ML17261A180
| ML17261A180 | |
| Person / Time | |
|---|---|
| Site: | Ginna  |
| Issue date: | 06/07/1974 |
| From: | YORK WASTEWATER CONSULTANTS, INC. |
| To: | |
| Shared Package | |
| ML17261A179 | List: |
| References | |
| TASK-02-02.B, TASK-2-2.B, TASK-RR NUDOCS 8004150462 | |
| Download: ML17261A180 (173) | |
Text
REPORT NO.
Y-8186 PAGE UPPER AIR METEOROLOGICAL STUDY FOR JL~f'l 1'01 74 PlA ROCHESTER GAS R ELECTRIC CO.
ROCHESTER, NEN YORK PREPARED BY:
YORK RESEARCH CORPORATION ONE RESEARCH DRIVE
- STAMFORD, CONNECTICUT 06906 June 7, 1970 yORK RESEARCH C ORPORATION
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STAMFORD, COYNECTICUT
REPORT NO.
Y-8186 PAGE TABLE OF CONTENTS LAUNCH SITES EXPLANATXON OF FIGURES TEST PERIOD WEATHER CONDXTXONS GEOSTROPHIC MINDS TEST RESULTS June 23-June 29, 1973 August'0-August 16, 1973 October ll-October lS, 1973 March ll-March lS, 197.0 April 23-April 28, 1974 BUFFALO SOUNDING CORRELATION DATA LOG LXST OF FIGURES SUÃ'SRY FIGURES PAGE 5
6 6
7 10 13 JUv. i3 l974 YQLuC RESEARCH CQRPQB,AT/QN
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s STAMFORD, CONNECT1 UT
REPORT NO.
Y-8186 PAGE 1
Launch Sites The two'ocations at which launches have been made, for this
- study, are the Sterling, New York environs and the.Ginna Generating Station.
Two sites have been used at Ginna but several sites have been used at Sterling.
At Ginna, all the launches were made in a large field approx-imately 2,000 feet to the west-northwest of the station build-ings, within 900 feet of the lake itself.
Host of the Stexling launches were made from a large field just to the southeast of the pxoposed fossil plant site about 1,500 feet from shore.
The following list specifies the launch and tracking sites used in the Sterling area 'where the letters correspond to the sites denoted on the maps.
(Figures 1 a-d)
A ~
B ~
Sterling Area Sites Denotes "Sterling Fossil Site" launch site "Sterling Met Tower'! launch site C.
"Irwin Road" launch site D.
E.
F.
G.
H.
K.
L.
NacNeil Road" laun'ch Site Denotes Tracking site "Barker Road" used on.4/25/70 Launch site at 90.2'zimuth from "Barkex Road" Launch site at 275.2'zimuth from "Barker Road" Denotes "Sidmans Hill"Tracking site used on 0/26/74 Launch site at 158.0'zimuth from "Sidmans Hill" Launch site at 247.0'zimuth from "Sidmans Hill" Denotes "Snake Swamp" Tracking site used on 4/27/74 Denotes "Southwest Oswego" Tracking site used on 0/27/74 YORK RESEARCH CORPORATION
REPORT NO.
Y-8186 PAGE.
2 EXPLANATION OF FIGURES V
The site location maps are from the Oswego New York Quadrangle published by the U.
S. Department of the Interior.
This map uses a 20 foot contour interval with a scale of 1" = 5000 feet.
Neather maps presented here are the 0700 EST maps published in the Daily Neather Map Series.
They are used. here only to illustrate the prevailing conditions on the day of launch, so the test results can be compared. to what would have been ex-pected, to occur from the synoptic patterns.
The balloon plots are computer generated plots of the output of York Research Corporation's pilot balloon and balloon sonde computer analysis.,programs.
The temperature and dew point plot is a delta from the surface temperature and dew point (plotted as
- 0) vs. height in meters.
The horizontal velocity plot is a trace of horizontal wind.
speed.
(in meters/sec.)
vs. height =in meters.
The vertical velocity trace is a delta from an average plot of meters/sec.
vs. height in meters.
The polar plots are plots of the horiz-ontal trajectory of the balloon determined. by positions cal-culated every 15 seconds.
'I The separate balloon sonde plots of 0/25-0/27 are traces of temperature in degrees (F) vs. height in feet.
The wind. in-dicators are the same as. those used on standard. weather maps.
TEST PERIOD NEAT1IER CONDITIONS Geostrophic wind computations have be'en made from pressure data reported at 0700 EST.
The grid. used.
was Buffalo and Albany for the East-Nest pressure difference, and. Montreal and. Avoca for the North-South pressure difference.
This large pressure grid.
was used. to eliminate any local effects on the pressures re-ported. by stations closer to Lake Ontario.
Table I lists the geostrophic winds for each test day, with the wind. speed in meters/sec.
The effect of geostrophic wind. as well as the prevailing weather conditions in the area of the site on each test day is described In the test results.
YORK RESEARCH CORPORATION
+2~
STAMFORD, CONNEC-,ICUT
REPORT QO.
y 8186 I
PAGE 3
TA3LE l.
Geoatro hie Nind 6/23/73 6/24/73 6/25/73 6/26/73 6/27/73 6/29/73 8/10/73 8jll/73 8/12 /73 8jl3/73 8/14/73 8/l6/73 270 Q 207 N 232 N 200 5 204 N 189 5
'78 5 290 P>
299 N 322 8 207 5 023 5 4.2 2.5 1.4 8.7 i2.9.
6.7 7.1 8o2 9.2 10.0 3lo9 10/11/73 10/l2/73
'01>3
/73 10/15/73 181 5 8.4 233 8 8.1 260 C< 13.4 311 N 18.5 3/11/74 3/12/74 3/13/74 3/14/74 3/l5/74
. 4/23/74 4/24/74 4/25/74 4/26/74 4/27/74 4/28/74 312 C 085 C<
353 9 348 N 225' 323 N 020 C~
011 C 334 C 257 5 2S4 5 7oG 7.5 21.7 18.4 4+2 12.6 14.1 2eS 11.5 13.5 Your: Rsssan.cH Con.boa.wrroN STAMPORD. COYYtiCT1CUT I
I
~PORT NO Y-8186 t
PAGE TEST RESULTS e
The results have been separated into the five test periods:
6/23/73-6/29/73, 8/10/73-8/16/73, 10/ll/73-10/15/73, 3/ll/70-3/15/74 and 4/23/74-0/28/7Q.
The daily weather maps are pre-sented first'nd. then the balloon plots for that test period..
The balloon plots have not been given figure numb'ers since they have all been assigned.
specific run ID numbers.
NOTE:
The computer generated.
balloon plots are arranged'n chronological order, NOT in order of the Run ID.
June 23 - June 29 1973 On June 23, as shown on Figure 2a, the pressure gradient over
.the Northeast was -small with light winds reported from a west-
- erly, 4 meter/sec.,
geostrophic wind..
The weather was hot and sunny with a few afternoon thunderstorms in the area.
Run ID's 7
and.
8 show 'Nest Northwesterly onshore flow at the surface with a sharp turn at 260 meters.
~ Prom Figure 2b the pressure gradient over the 'Northeast on June 24 was very small xesulting in light'inds reported from a South-Southwesterly, 2.5 met'er/sec.
geostrophic wind. and the sky was mostly clear all day.
