out of a possible 10
during the period from sunrise to sunset in the region and
4.5 out of a possible 10 for all 24-hour midnight to midnight
periods during the month. The area experienced a total of
twelve clear days, six partly cloudy days, and twelve cloudy
days during November. Thunderstorms were scattered over the
region on November 18th. Grand Junction, Colorado, about sixty
miles to the south-southwest of the Tract C-b, measured 1.18
inches of precipitation during November, which is .57 inches

above normal for the month.

[Il C-768

FADIAN corrporarTion

The following is a summary of all official FKUS
Air Stagnation Narratives issued by the National Weather
Service during November which pertain to the Tract C-b
region. These messages were received over the National
Weather Service's "C'' Service Teletype Circuit, to which Radian

subscribes via a terminal in its Austin facilities.

- November 7th: "Gradual flattening of the
upper ridge over the Southwest in conjunc-
tion with the surface high will result in
localized marginal dispersion over sections
of California, eastern Nevada, Utah, western
Colorado, Arizona and New Mexico today..."
"Localized dispersion problems due to weak
low level gradients through the interior
Southwest will improve rapidly after the

morning of November 8th..."

‘. November 13th: "The ridge over the Pacific
Northwest is forecast to weaken and be
forced southeast, spreading stagnation into
the Great Basin and Idaho tonight...stagna-
tion in the Great Basin will affect mainly

night and morning dispersion conditions."

* November 14th: "A short wave moving into
Colorado by Friday evening will cause weak-
ening of the ridge in the West..."

- November 22nd: "In the wake of the upper
trough moving out of the Rockies, computer-
ized upper level progs show some ridging

from California to Colorado by the morning

II C-769

| ec)

perenne

ELA DIAM corporarion

of the 24th. This, in conjunction with

the surface high and its associated light
low level winds, may result in some mar-
ginal dispersion conditions in the usually
susceptible areas in sections of California,
Nevada, Utah, and Colorado during the next
36 to 48 hours. Low mixing heights during
the late night and early morning hours will
also support this stagnation although trans-
port winds will generally be above the re-

quired minimums..."

IIT C-770

E2ZAISISAD corPoRarion

C. Discussion of the Meteorological
Conditions in the Monitoring
Network during November

Cold temperatures and periods of snowfall became
rather common in the ambient air monitoring network in and around
the Tract C-b during the month of November. Average tempera-
tures in the network ranged from 26.7°F at Trailers 020 and
021 in the Piceance Creek Valley to 33.3°F at the 200-foot
level of the meteorological tower at Trailer 023 on the Tract
C-b itself. Winds during the month were moderate in force on
the plateau around the meteorological tower and rather light
in the Piceance Creek Valley, where katabatic and anabatic

(downslope and upslope, respectively) circulation cells accounted

for much of the wind. Monthly average relative humidities

both on the plateau and in the valley ranged between 60 and
70 percent. Vector wind directions were southeasterly in the
Piceance Creek Valley where the flow is constrained by the.
valley walls and south-southwesterly on the plateau, where syn-
optic-scale pressure gradient forces normally control the
direction and speed of the wind.

The katabatic circulation cell continued to exert a
large influence on the meteorology of the Piceance Creek Valley
during November, althouth the anabatic, or upslope, circulation
cell which normally develops during the daylight hours was
almost non-existent during the month. The katabatic flow was
normally strongest, about 10 miles per hour sustained winds,
at Trailer 022 at the eastern end of the monitoring network in
the valley. The strongest drainage winds at this station
normally occurred from 0100 to 0500 hours in the morning.

When northwesterly gradient winds extended down into the valley,
they were normally strongest at Trailer 021, at the westem

end of the valley monitoring network.

IT G-774

cre 6

RADIAN corporation

Vector resultant winds for the valley stations during
the month were: 1.4 miles per hour from 138.6° at Trailer 020,
1.3 miles per hour from 123.2° at Trailer 021 and 3.2 miles
per hour from 108.9° at Trailer 022. The highest five-minute
average winds recorded during the month in the valley were 19
miles per hour at Trailer 020 on the 18th, 23 miles per hour
at Trailer 021 on the 28th, and 18 miles per hour at Trailer
O272-o6m the: 2/th... The highest daily average winds occurred on
November 28th.