Run 410 shows simply a Nest Southwest flow to 700 meters, but Runs 11-13 show the flow at the surface to be Northwesterly turning to Southwest at'round.
300 meters.
Run Nll shows a distinct Northerly wind at the surface which backs with altitude to Southwesterly (the vertical extent of the onshore Northerly winds is 200 meters).
The horizontal velocity is also a minimum at the turn with a maximum in the onshore flow (indicating a lake.breeze circulation).
Runs 15 and. 16 no longer exhibit this Northerly surface wind.
From Figure 2c the gradient over the Northeast is very small on June 25 producing the weakest geostrophic winds of any test day, Southwest at 1.<~ m/s, (a necessity for a strong lake breeze pattern).
Run
=.".18 displays a very distinct offshore flow at the surface (Southeast winds) up to 170 meters.
The wind from 200 to 900 meters slowly backs from the Northwesterly return flow to the Southwest flow aloft.
Runs 19-21 illustrate the strengthen-ing and deepening of the lake breeze circulation with time under clear skies (note the horizontal speeds a maximum at the ground and increasing with time).
Run
-".1 is the,1050 EST balloon sonde.
The plot shoiis a 100 meter isothermal layer above the surface which corresponds to the Northerly onshore surface winds.
As the winds veer with altitwide the velocity decreases and the lapse rate oscillates between stable and unstable.
At 600 meters when YORE: RESEARCH CORPOB.ATIO~
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STAMFORD, CON+EC11CUT
REPORT NO.
Y-8186 PAGE 5
the winds become Southerly, the temperature again becomes isothermal in this return flow aloft.
The total height of this circulation was 500-600 meters before the balloon accel-erates into the Southwesterly flow aloft.
On June 26, launches were made from the Ginna Station under the conditions shown in Figure 2d with a geostrophic wind of South at 8.7 meters/'sec..
Runs 22-25 show basically Southerly winds throughout the flight with little turning.
Figure 2e shows the gradient causing the strong geostrophic winds on June 27, (SSN at 13 m/s).
Overcast and. raining, Runs 26-27 taken between rain showers show no turning with altitude.
On June 29, Figure 2f shows the conditions yield-ing a South at 7 m/s geostrophic wind.
Run 28 looks much the
~ same as Runs 26 and. 27.
Au st 10 - Au st 16 1973 Figuxe 3a illustrates the conditions on August 10.,
a Nest geu-strophic wind at 7 m/s.
Runs 2, 29, 30, 3
show winds basically fxom the Southwest with the winds on Run 4 more Southerly.
The temperature profile of Run 2 shows an inversion to 200 meters and. adiabatic above..
The temperature plots of Runs 3 and 4
show mexely an adiabatic lapse rate to 700 meters.
With a Nest geostrophic wind at 8 m/s, Runs 5, 6, and 32 show winds becoming Westerly with height from the Southwest.
The temperature plot of Run 5 shows no inversion present.
The temperature plot of Run 6 has an isothermal layer between 80 and.
220 meters, but Run 32 has no inversion, in fact the lapse near the surface is unstable.
August 12 was mostly clear but the geostrophic wind. was Nest at 9 m/s..
The winds at the surface of Run 33 are SN during the inversion layer in the temperature plot to 200 meters.
Above this inversion the wind becomes Westerly.
The winds of Runs 34 and 35 are INN from the surface with little turning.
On August 1'4 launches were made at Ginna under the conditions of Figure 3d with a South geostrophic wind at 4 rois..
Run 37 shows a strong ground inversion up to 320 meters.
This alti-tude corresponds to the. altitude where the winds turn'rom
'ORK RESEARCH CORPORATION
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sTAMFoRD, coNNEcTIcUT
REPORT NO.
Y-8186 PAGE 6
5N to southerly-Runs 38-43 illustrate winds that are south-woutheasterly with little turning with height.
" Run 42 shows 8 slightly unstable atmosphere up to 400 meters.
On August 16th, Figure 3f shows a high over the Great Lakes with a computed geostx'ophic wind of NNE at 2 m/s.
Run 44 shows a sharp shallow inversion with a neutral lapse above.
Run 46, inland, shows a similar temperature pxofile to Run 47 taken at the Fossil site.
October ll - October 15 On October ll R 12 the geostrophic winds wexe south at 8 m/s and southwest at 8 m/s respectively (Figures 4a K b)
~
The winds on both days did approach SN as the altitude increased.
Run 49 shows an invexsion up to 300 meters and isothermal above.
Runs 50, 52 R 54 show isothermal layers to 1000 m.,
600 m., and 670 m respectively.
Run 54 shows the only case where any condition existed on any. run that approached a lid due to a strong inversion aloft.
On October 13 with a west at 13 m/s geostrophic wind, a shallow inversion developed on Run SS up to 200 meters (the height also of the southerly winds at the surface before the turn to west-erly).
Strong winds in Runs 56-S9 correspond to a mostly neu-txal atmosphere for the rest of the day.
A 19 meter/sec.
northwesterly geostrophic wind completely dominated the flow on October 15.
Run 60 shows a weak inversion up to 400 meters with isothermal conditions above.
Runs 62 R
64 show neutral and isotherman atmospheres up to 1200 meters respectively.
March ll - March 15 1974 The conditions of the March test period were strong winds and cold temperatuxes on all five days.
The temperature profiles are therefoxe difficult to interpret since the lake was warmer than the land and the air flow during these runs, so air coming off the water would be unstable due to warming from below over the lake and cooling from below over the land.
YORK RESEARCH CQRPQRATIQN
~ '
STAMFORD, CONNECTICUT
REPORT NO.
Y-8186 I
I PAGE On Harch 13, the strongest geostrophic winds for any test day
- occurred, North at 22 m/sec.
Launches were made at the Ginna Station under mostly clear skies.
The Runs (71-.74) show strong Northwest winds with mostly neutral lapse xates up to 1000.
meters.
Run 75 at 0830 on March ll shows a sharp ground inversion to 120 meters and an unstable layer above.
This may be a result of gxound cooling as unstable lake air moves over the cold
- land, an effect that is the exact opposite of the TXBL des-cribed hy Lyons on. Lake Michigan.
A ril 23 - A ril 28 1974 The April test period was an intensive test pexiod to determine if a TXBL exists in onshore gradient and onshore lake bxeeze Slow.
After overcast and rain on April 23 and 20, the skies cleared and onshoxe gradient flow occurred on April 25 and 26 (geostrophic North at 3 m/s and Northwest at 12 m/sec., res-pectively) and the synoptic flow decreased enough to produce a lake bxeeze circulation on April 27, (geostrophic Nest at 0 m/sec.)
Run 86 on 0/25 shows an inversion to 300 meters corresponding to the westerly wind at the surface before the veering to northerly winds in the upper'flow.
The track site was then moved to Barker Road ("E" on Pigux'e lb) and launches were made from site F, then site G, and then site F again.
Figures 7a and h represent large scale plots 'of the temperature data Sor sites P and G respectively.
Piguxe 7b, being from the site close to shore shows warming at the gx'ound with stable, (almost isothermal), air above to 1000 meters.
The soundings at the inland site show a basically un-stable atmosphere (except for a neutxal layer between 300 and 800 meters) all the way to 1000 meters.
Hence the isothermal air from the lake has been completely changed to an unstable atmosphere.
Prom the winds obtained in these runs, the inland site was effectively 3 miles inland and this overland distance, the ai& heing heated from below, was enough to destroy the stability of the onshore flow. If a TXBL did exist, below 1000 meters it existed closer to shore than 3 miles.
YORK RESEARCH CORPORATION
~
STAMFORD, CONNECTICUT
REPORT NO.
Y-8186 PAGE 8
Figures,8a and b are plots of Runs 93 and 97 and Run 95 res-pectively from sites I and J respectively..
Prom the winds obtain-ed, site 1 is effectively 3 miles inland, and s'ite J was O.S miles inland.
Prom Run 92 the air off the lake'p to at least 600
~
meters was again almost isothermal.
The latexuns however show no indication of the isothermal layer.
The most obvious point on Pigures 8a R b is the shallow ex-tremely unstable layer present'n all three traces.
(Note also the increase in wind speed, above this unstable 1ayer).
This unstable layex occurs at S30 meters for both inland. runs even though they are thxee hours apax't, the run close to shore however occurs at 3SO meters.
Both inland temperature profiles again show 'no isothermal air up to 1000 meters.
On April 27, Run 99 shows an inversion to 900 meters with xelatively light winds.
The winds remained, light out of the southwest until 1030 E when the lake breeze came"ashore at Snake Swamp (Site K) ~
The polar plots of runs 100,
- 101, and 102 axe too small scale to show the shallow onshore flow but it did exist, at both sites K and L.
Pigures 9a
& b are temperature plots of Runs 101 and 102 at sites K and L respectively
.The temperature traces of both Runs 100 and 101 resemble the ascent part of Figure 9a, es-pecially the stable trace below 200 meters.
This stable air is the low level onshore flow off the cold lake.
Xn the southerly return flow above, the, lapse rate.is neutral with some, small layexs of instability.
The descent paxt of Figure 9a resulted when the Balloon broke and the temperature sensor dropped into the lake.
This trace is almost parallel to the ascent trace in the southerly flow aloft.
However, there is a vexy strong inversion above the lake up to 300 meters out where the sensor impacted.
A plume, therefore, could not descend to the lake surface and be caught in the onshore westerly winds that exist below this inversion, but would continue out in the southerly winds, thus preventing any recirculation anywhere near a shoxeline source.
Figure 9b is the temperature px'ofile at site L, 2 miles inland.
This site'as chosen because it represents the maximum inland penetration of the lake breeze, Xt did not even exist at the east end of the field used as a baseline,, only the west end.
YORK RESEARCH CORPORATION
0 I
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REPORT NO.
Y-8186 pAGE 6
Note that all the stable flow at the surface is now heated from below and. not stable.
Xf a TIBL existed in the stable onshore flow it must have been very close to shore and. could only have attained. the same height as the stable layer, only
.200 meters.
Run 103 from the fossil site also showed.
a stable layer at the surface to 300 meters moving onshore with a south westerly return flow aloft with a neutral lapse rate.
Run 100 at sun-down shows a surface offshore flow with a slight inversion up, to 300 meters and neutral lapse rate above.
Run 105 shows a
ground inversion up to
~f00 meters at 0530 the next morning.
BUFFALO SOUNDING CORRELATION The soundings taken twice a day at Buffalo Airport have been plotted (Figure 10) on the same scale with the Sterling and.
Ginna balloon sondes for comparison.
Soundings have also been plotted from Grand Xsland, a location near Buffalo.
Xn the areas of overlap of the traces the balloon sondes from the Rochester and Oswego area,do not seem to be significantly different from Buffalo.
YORK RESEARCH CORPORATION sTAMFQRD, cOANECTICUT
REPORT NO.
Y-8186 PAGE 10 TABLE 1
~Data Do Run 1D Ol 02 03 04 05 06
~
O7 08 09 10 11 12 13 14ls 16 17 18 19 20 21 22 23 24 25 26 27 28 29 30 31 32 33 35 Date 6/2s/73 8/10/73 8/10/73 8/10/73 8/11/73 8/ll/73"'/23/73 6/23/73 6/23/73 6/24/73 6/24/73 6/24/73
~ 6/24/73 6/24/73 6/24/73 6/24/73 6/2S/73 6/2S/73 6/2s/73 6/2S/73 6/25/73 6/26/73 6/26/73 6/26/73 6/26/73 6/27/73 6/27/73 6/29/73 8/10/73 8/10/73 8/1O/73 8/ll/73 8/12/73 8/12/73 8/12/73 Time
~DDT 1050 0630 1200 1445 0640 1300 1020 1430 1600 0930 1100 1230 1400 1600 1.800 2000 044S 0645 0800 0900 1000 1000 1100 1230 1400 1030 1200 0730 0730 1130 1510 1445 0530 1205 1530 Site fx'om Ha A
A A
A A
A A
A A
A A
A A
A A
A A
A A
A A
Ginna Ginna Ginna Ginna B
B B
A A
A A
A C
A Temp.
Data Yes Yes Yes Yes Yes Yes'es Yes Yes YORK RESEARCH CORPORATION N
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STAMFORD, CON NECTICUT
I i
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4 REppRT Np Y-8186 PAGE 11 TABLE 1
~Data Lo (Cont'd.)
Run XD 36 37 38 39 40
~ 41
~ 42 43 44
.45 46 47 48 49 50 Sl 52 53 54 55 56 57 58 59 60 61 62 63 64 65 66 67 68 69 Date 8/13/73 8/14/73 8/14/73 8/14/73 8/14/73 8/14/73 8/14/73 8/14/73 8/16/73 8/16/73 Not completed 8/16/73 10/ll/73 10jl2/73 10/12/73 10/12/73 10/12/73 10/12/73 10/12/73 10/13/73 10jl3/73 10/13 j'73 10/13/73 10/13/73 10/1S/73 10/15/73 10/15/73 10/15/73 10/1S/73 3/ll/74 3/12/74 3/12/74 3/12/74 Time
~S~T 0930 0530 0730 0900 1000 1100 1215 1340 0600 0930 134S 175S 0650 1000 1105 1345 1530 1720 0700 101S.
1130 1400 1615 0645 1245 1415 1550 1700 1720 1745 0650 1320 1525 Site from Ma A
Ginna Ginna Ginna Ginna Ginna Ginna Ginna A
D A
A A
A A
A A
A
=A A
A A
A A
A A
A A
A A
A A
A s
Temp.
Data Yes Yes Yes Yes Yes'es Yes Yes Yes Yes Yes'es Yes Yes Yes Yes Yes Yes Yes YORK RESEARCH CORPORATION
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STAMFORD, CON NECTICUT
I
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REPORT NQ.
Y-8186 PAGE 12 Run ID.
70 71 72 73 74'5 76 77 78 79 80 81 82 83 84 85 86 87 88 89 90 91 92 93 94 95 96 97 98 99 100 101 102 103 104 10S Date 3/12/74 3/13/74 3/13/74 3/13/74 3/13/74 3/14/74 3/14/73 3/14/74 3/14/70.
3/15/74 4/23/74 4/23/74 4/24/74 4/24/74 4/24/74 4/24/74 4/2S/74 4/2S/74
~
4/25/74 4/25/74 4/25/74 4/25/74 4/26/74 4/26/74 4/26/74 4/26/74 4/26/74 4/26/74 4/26/74 4/27/74 4/27/74 4/27/74 4/27/74 4/27/74 4/27/74 4/28/74 TABLE 1 (cont'd.)