Relative humidities were rather uniform in the Piceance
Creek Valley during the month. The monthly average relative
humidities ranged from 69.9% at Trailer 022 to 62.6% at
Trailer 021. Trailer 020 was intermediate with a 66% average
relative humidity. The highest daily average relative humidities

during the month occurred on November 21st.

Nighttime temperatures once again were coldest at
Trailer 021 during November, due to the light winds, dry air,
and strong radiational cooling which normally prevailed at this
site. The other valley sites also experienced strong radia-
tional cooling conditions, but not to the extent that they
developed at Trailer 021. On a clear night with light winds,
the air at Trailer 021 was normally 5 degrees colder during
the early morning hours than it was at Trailer 020, 10 degrees
colder than the air at Trailer 022, and 15 degrees or more
colder than the air on the plateau near the meteorological
tower. It can therefore be said that nighttime temperatures
on clear nights generally increased as one progressed eastward
up the Piceance Creek Valley. However, on nights when winds
were strong, skies were cloudy, and precipitation fell, the
streng radiational cooling did not develop and temperatures
were rather uniform throughout the monitoring network, from the

valley to the plateau.

IT C=772

RADPIAN corroratTion

Monthly average temperatures in the valley ranged from
26.7° at both Trailers 020 and 021 to 28.9° at Trailer 022.
The highest daily average temperatures in the valley during the
month occurred on November 22nd, while the lowest daily average
temperatures were experienced on November 29th. The highest
five-minute maximum temperature in the valley during November
was 54°F at Trailer 022 on November 21st. Daytime maximum
temperatures in the valley were generally highest at Trailer

022. The lowest temperatures recorded in the valley were
-17°F and -16°F, both occurring at Trailer 021, on November 29th

and 30th, respectively.

On the plateau, meteorological conditions were often
somewhat different from those in the Piceance Creek Valley.
The diurnal variations in temperature and wind direction
which were so prominent in the valley were not of as much
importance on the plateau. The diurnal range of temperatures
was much smaller within the Tract C-b itself because of three
factors: (1) the plateau was not affected by the katabatic
circulation cell to the extent that it affected the valley,
(2) radiational cooling conditions were not as strongly developed
on the plateau as they were in the valley, and (3) thermally
induced vertical mixing of the air during clear or partly

cloudy days resulted in rather uniform afternoon temperatures

throughout the monitoring network. The fifteen degree differences

in temperature which existed during the night were not present
during the day. During cloudy, windy, or wet conditions, how-
ever, the temperatures were approximately the same at any given
time, whether it was a meteorological tower level or a site in
the valley.

Winds were generally much stronger on the plateau than
they were in the valley. This can be attributed to the fact
that the synoptic-scale pressure gradient force winds which
affect the plateau seldom extend into the valley because of the

terrain constraints, ime Cower site, in particular; is often

Il C-773

PA PIAN corrornvrion

affected by very strong winds which are affected only mini-
mally by the terrain and its frictional dissipation forces.

The meteorological tower continued to monitor some
remarkable meteorological effects during November. On days
with light winds and little, if any, pressure gradient forces,
the winds varied considerably in direction with height and the
winds were normally strongest at the 100-foot level. On days
with strong south-southwesterly winds, the winds increased in
speed by about 25% from the 30-foot level to the 200-foot level
and generally veered in direction (progression in a clockwise
direction) by about 10 degrees from 30-feet to 200-feet.

When strong northerly winds prevailed, about a 20% increase

in speed from 30-feet to 200-feet occurred and the winds
generally backed in direction (counter-clockwise) with increas-
ing height. However, these phenomena are consistent with
meteorological rules.