~Data Lo Time
~DDI 1710
'700 1315 1610 173S 0830 1300 1500 1700 0645 1630 1700 1330
'400 1430 1630 0600 1140 1220 1310 134S 1800 0615 1200 1215 1400 1420 1500 1720 0515 1140
- 1310 1350 14S5 1900 0530 Site from Ha s
A Ginna Ginna Ginna Ginna A
A A
A A
A A
A A
A A
A F
G G
F
~ 'A I
. l J
JI A
-K K
L A
A A
Temp.
Data Yes Yes Yes Yes Yes Yes.
Yes Yes Yes'es Yes Yes Yes
-Yes" Yes Yes Yes Yes Yes Yes Yes Yes Yes Yes Yes Yes YORK RESEARCH CORPORATION STAMFORD, CONNECTICUT
REPORT NO.
Y-8186 PAGE.
13 LIST OF FIGURES 1 a-d 2 a-f 3 a-f 4 a-d 5 a-e
~ 6 a-f 7 a b
8a b
9 a b
'10 Sterling Area Site Maps Weather Maps for June 23-29, 1973 Weather Map s for August 10-16, 197 3 Weather Maps for October 11-15, 1973 Weather Maps far March 11-15, 1974 Weather Maps for April 23-28, 1974 Temperature Sounding 4/25/74 1140 E R 1345 E
Temperature Sounding 4/25/74 - 1310 E
Temperature Sounding 4/26/74 - 1200 E R 1500 E
Temperature Sounding 4/26/74 - 1400 E
Temperature Sounding 4/27/74 - 1310 E
Temperature Sounding 4/27/74 - 1350 E
Buffalo Airport Soundings YORK RESEARCH CORPORATION
'TAMI'ORD,COiNECTlCUT
REPORT NO.
Y-8186 PAGE.
14
SUMMARY
From the 105 runs made in the test year, it is interesting to note that'he winds do indeed approach the calculated geostrophic wind.
The speeds and directions approach the geostrophic wind surprisingly close even above inversions and circulations.
A factor that has become apparent is that ground. based, inver-sions do develop and at times become quite extensive.
These invexsions seem to be governed. by the geostrophic wind..
The weaker the geostrophic wind., the deeper the inversion and also the more Southerly the geostrophic wind., the deeper the inver-sion.
This is probably due to the fact that,a Southerly wind passes over large areas of cold land..
From the data obtained.,
there seems to be no obvious difference
.between Ginna and. Sterling winds.
Only one case of a reasonably strong "lid" was found (Run 54) in all of the sonde runs made.
- Hence, from these data the conclusion is drawn that lids do not develop in this area at least to the altitudes tested.
On June 24 and 25, 1973 and April 27, 1974, the development of an offshore lake breeze circul'ation pattern is quite evident including the temperature vs. height traces that are commonly found. for off-water circulations.
Obviously, no circulation develops with a Westerly geostrophic wind, or with Easterly winds since E'asterly winds are generally strong winds in that area.
Hence, only light Southerly or Westerly geostrophic winds will enable a circulation to develop.
From the runs of June and August of 1973, and April 1974, the maximum geostrophic speed in which a lake breeze will develop appears to be about S meters/sec.
with a cold lake (June and April data).
No lake breeze developed in August even with a geostrophic wind of 210' 3.7 meters/sec.,
perhaps due to the lake water being too warm.
Prom the temperature trace of the descent of the sensor into the lake, and from observations o'f the strengthening and changing of the circulation with time, it seems very unlikely that a
circulation would develop and remain constant for long periods of time
~
On the test days of onshore gradient flow, no TXBL of the type described by Lyons can be surmised by the data.
This conclusion is based on the April test period where attempts were made to locate such a condition by traversing iqland as far as 3 miles..
YORK RESEARCH CORPORATION sI'AMFoRD, coNNEGTIGUT
REPORT NO.
PAGE.
Prepared'y:
Michael N. Kozenko Project Director Reviewed By:
P Charles E. Kitson Project Manager gQQK H~PQQ C,'H CQP PQQQ+$ Q+
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STAMFORD, CONNECTICUT
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REPORT NO. PAGE. hUGUST 10, 1973 4 r tt 1012 + IOCOl I 0 IR ~ ~ 'i !'t 7 t 5, Cl gV'2 ' t ,ri)- i t'~i" 51aq V, ogl ~ 22 5t 'I < V ~ Ctr - igt)1 li ,Ttt cs t)5 ct'tl ~ I t st ~ ) 4+ct +/ a 2+ 0 2r 55 I J 4 ~ t '2 Ct lr tll tll c" rP 0 ~ oN<cv 'I ct ' ll ctc l), ~ ) lt ~C,42 5 J ~9 2 4" 5.7 A ,2+ tc)tt, ~ tt~ -re l ~ J ~ "w Ic r >r Il ":ct +rs ting I\\7 SS Pt I I'ttrttS ~ r.l/ I ,J 71 Sc C'e <<4~~ 0 '.c,: SS I lr 0 of'OL tr ~I ~; ll SV tyS'i'tii c C'ag I)f I +S ~ rt 4 4) c) SI )14 g i))2 ~'2 O'Ig tl 'I rr. ~ =.' '24 ~ ti ~ pf 3 b 'hTURDhY, hUGUST 1 1 ~ " '10 0 'O)0 )040 ~ IOOI ~ I IOOC YORK RESEARCH CORPORATION ~ sTAMPDRD, coNNEGTIGUT M
I I c 4 REPORT NO. PAGE I 2973 gure 3 c I 10 1012 s IOP! csi 4.,44. r Stv W.' ~ 4 44 c<<c / S .1 ~4 44ct ct 22 tto ~ @can <<tet 4>> ~P.ta &cga+ts tt r 4 4~ ct 4 ~ ysc Cr4'>>r sc ~\\ 4 +at ft 4 <<f t <<"gets 44 4 +c ~ ~ c oc tc rcc vrtr 'I r l cs 4 ~ <<4O>>. v n bc sagss ~ scl J at st ~ L tr S ~ 44 n ccS 44~>> <<t 2tsr 1 tv t tc tc 04'igure 3 d ~!el.'al)AY. AQQlIST >3t )ct73 I
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~ ~ s I REPORT NO PAGE Figure 6 at TUESDAY. APRIL 23, 197$ " $024 ', 'CQt ~ $0~ IOI5 I t (( ~ I 1St I (1 t yP'/ ~ >gr.: .c-~/ "IO 2 I 6 3i'DIO l t-, "/( ( j. ~ ~ I'+iwt Ot ~ ~ >>(Vt III'I ( t ~ ~ v3 (v 0 Po00t <<( 4 i(1'. 3k 4~ <<'~ r ~ t<< tt tt 3 v ov t ( I($<< ~ I Dv X+o(-t tJ 3~bt53 <<o g<< C I~(I' tent (01 ~ +3 'W Qt It v II overt ~ tD> / I 30( 0 t giv 0) I ~ ~ ~ N %~,~t tt CC ((t. I ~ %D LL<<J' ~ PI&re 6.b v$/EDNEsoAY; A'PRII, 24, 1974 k 'I016 Ct ~ (33 I '$0041,'10(N~ uCA,IDIO $016; 10$). t 10'. BOP.- 10<<QO I --k> <<io 1,0 "(r ~,.t: II (t(. Qt' )/.<<'<< $$v'4 "4/ 1$ 0 ~>>t I 0 v t ~ Itr(tl'I ~>A.~QS o.f g.;/t'-5 ( ~ 0 I 41 3 I(,9't I 1 h (II ((u Io ~ r ~ ~' ., vol 'I'" t( +O o %g '( //.<.<<. YORK RESEARCH CORPORATION ~ ~ ~ sTAMF0RD, CQNNEGTIGUT
I I ~ I L REPORT NO. PAGE Figure 6 e ITJIURSDAY. APRlL 2Kb 1974 )( I g,y.l ~ 100(X IV(<e(1'll 1015 1020 I IO ),.qb '~ I r- . qJ.. ~LZ/'O '1000 ( OW bb) ~ .'4(.,<<. '-. '. ~~ v 1 lo( HIGH~4/ V 4bam j>> ~m4 3 >/ g..., (i" p o.j 8b~. ~i4(I ~o- ~I(a st.>>" ~ ~L g> "'lV'%I'I4 ~ ~ 1>>A OIt4 V >M v bV ~%Q ,S. (b4
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REPORT NO. PAGE ~pc, s wig& SATURDAY,APRIL 2.. l9 ~ass Q tt/~>> zs au tt 1 ~ ~ r s ) /y ~'e ~/ S$.. I s' g .c5 Ct L% os tt >j4+ 4l /t +ddt t . +~'4~ 'tto tit1 wos t Figure 6 f;UNDAY. lmO 'lolc " -ll6 ~ sp-nr APRIL 28. 1874 s ll ggci+ ",~ 'lp t ~ C gt C C" Pt gJ/ v s o .sc, I d. ~ Otl ' p t s s t l,l g' let + lpOh h tA 5th tt ti mt ~ Ot, I t 6 pA I '"l hp ll >x l / s YORK RESEARCH CORPORATION ~ 'TAMFORD, CONNECTICUT
REPORT NO. PAGE BALLOON-SONDE SOUNDING FIGURE '-7 a Site: Barker Road Date: 4/25/V4 Time: 1345E -x 1140E -o ~ 4 ~ ~ ~ I ~ ~ ~ ~ ~ ~ ~ * ~ 3500 ~ ~ I ~ tr.'.O"- ~ ~ I ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ rl ~.... ~ I ~ ~ ~ ~ +. ~ ~ ~ ~ ~ ~ ~ ~ ~ I ~ I ~r ~ I ~ ~ r ~ ~ ~ ~ ~ ~ ~ ~ ~ 3000 .44lr. I ~ ~ ~ ~ =::i;.:L I 0 ~ ~ ~ ~ ~ ~ ~ 'I 4 u ~ 2500 ~ ~ ~ ~ I ~ ~ r ~ ~ I ~ r ~ 2000 H'.!1i:: 4 ~ N ~.- ~ ~ ~ ~ ~ ~ ~ ~ ~ I ~ ~ ~ r r 1500 [-4 1000 ~ ~ ~ ~ ~ ~ ~ I ~ ' ~ I ~ I ~ ~ ~ ~ r ~ ~ ~ ~ ~ ~ \\ ~ ~ ~ ~ ~ I I ~ ~ ~ ~ ~ I ~ 500 ~ I << ~ ~ ~ ~ ~ ~ I ~ ~ ~ ~ r ~ ~ ~
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~, ~ REPORT NO. PAGE e Barker Road >>tet 4/25/V4 Time . I3I0 ONDE SOUNDING 7 b BALLOON-S FIGURE 4000 ~ ~ 3500 t ~ ~ JI ~ I ~ ~ I ~ 3000 ~ ~ ~ I- ~ ~ ~ ~ t ~ ~ 2500. ~ t ~ I ~. ~ ~ ~ ~ ~ ~ ~ t ~ t t ~ ~ 2000 ~ ~ ~t ~t ~ ~tt ~ ~t ~ ~ ~ I ~ ~ tt ~I 1500 '000 ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ' ~ ~ ~ ~ I. ~ ~ ~ ~ t ~ ~ ~I ~ ~ ~ I ~ ~ 500 ~ ~I 4 ~ ~ I ~ ~ ~ ~ ~ I ~ ~ ~ ~ I ~ ~ ~ ~ I ~ I ~ ~ ~ ~ ~ +. ~ ~ ~ 0 -10 -8 -6 -4 -2 +2 +4 +G +8 +10 CENTERED AT 4~ ~ F. TE NIP ER ATURE YOZt< RSSZaaC+ COarcawriOW ~ sTAMFDRD, coNNEGTIGUT
I' REPORT NO. PAGF I3ALLOON-SONDE SOUNDING PXGURE 8 a 4000 Site: Sidman's Hill .. Date: 4/26/V4 Time: 122IO E -< 1500 E -e ~ ~ ~ ~ I ~ ~ ~ ~ 3500 ~ ~ ~ ~ I ~ J F t ~ t ~ ~ 3000 t ~ 2500 ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ t ~ '000 I ~ ~ ~ 1500 B. 1000 iliit' ~ ~ ~ ~ ~ ~ ~ ~ t ~ ~ ~ ~ ~ ~ ~ ~ I ~ ~ ~ ~ ~ ~ ~ I ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ I I ~ ~ ~ ~ ~ ~ ~ Jt ~ ~ ~ ~ ~ ~ ~ ~ .'ii:i::ik ~ ~ ' ~' ~ I ~ ~ ~ t 'I 500 ~ ~ ~ ~ ~ ~ ~ I ~ ' I ~