When windy, cloudy, or rain/snow conditions existed,
temperatures generally varied little with height at the meteo-
rological tower, a Situation which is to be expected because
of the neutral stability conditions which prevail under such
conditions. However, on clear days or nights when winds were
fairly light, the lowest 100 feet of the surface boundary layer
on the plateau were often decoupled from the atmosphere above
it. That is, the ground-based radiation inversion generated
during the night often was confined to the lowest 100 feet,
with the temperature decreasing with height above that level.
Conversely, during the daytime hours on sunny days, the tem-
perature normally decreased with height up to the 100-foot
level. Above that height, however, an inversion layer some-
times existed. On such occasions, therefore, the mixing
depth over the meteorological tower site was only 100 feet.

This elevated inversion situation was not a common occurrence,

Il C-774

EF2.4'DIAM corPpornrion

but occurred often enough during November to merit some

mention.

The average vector resultant wind speed increased
with height at the meteorological tower. The resultant speed
was 3 miles per hour at 30-feet, 3.4 miles per hour at 100-feet,
and 4 miles per hour at 200-feet. The vector resultant wind
directions were 202.4 degrees at 30-feet, 189.9 degrees at 100-
feet, and 214.0 degrees at 200-feet. For purposes of comparison,
Trailer 024, about 1 mile north of the meteorological tower
site, had a vector resultant wind direction of 145.5 degrees
and a resultant speed of 1.1 miles per hour.

The highest daily average wind speeds on the plateau,
up to 18.6 miles per hour at the 200-foot level, were recorded
on November 18th, while the lowest daily average wind speeds
on the plateau occurred on November 9th. The highest five-
minute average wind speeds at the meteorological tower occurred
on November 25th.

The monthly average temperatures at the tower site
increased with height, ranging from 31.8°F at 8 feet (partially
because of radiational cooling effects) to 33.3°F at 200 feet.

The 30-foot level averaged 32.4°F and the 100-foot level averaged

33.1°F. The highest daily average temperatures during the
month, 41.2°F to LIEGE, occurred on November 21st. The coldest
‘daily average temperatures on the plateau were recorded on
November 29th, with the daily averages ranging from 13.6°F to
1523 Ey. The highest five-minute average temperature recorded

at the tower site during the month was 53°F at the 8-foot level
on the 21st. The lowest temperature recorded on the plateau
was 3°F, at both the 8- and 200-foot levels on the 29th.

LG aitS

RADIAN corroratrion

Relative humidities were fairly uniform over the
plateau during the month, averaging in the low 60's at all four
tower levels and at Trailer 024. November 3rd and 9th were the
most humid days of the month on the plateau, while the 21st was
the driest.

Solar radiation measurements showed a direct cor-
relation with cloud cover, atmospheric moisture, turbidity of
the air, and solar elevation during November. The highest
hourly totals of solar radiation received at the meteorological
tower during the month were 49.20 langleys from 1100 to 1200
hours on November 29th and 48.50 langleys from 1000 to 1100
hours on November 5th. .

[I C-776

E2ZAIDI 21 corrorarion

VI. DATA PRESENTATION AND SUMMARY

This section includes summaries for various recorded
data at the monitoring sites. The data presentations indicate
the variability of recorded concentrations and meteorological
parameters with location and time. In addition, correlation
of concentration with wind direction is shown. All data
channels except suspended particulates (24-hour samples) are
sampled once each second, but recorded as five-minute arithmetic
averages of the one-second samples. In some cases, the one-
second sampling rate is faster than the time required for the
instrument to process a sample; however, these instruments have
sample-and-hold circuits that retain the previous value until
updated. This averaging technique tends to smooth the recorded
parameters and reduce the effects of electronic noise inherent
in any electronic instruments.

The random noise is present both from the recording
instruments and quantization in the analog-to-digital conversion.
The lower threshold for all analytical instruments is twice the
maximum noise level generated by the instruments. This lower
threshold is 5 ppb for all instruments except the ozone analyzer,
for which it is 0.5 ppb. Any values appearing in the presenta-
tions that are less than the threshold indicate minimal levels
and should not be construed as absolute levels because of
recording system noise. In addition, averages of the random
noise tend toward zero, and any zero entries appearing in the
data presentations do not necessarily indicate absolute zero
concentration.