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I I h ~ ~ REPORT NO. BALLOON-SONDE SOUNDING 8> 4000 Site: Sidman's Hill Date I 4/26/V4 Time'400 E - + PAGE 5'S'. ( ~ 3500 ~ ~ ~ 4 ~ ~ ~ i ~ I ~ ' 3000 ~ ~ ~ ~ ~ ~ 2500. ~ ~ ~ ~ ~ ~ ~ J W ~ ~ ~ ~ ~ I 2000 1500 Pl Fl 1000 ~ \\ ~ ~ I ~ ~ I4 ~+r ~ ~ ~ ~ ~ ~4 ~ Q ~ ~ ~ ~ ~ ~ ~ ~ ~ 'Q" } ~ ~ ~ ~ ~ ~ ~ 4 ~ ~ I ~ ~ ~ ~ I ~ ~ ~ 4 ~ ~lt ~ ~ ~ I I ~ ~ I ~ ~ 'I '::I ': + ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ . ~ ~ ~ ~ ~ 500 ~ ~ ~ I ~ ~ ~ 4 0 ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ 0 ~ -10 -8 -G -4 -2 +2 +4 +G +8 )<)0 TE IHIPEHATUBE CRNTEl<ED AT' F. YORK RESEARCH CORPORATION ~GZI 'TAhfFORD, CONNECYlCUT
REPORT NO. I3ALLOON-FXC 4000 SONDE SOUNDING UBE 9 a PAGE. SIte: Snake Swamp Date: 4/27/V4 " TIme'1310E ILscont-o tr ~t ~ ~ ~tC/ 0 ~ ~ ~ ~ ~. ~ ~ t 0 4 00 ~ ~ mm-..=:t:-..::=- ~ -.::: ~ ~ ~ I I ~ ~ 3000 ~ ~ ~ ~ ~ t I ~ I ~ I' I ~ ~ t ~ 2500 I ~ \\ ~ ~ I ~ f ,'teal 2000 1500 i5 1000 ~ ~ ~r ~ ~ ~ ~ ~ ~ ~ ~ - ~ ~ I ~ ~ ~ I ~ ~ I l': ~ ~ ~ ~ ~"I-" ~ ~ f ~ ~ ~ ~ "::::I:-':::::::.:I:::
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I PAGE REPORT NO. Site: southwest Oswego Date: /27/74 Time: ypgp BSrg SONDE SOUND1NG 9 b BALLOON-F1:CURE 4000 ~ ~ I \\ ~ ~ ~ ~ > i ~ ~ ~ w 4 I(. Oa... 3500 j ~ 4 ~ ~ ~ ~ ~ ~ ~ w 3000 2500 ~w ~ ~ 4 Jg ~w ~ ~ ~ ~ r ~ ~ ~ 2000 ~ ~ I r ~ ~ ~ ~ ~ ~ ~ w ~ ~ ~ ~ ~ r w ~ ~ ~ ~ ~ ~ ~ ~ ~ wr ~ r m~3 1500 1000 ~ ~ ~ ~ I ~ ~ 500 ~ ~ ~ 0 ~ ~ ~ ~ ~ ~ ~ ~l a ~ I ~ ~ ~ ~ ~ r'r ~ ~ ~ ~ 0 -10 CENTERED AT '. 5p o YORK RESEP RCH CORPORATION -8 -6 -4 -2 '2 +4 +6 +8 +10
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I ~ ~ ~ ~ -I . ~r O CI OO LL $6+E BALLOPN SOUNDING DATE I SID/RNS HILL I DRTE '42674'.. l TIME(EST) 1400E'UN ID NUMBER 46 BURFRCE CONDITIONS TEMP 9.6 C DEN PGINWj-POLRR RZIMUTH 247.0 POLRR OISTRNCE(M) 1648 -AVa-VERT. VELOCITY(M/SEC-)! I I I C3 C 3+7 ~ ~ I +- j I, I OO Ofo C) X OO ~O QO bJO L I I ~ I r I t ~ ...c. 1 I t ~ I ,', r I J I ~ I ~ I j I I ~ t ~ II I I ~ L ~ ~I ~ I I,'.I I '=Lt I I I I ~ ~ ~ C C ~ I I I ~ ~ ~ y ~ II I;q,i l ~ CI i i r" I I .L E oo I- ~ I a I J oo OO C O r ~ C I / I 5 ~ ~ I ~ I ~ I" I I ~ I ~. 8 I r f OO I ~ I I I I ~ ~ I I ~ I ~ ~ ~ ~ < I'5 I ~ ~ ~ ~ I I ~ 1.4! I 'Lt t ~ ' I ~ ~ I ~ ~ II ~ ~ ~ ~ ~ I I ~ O-1O.Oa O:.OO D. T. PEG D."I' 5>" 0 1 'C C 0 aoGO coo
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ol -'-.': L a 'j i J .L Oo oo PT.8C TEMP -17.8: OEH POIAT ~ ~ POLAR AZIMUTH 247 0 POLAR DISTANCE(H)i 154 RV-VERT.- VELOCITY(N/SEC) 2-Qi RG~E BALLOON SOUNDING DATA S IDNANS HILL OATE '42674; TINE(EST) 1420E. RUN ID NUt'IBER 96 SURFACE CONDITIONS I a a a oo o CO C) )jc O CI ~o a ial. ~ ~ - I'} ~ I a"!' ~ ~ I.I..I ~ 1! . ~I-i II ~ I I ~ I ~ ! ~ ~ I I I+ I ~ ~ I 'iii" ~ I ~ I I ~ I ~ I ~ I a ~ ~ 4 a +a I I; j ~ I ~ I Qo ~o oo o Oo I I I t I ~ I I a J a A I ~ ~M t l ~ I I i.:.}""- ~ II I, ~ r I ~ ~ I ~.. 1 I I.~.. I r 'I.". I,.I I I I a I ~ I I I'I ~ ~ ~.I I a. I a II!taI I ~I}-iI .I.JtJ ~ ~ I ~ ~ ~ I ~ a a .00 10 q DEO C D.T ~ ~ L ~ I 0 I a ,10.0a o 000.00, 10.00 HOR.:SPO (0/SEC) I 20.0o-s.oa .} VEE 000! R ~ SPO. N/SEC)', .00
e-I ~ I ~ 1 L I I.. i.e: - ~ l I I e oo o CV I I oo oo o CO C) oo ~lO I Qo Mo L oo o oo i -so.oo a.oa D ~ T ~ DEO iC RG+E PRLLOOH SOUHDIHG DRTR ~ SIQ(RNS HILL I-bATE '42874. 1 TINE(ksr) 1500E! RUH Ia NUHBER 97 =.i SURFRCE CONDITIONS TEMP '8-8 C DEH POINT": E~Z, I POI R "RZIViUTH i58.0 POLR DISTRNCEIH) 2888'. . RV. VER . VELOCITY(HiSEC).-'--2.8:-- I ~ ~ p ~ ~ .. ~ i ~ L ~ e I ~ ' ~ ~ I ~ I ~ i'e I ,-I I ' ~ i ~ I I ~ ~ I I I I 1 . eI e .a. L r ~, ~ I I ~ .00 I 0.00 'i.ao VER.iSPD:. (I1/SEC) I.a.ooo,oo I.a.ao 20 00-5 HPR ~ SPD i (N/SEC) I I ~ ~ ~ ~ I I I I L i 0 I I OO i 3g. I I S I W E
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RUN I UMBER 98 SURFR 'E COllDITIONS TE 9'-9 C DEN POIN ~ ~ ~ POL R AZIMUTH 314'0 POL.R DISTRNCE(M)I 152. V. YE T. VELOCITYfMlSEC) 4.2 C Ik l --3.4~ I PG+E BALLOON SOUNDING DATR STERLING; FOSSIL SITE DRTE 42 74. II I I I I I I I I I I I oo o CO C3 Xoo ~Q) Qo >o oo o I I I I I I I I i I 1 I I I C I i I I I ~ I I ~ 'I ~ ~ ~ ~ ' t ~ ~ I I I i i I S l I ~I I I I ~ i oo j I" I oo I I -'10.00 0.00 D ~ T ~ DEG.C I I. l i i '0.09).00- ,10.00 l 20.00-5 HOR. SPO'. ~~iSEC> .oo: o,.oo VER ~