All pollutant data (except for particulate data) is

taken at the monitoring site in integer parts per billion (ppb)

but is presented here in micrograms per cubic meter (g/m*)

Pi? / 7

eae |

EQLFADIZAA CcorrPoraricon

assuming standard temperature and pressure of 25°C and 760 mmHg
(1013.2 millibars), respectively. The scale factors required
to convert ug/m* at standard conditions back to ppb for the
various pollutants are given in the following table.

POLLUTANT - TO CONVERT pg/m? At 25°C
AND 760 mmHg TO ppb MULTIPLY BY

It should also be noted that NO is measured as NO2. No
regulations presently exist for NO, and it can be oxidized to
NO. quite readily so it is more meaningful to report the NO2
equivalent of the NO. In addition, it permits simple subtrac-
tion of NO from NO, to obtain NO2. It also should be noted
that total hydrocarbons are measured as the equivalent methane

value.

II. C-778

FRA IZAADI corrPorarion

Table IV displays the quarterly statistics for
each monitoring station. All averages are arithmetic except

for suspended particulates which are geometric means, The
maximum average for various averaging times is also shown.

The averaging times are selected to provide comparison to
ambient air standards. It should also be pointed out that the
maximum l-hour SO, concentration is actually a thirty-minute
average. The 24-hour particulate "average" is actually one
sample taken from midnight to midnight, and the 3-hour hydro-
carbon average covers only 6:00 to 9:00 a.m. For averaging
times less than or equal to three hours, the sliding average is
stepped one five-minute sample at a time. For longer averaging
times the step size is twelve samples or one hour. For averaging
times less than or equal to one hour, 100 percent of the five-
Minute samples must be present to compute an average. Averaging
times greater than one hour require 90 percent. Whether or not
a sliding average is computed is solely determined by the
number of samples present in that averaging time.

Table V demonstrates the distribution of particulate
concentration. For each site, the number of recorded samples
occurring in each of fourteen classes is displayed. In addition,
the geometric mean of particulate samples at each site is shown.

Table VI presents daily averages for all of the baseline
gases that are monitored, and for total suspended particulates.
The averages are grouped by month and individual location. A
blank entry in this table indicates that less than 50 percent
of the five-minute samples were recorded for that particular
day. (Note: Particulate samples are 24-hour samples.) All

concentrations are in micrograms per cubic meter.

1G EM Gomes gi 8

Peele eR

| ere |

a we. |

ERCADIAAN corporation

To demonstrate the functional dependence of recorded
parameters upon wind direction, Table VII shows pollutant con-
centration displayed in a bi-variate distribution with wind
direction. The tables display the total number of five-minute
samples occurring in each concentration and wind speed class.
The mean concentration for all samples occurring in each wind
class are also shom. This distribution demonstrates the
dependence of high pollutant concentrations upon wind direction.

Table VIII, which depicts the stability wind roses for
September, October, and November, and the quarter covering those
three months, was generated by means of the STAR Program. An
inspection of the stability wind roses reveals that of the
Bix sstabilityzetassas. VAY. “BAe CY Db, 2 ee atid ete),
and "F" stabilities were rather common during the period,
while "A" stability occurred only rarely in the vicinity of
the Tract C-b. The STAR Program incorporates meteorological
techniques and methodologies developed by Dr. F. Pasquill and
D. Bruce Turner to produce a bi-variate frequency distribution
of six wind speed classes and sixteen wind direction sectors

as a function of six separate stability classes.

The wind speed classes in this Pasquill formulation
correspond to the first six wind speed (or force) categories
of the commonly used Beaufort Wind Scale, which was devised by
Admiral Beaufort of the British Navy in the early nineteenth
century. The wind speed classes in these tables are constructed
using knots (1.16 miles per hour) as the unit of measurement.
The sixteen wind direction classifications are referenced
to true north, with each direction representing a 22% degree
sector of the full 360 degree circle.