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,.s oo I ~ } I o ' I oo o C} oo o O.K1. 8 ~ VERT.- VELOCITY(H/SEC) RG+E. BFILLOON SOUNDING ORTH'TE}ILTNG FSSS(L SITE ,.DRTE '42774'TIHE(EsT) asisE! FAUN ID NUHIBER 99 I SURFRCE COI<OITIOHS TEHP 2'S' PEN'OINT, }- POLRR: AZIHUTH 314'. 0 POLRR'ISTANCE(H)f 162..' ~ ~ ~ ~ ~ I ~ ~ C) y oo ~o ~Q) I Qo ~o Mo s I ~ }'s I ~ s I I } ~ ~ L. s ~ I s ~ I ~ I I.I" ~ ~ T s I I s s ~ s ~ ~ ~ J s ~ } s ~ ~ T s Y I I s I ~ I I s I ' }.' ~ ~ s s I ~ Q ~ ~ ~ oo oM oo ,10~ 00
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I ~ I i ~ I o CD oO i ~ ~ ~ ~ ~ TIM ( EST ) 1140E. RUH ID NUMBER 0 SURTACE COHDITIONS 'I TEMP 8 6 C DEW"POINT i GLAR AZIMUTH 22S'.6 GLAR DISTANCE(M).'22. VERT. VELOCITY(M/SEC) --- --AV. RG+ BALLOON SOUNDING DAT S(FlgE SNAMP t)AT 4277 ~ I I I I I l i I O lD o CO C) X CDO ~CO I Qo I Bio oo o ~ ~ 1! "- i ~ I - ~. ~ *l i ~ l i I i ~ I I -'- ~ J. L J + l".: i ~ ~g ~ ~ ~ i ~ I r i ~ i ~ I i ~ I ~ i '- ' I-I .' l.l I.j li! ~ I I I ~ ~ i L Ilij i!'i I 'I 'I i I l I i I E II oo oo L i l oo I I i l S lI l ~ ~ oo a oo -10.00 D ~ T ~ DEB'C
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P 12-2 C DEH POINT =4 I o P PO RV ~ Y RR AZIMUTH 229-'.5 RR DISTRHCE(M) 122 'T= YELOCITY(M/SEC) ':I' 3 13 oo o CO C3 oo ~o ~Q) l Qo 41o P \\ a I I a a I', J I ~ a p ~ I I ~I I I 1 I I LL oo o C4 I ~ I I a I I a 'I J I a I I I I oo I o I 1,0 ~ 000.00 I HQ .OO: O::.Oo 10.00 20 Do-5 R SPD;. -10 00 0.00 D ~ T ~ DEO'C 5 woo YER 'SPD' (M/SEC) lj I I I I I (M/SPC) I I r I l a I.. 'J' I r-I ~ t a ~ a ~ ~ I H I I a o IJ a I I o S I 'l L I I l I I
LL TT -. i ~... ~ ~ ~ i+- ~ ~ i o RUN SURFA 'TE I PO PO AY'E NUMBER 2 E COHDITIONS P 15.6 C'EN POINT AR AZIMUTH 266.'.9 AR DISTANCE(M)'52. RT. YELOCInIMiSEC) RG+ BALLOON SOUHDING DAT ~SO THIIEST OSNEGO . DAT '42774'.....i TIME EST) .1350Ei I I ~ i ~I';I 3 +'3I i I oo o ~ C) C) oo ~o ~lO I Qo Mo Z+ ~ ~ I ~ ~ ~ ~ I ~ I I I I ~ i I I I I ~ ~ l I \\ I oo II I l I oo oo o oo L J. ~ ~ ~ I I l '.i I ~ I - J ~ I ~ ~ 't ~ I I S I -10.00 0.00 0 T OED C
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I o Ct) -I J ~ ~ ~:--~-- ~ ~ J .I I I' I. I DO oO D CQ C) OO ~O ~ CC) QoO Uo I I I I I 4 I RG+E BALLOON SOUNDING ORTII STERLING(FOSSTL SITE . DRTE 42774' I... i. TINE ST) (465EI I RUN I NUHBER 3 l SURF E CONDITIONS I Pc PO PO -AV IP 17.8 C "DEN POTHT I-.8 L I .I I J ~ 1 II.I.. i".. ~ t ~ t ~. I ~ I AR AZIMUTH 314;0 AR DISTANCE(H).'62" RT'ELOCITY(H/SEC) 2a3'.--- ~ I t ~. I ~ I I I, ~ t ~ ~ ~ I I ~ t ~ I II I oo o I Cr OO ON ~ t I ~I 4 ~ ~ ~ t ~t 'J I I ~ ~ ~ I I ... 5.). ) ~ I 1 I ~ ~ ~ oO -:10.00D'T O;.Oo OEG I 1Q. 0(XI'a00 I
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h I-h ~ II ~ ~ ~ h oo;ol C4 RG+E BALLO H SOUNDING DAT STERL IN'S 8 IL S ITE DATE '4277K, I. TINE(EST) P900E( RUN ID H ABER '4'URFACE OHDITIOHS I TEHP 1.8 C DEW POINT. POLAR .ZIHUTH 3t4.'.0 POLAR ISTANCEIN)'62. AV. VERT VELOCITY[H/SEC-) oo oo I I J I II I-2 18 oo o(0 CD oo ~o ~ ~ ~ I ~ ~
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oo o h 'h ~, ~ Do oo oo o POLAR DlSTAHCE(N)l 152. Y.. VERT'. VELOCITY(li/SEC) . -"A RG+E PALLOOH SOUHDIHG DATA STERLIHG: FOSSIL SITE .bATE '42874I ,TINE(KSTl 0530E RUH ID HUl(BER 5 SURFACE COHOIT?OHS 'TEHP 16.4 C DER-'POIHT S POLAR AZIMUTH 314'.0 3 v2 '1 ~ ~ ~ ~ r ~ ~ ~ ! l I ~ I ~ I I ~ ~ ~ ~ (0 oo ~o ~CD I Qo IIo (do I ~ ~ fI ~ ~ ~ ~ ~ I l I ~ ~ h ~ I ~ ~ h ~ I 1 ~ ~ ~ I "I ~ t ~ I I ~ I I ! o o oo. E DD o I), '..L I ~ ~ ~ I 1 I I ~ I I S I ~J Do h 1r ~ I ~ o-10.00 O.OD D. T ~ DEO.C r r I'0.093'.00 10.00 I H.OR i SPD (N/SEC) I ~
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IO CDO Ill CD CD o CD CD CD CO O IIIo CD ~o ~o h. ~o C=Io go ~ID hl)Oo ~o Q:Oo ~Cd CI I O I-o ~ID CE CD CD CD o CD BUFFRLO RRPT X 73 6 25 700 BUFFRLO RRPT X 73 6 25 1900 STERLIHO le RUB [0 2 .73 6 25 1050 \\ I 'I 1 \\l I I I I I I I I 1 I I I I I I I I I \\ I I II IIIII \\ 1 \\ I 'I CD CD 'b.oo Ia.ao 2o.oo Sa.oo co.oo so.oo Sa.oo 7o.oo Bo.oo so.oo Ioo-oo TEMPERATURE OEG. F
o oo ID o ID ORAHO fS. X 73 6 25 2040 STSRLfHO fO RUN fO f 73 6 26 1050 oo oo oo 0o ID ~ CO C) >oo ~o ~o 4 ~o <o ~o ~ID txJ)~o ~o Qoo ~OJ CI o I-o ~ID Cf: 1 \\ \\ '1 1 1 1 1 o o ooo ID 1 l 1 1 \\ X oo b.00 10.00 20.00 30.00 40.00 50.00 60.00 70.00 60.00 90.00 100.00 TENPERRTURE DEB. F