II C-780

RADIZAN corporarion

The wind direction and wind speed measurements
used in this stability wind rose distribution were obtained
from the 100-foot measurement level of the meteorological
tower (Trailer 023) on the Tract C-b. The tower wind data
was used in preference to wind data from the valley stations
or other meteorological sources because that area of the
plateau was deemed to experience wind flows which were most
applicable to the points of interest in pollutant modelling;
terrain factors were also of less importance in the wind
speeds and directions experienced at this location, so that
synoptic-scale meteorological features exerted a larger
influence on the flow. The 100-foot level wind data was used
because the wind instruments at this level had more "up"
time over the quarter under consideration here. The wind data
at the 100-foot level may differ slightly from that at the
30-foot level or the 200-foot level (mainly because of the
variability of wind direction with height during periods
of light and variable winds and the general increase of wind
speed with height which accompanies gradient winds that
exceed 7 or 8 knots), but the differences will not affect the
stability wind roses appreciably. Therefore, the wind data
used here should be considered to be highly representative
of the plateau region.

The radiation data which made up the other half of
the data input to the STAR Program was obtained from cloud
cover and ceiling data from the Grand Junction, Colorado,
National Weather Service Office. The inputs which combine
to determine the radiation index using STAR Program methods
are: (1) cloud cover in tenths, (2) cloud height above the
ground if a ceiling exists, and (3) solar elevetion (or time
of day for nighttime applications). The cloud data from
Grand Junction was used because it was deemed to be the most
representative data available in the area of the Tract C-b

(approximately 60 miles to the south-southwest). Moreover,

Et G-78)

Keg |: SRS |

| FRADIAT CORPORATION

since the majority of the cloudiness in this area during the
quarter was of the middle and/or high varieties, which are nor-
mally uniform in their coverage characteristics and heights
over a region while at the same time extending over a large
area (a synoptic-scale feature) during their occurrence, the
-use of Grand Junction cloud data is deemed to be meteorologically
sound. Periods of clear skies should also be uniform in
spatial and temporal extent in the Grand Junction - Tract C-b
expanse. Some slight variances in cloud coverage amounts

could have occurred during periods of iocal storms, low
cloudiness, or terrain-induced cloudiness and fog. However,
there was probably only a minimal number of such occurrences,
so that the stability wind roses are applicable to the Tract
C-b region.

This method of radiation index determination (use of
cloud cover data from Grand Junction) was chosen over the pyra-
nometer data recorded on-site because the pyranometer data was
not available for the entire quarter. Radian recommends the
use of pyranometer data for daytime hours, and the change in
temperature versus height (lapse rate from met tower) for night-
time to determine the radiation index. This method will be used

in future reports.

II C-7/82

— ——
-_——— -

EOEAIDILANM corporaArion

_BEAUFORT WIND SCALE FOR OBSERVATIONS AT LAND STATIONS

Correspondinz Limits of Wind Speed

Explanatory at 10 meters zb. erd. 5
Title ~ ” Specification for Use $$ ——<_———
ea : 3 Mi/hr. ICnots Km/hr. M /szc- Fefecc. i
0 Calntazciece as sisce Smolce rises vertically... ..cecee cee eee 2. <i <1 <1 Ga: < 1 ,
1 LwhQait.ose-seo- Direction of wiad shown by smoxe drift, r .
but not by wind vanes....- Fes wttte 1-3 3-3 1-5 0.3-1.5 1-5
2 Light breeze....--| Wind felt oa face: Icaves rustle; orcinary
; ; vane moved by wind 5.0526 22-0006 s00 4-7 4-6 6-31 1.6-3.3 6-11
3 | Gentle breeze..... Leaves and small twigs in constant mo- :
tion; wind extends Echt flag........-. §-12 7-10 12-19 3.4-5.4 12-1S
4 |} Moderate breeze..-| Raises dust and loose paper; small bran- :
. ; ches are moved!so csc sce-s s- cewee- see 13-15 11-16 20-28 5.5-7.9 19-26
S | Fresh breeze.....- Small trees in leaf begin to sway; wave- . “
Batis lets forn:cd oa intand waters.......--- 19-24 17-21 29-38 §.0-10.7 27-35
G | Strong breeze:2... Large branchesiu motion; whistling heard
in telegraph wires; umbrellas uscd with sat
Ciewll ys oo es esata = Smee = ee 25-31 22-27 3949 10.8-13.8 36-45
7 (| Wigh wind........] Whole trees fe motion; inconvenience felt
when walking against wind. .........- 32-38 28-33 50-61 13.9-17.1 46-56
Fresh gales. Preaks twigs of trees: generally impedes “
g PIORKCSS. o.- Sowciand cases oes + oanceies 39-46 34-40 62-75 17.2-20.7 57-5
Strong paleo... - “Slight stractural damage eccurs (chimney . .
pots aml Slates cea Oved) aso. scaw ssc 47-S4 41-47 75-85 20.8-24.4 69-E3
10 Whole pale... --...] Scidom expericzced inland; trees uprosted ;
j considerable structural damage occurs... 55-63 48-S5 S9-102 2:1.5-28.4 1-95
11 Storntiocses secs - Very rarely experizaced; acco:npanicd by .
widespread aimeseciGe sas Se. oo na oe 64-72 56-63 103-117 28.8-32.6 94-50%
32 Vurricaneieameen~ 2incass0s cee eneeeee woe ese Se wes watens bert VSre2 61-71 118-133 32.7-36.9 107-323"
3 [acweco kt Meeks] 1 eon e ree te pemnc cm areas 3-92 72-0 134-149 | 37.0-41.4 | 122-125
ON Lee riScid OL oC CLIO BOCe islets aiainia aiaiaiaie aiaiaiete HbdlecogopoIS G06 93-102 &1-S9 150-106 41.5-46.1 \37-15%:
DSi Dra te At 8) Ee Ao One COG OOS Oat 105-}14 99-99 167-183 45.2-S0.9 $52-105
HG Fle cis sleeteicieete ee Nall) starslate os eictalais oi e'cle's aie) e1otstetetel oleininiaininieieiele 31S-125 100-108 1£4-201 $1.0-S6.0 167-i=3
YM MOOR nc Oe OR ee ean cet er eee: 126-136 1 309-118 | 202-220 1 56.1-61.2 $i-253
Source: Table 36(p. 119) in RJ. List (£951); Smithsonian Meteorotogical Tables; Smithsonian Miscell. Coll. Vol. 11-4. ‘

Table IX demonstrates the diurnal variation of various
recorded parameters. Hourly averages are determined by arithmeti-
cally averaging five-minute samples, except for wind direction
averages which are computed vectorially assuming unit vector
magnitudes. Totals in the diurnal wind direction tables are i
vector averages of the columns and rows. For all parameters, .
a blank entry in the diurnal variation table indicates that less
than half (i.e., less than 6) of the five-minute samples for
that hour are present. |

1

BL C=283

FASIAN corporation

Times given in the data presentation are Mountain Day-
light Saving Time until toward the end of the month of October when
the computer clocks were manually reset to Mountain Standard: Time.
When the computer clocks were set back one hour, one hour's worth

of data was overwritten.

To facilitate comparison of recorded concentrations to

ambient air quality standards, the following regulations are

presented.

II C-784

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TABLE V

SEPTEMBER 1974 - NOVEMBER 1974
C-b SHALE OIL MONITORING PROJECT

SITE 020 021 022 023 024

CONCENTRATION
ug/m?
>260
240-260
220-240
200-220
180-200
160-180
140-160
120-140
100-120
80-100
60- 80
40- 60
20- 40

(eo) loy fo Noy te)
way
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<7) ply E 14

TOTAL iz 18 7 9

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Ei ¢-791

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TABLE VII

FUNCTIONAL DEPENDENCE OF RECORDED
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NIURNAL VARIATION OF . fon NIOXIDE (UG/He#5)

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28

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PERIONCLL/ 1/74 TO 11/30/74)

- 21

TRAILER NO,

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24 MEAN

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Pie L091

D2EAIDIAAM corporntrion

Particulate loadings at the Tract C-b monitoring

' stations are determined daily by use of Hi-Vol filters. The

standard fiberglass filters are used for routine sampling.
Supplementary filters are taken every sixth day at Trailer 023
to permit actual chemical analysis of the particulate matter.
Special low background cellulose filters are used for this

purpose.
Two types of samples are taken:

1. <A quarterly composite to determine
average concentrations.

2. A spot sample to detect any gross
short-term variations from the

average.

Half of each filter is retained to permit detailed
examination if any unforeseen problems or high levels occur.
The filters are analyzed for trace elements using a spark source ©
mass spectrometry survey scan and for gross a and 8 radioactivity.

the results Dor theypast quarter ‘are. attached: ‘The
levels reported are quite low with no problems evident. Units
reported are ppm for the trace elements and pCi/gm for radio-

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ALR No.:

Sample ID Number:

Uranium
Thorium
Bismuth
Lead
Thallium

-- Mercury
Gold

Platinum
Iridium
Osmium
Rhenium
Tungsten
Tantalum
Lafnium

Lutecium

Ytterbium ~

Thallium
Exbium

Holmium

Dysprosium

—_—

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185-1631-5 (Composite of 1, 2, 3, 5)
'% of filter #0001, #0002, #0003, #0005

Concentrations in parts per million by weight

Terbium

Gadolinium

Europium
Samarium
Neodymium

Praseodymium

Cerium
Lanthanum
Barium
Cesium
LTodine
Tellurium
Antimony
Tin
Indium
Cadmium
Silver
Palladium
Rhodium

14
10
4.7
oe
39
pe

se

2.0%

Ruthenium

Molybdenum 8.6

Niobium
Zirconium
YEtCriwaM
Strontium
Rubidium
Bromine
Selenium
Arsenic
Germanium
Gallium

Zine

|Copper

Nickel

1 CobaLle

Iron
Manganese

Chromium

ese
9.2
‘oat

Vanadium
Titanium
Scandium
Calcium
Potassium
Chlorine
Sulphur

Phosphorus

Silicon
Aluminum
Magnesium
Sodium
Fluorine
Oxygen
Nitrogen
Carbon
Boron
Beryllium
Lithium

NOTES: NR - Not Reported; blanks indicate below detectable limits.
Total Loaded Area,

Total Particle Loading - 0.0547 grams

(average weight for complete filters)

Oe ou

C-1094

F2 2A000(AN CoRPeRATION

Gx w.: 185-1631-5-4 |
' Sample ID Number: Zrofiiter FO004 ~~. T.*

Concentrations in parts per million by weight

“

Uranium Terbium Ruthenium : Vanadium 76

Poe
3 Thorium 175 Gadolinium Molybdenum 23 Titanium 430
: ; Bismuth | 1.6 | Evropiun — Niobium 4.5 Scandium
rs - Lead 480 Samarium |Zirconium 52 Calcium 54,000
| phalliun — Neodymium 4.6 |Yttrium . 8.4 | Potassium 32,000
Mercury <7 | Praseodymium 3.3 Strontium 300 © Chlorine 130
Gold Cerium © 24° ~_|Rubidium 180 | Sulphur —-3600
Platinum. Lanthanum 9.2 Bromine 5 Hebe Phosphorus 230
BR Iridium | Bapiun ©). 420) [Selenium 03-8. |"Silzeqm a
Osmium Cesium | 6.1 . |Arsenic 34. -| Aluminum 8100
en Lodine ~ “\Germanium =~ Maznesium 23,000
| Tungsten 1.6 | Tellurium 2.0. jGallium 2°28 Sodium 2800
r Tantalum | | Antimony Soh Zine 1200| Fluorine 210
Hafniun Tin “88° |Copper 880 | Oxygen NR
fs eetecium Indium ” weckel Mien Nitrogen NR
Ytterbium Cadmium | 0.04 {Cobalt 19° | Carbon NR
|; Thallium Silver 6.5 |Iron 3600] Boron 400
} Erbium | Palladium Manganese 610 Beryllium Ome
Holmium Rhodium m 94 m 14

Chromium — Lithium

Dysprosium

NOTES:. NR - Not Reported; blanks indicate below detectable limits.
Total Loaded Area, 262 ein? Bysgt the “ie a oe ;

Total Particle Loading - 0.0421 grams
oe (total exposed area - 420 cm?)

18 ae