~4<7) o oo ID BUFFRLO RRPT X 73 8 10 700 STERLTHO 8 RUII 10 2 73 8 10 630 o o ID ~e CO C) Xoo ~o ~o IJ ~o I:Io +CV IJI) I=oooo (Q ~ ~CO C) I o I-o ~ID CE BUFFRLO RRPT X 73 8 10 1900 ST ERL INO RUN 10 3 73 8 10 1200 STERL[HO + RUH 10 4 73 8 10 1446 llllll lhllll lll l ~ lhll l 'I l l 1 \\ \\ 'f 1 l l l 1 l l l l 'l l o b.00 10.00 20 00 30 00 40 00 50.00 60.00 70.00 80.00 90 F 00 100 00 TEMPERATURE DEG. F
oo CIL CD IIL oo oo o CD o ID CO o "o CD &o ~o 4 ~o >o ILJ ~o ~o Qo CD ~CO 0 ~o Wo +CD CC o oo o ID GRANO 1' 73 8 10 730 GRAND fS 73 8 10 2030 STERLfNO 8 RUN 10 2 73 8 10 630 SfERLINO RUII 10 3 73 8 10 1200 SfERLfNO + RUN IO 4 73 8 10 1445 I I f I I I I I I l l l l l ll ll l lfi CD CD b-00 10.00'0.00 30.00 40.00 60.00 60.00 70 F 00 80.00 90.00 100 00 TEHPERFITURE OEG. F
oo oo ID CI o ID oO o oo O ID CO C) >o' ~oo I-co 4 ~o t=to +CO 4J)~o ~o Q O ~@I C3 t o wo I-o ~lD CK BUFFALO RRPT X 73 8 11 700 SUFFRLO RRPT 73 8 11 1900 STSRLfNO 8 RUtt 10 5 73 8 ll 640 STERLftt0 RUtt 10 6 73 8 11 1300 SfhRLfNO + RUtt f0 32 73 8 11 1445 'f 'f \\ l 'l ll 'l l 'l l l l l \\ \\ \\ \\ \\ 'l \\ l l l l l \\ \\l l l \\ 1 \\ o o OO CI ID Oo b-00 10 00 20.00 30<<00 40.00 50.00 60.00 l0.00 80 00 90 00 100 00 TENPERRTURE OEG. F
LJ O ID OO O ID ORRHO tS X 73 8 11 800 SfERLfHO 8 RUH 10 6 73 8 11 640 Oo OO Oo ID ~ CO CD oo ~o ~o fI ~o CDo ~R CD'IJ) CDO ~o Q Oo ~Cd CD +O I-o ~ID CC OO Oo oO o tD ORAHO fS. SfERLfNO 73 8 11 1936 RUH tO 6 73 8 11 1300 STERLfNO + RUH 10 32 73 8 11 1445 I I I 'I I \\ I \\ \\ l I I I I I I I/ I ( I / Oo b 00 10 F 00 20.00 30 F 00 40 F 00 60.00 60.00" 70.00 80-00 90.00 100 00 TEMPERATURE DEG. F
OO 10 CI O tlat o o Oo O lD C) >oO ~o ~o LL ~o <O ~O cv hJ)~o Q,Oo ~CO CI +O o ~U7 CC CIo O OO o lA BUFFALO ARPT X 73 8 12 700 BUFFALO ARPT 73 8 12 1900 STERLIHO 6 RUN fo 33 73 8 12 630 IRWIN Ro RUH Io 34 73 8 12 1205 LLll LL L'l0. Ll LLlllll'lllll
- 'll llllll Ll LL 1'L Ll L 'L Ll ll ll LL n
1 '\\ L 'L ~ 'I CI CI 0 b-oo 10.00 20.00 30.00 40.OO SO.OO BO.OO 70.00 80.00 90.00 100 F 00 TEMPERATURE DEB. F
O ID OO LD O O ORRHO IS X STERLIHO 6 73 8 12 800 RUH IO 33 73 8 12 530 ORRHO IS. )X IRMIH RO a 73 8 12 1900 RUH Io 34 73 8 12 1206 ID ~ A o >OO ~ O ~o h. ~O t=IO ~O ~ID txJ) ~O ~o Q OO ~Cd C3 +O wo I0 ~ID CL O OO O O lD l \\ 1l ll ll llllll ~ n . 'llll 99 1 I I 1 / I I O 0 -oa Io.oo 2a.oa So.aa 4o.oo So.ao so.oo. 7o.oo So.oo So.oo Iao.oo TEMPERATURE OEG; F ~ ~ ~
CD CD CD tD o CD CDIlt CDo CDo BUFFRLO RRPT X 73 8 14 700 BUFFRLO RRPT 73 8 14 1800 OINHR ST 6 RUB to 37 73 8 14 530 OleiR ST RUN fo 42 73 8 14 1215 CDo CDtlt ee C9 C7 >o CD CDo 1t ~o Oo ~o 4J C-"t~o g) ~ Q oo ~OJ C) t o ~o I o ~O CD CD CDo o CD o tlat 1 'l l 'l l l l \\ 1 'l \\ 'l 1 'l l \\ l \\ \\ l I I C CD CD b-ao 10 80.00 1oo.oa .oo 2a.oo Sa.oa 4o.oo so.ao 60.00 ~ 70.00 80. TEt1PERRTURE OEG-F
CDO CD CD ID V7 CDO oo CD CD CD tlat C) >oO ~o I-n IC ~o <o LCj)go ~o Q;Oo WN o ~o wo I-o ~ID CC CD CD CD CD CD O tD DRAND IS ~ X DINHA ST 8 73 8 14 900 RUN ID 37 73 8 14 530 DRRHD IS ~ DINNA ST 73 8 14 1915 RUH ID 42 73 8 14 1215 1 \\ \\ 1 1 \\ \\ \\ I I I I 1 CD CD b 00 10.00 20.00 30.00 40.00 50.00 60.00 70.00 80.00 90.00 100-00 TEMPERATURE DEG. F '
4 4 D CDD ID D CD III BUFFALO RRPT X STERLfNO 6 73 8 16 700 RUN fo 44 73 8 16 600 D CDD DD ID ~o CO C) >DD ~D ~CD II w<D ~m ~cu M) ~D ~D (PD ~OI CI ~D I D ~ID CK CDD CI D CI D lO 8UFFRLO RRPT 73 8 16 1900 IIACNEfL RUN fo 46 73 8 16 930 ~ 9 I'ERLINo + RUN fo 47 73 8 16 1346 I I I I I I I I I \\ 'I \\ / // / \\ / \\ I I I I I I l. I 'I I I I \\ \\ I I I I' 'I \\ \\ D b.oo 10.00 20.00 30.00 40.00 SO 00 60.00 70.00 80.00 90.00 100.00 TEt1PERATURE OEG. F
O CD ID oO Ill OO Oo ID lA ~ C) C) >o ~ O ~o 1C Wo <o ~o W) Ooo CQ ~ Qo WM lD +o I o +CSEE Cf: ORRHO IS ~ X 73 8 18 1900 STERLIHO 8 RUH IO 44 73 8 16 600 HRCHEfL RUH IO 4S 73 8 16 930 SIERLfHO + RUH IO 47 73 8 16 1345 1 1 1 \\ 1 \\ \\ \\ I CDo OO O O lA Oo t).00 10.00 20.00 30.00 40.00 SO.OO 60.00.. 70.00 80.00 90.00 100 00 TEMPERATURE DEB. F l lg
o oo tO oo oIll V' o oo oooM ~s C9 C) >oo ~o ~o 4 wI-Io CC o ~ID 4J ~o ~C4 CI I o wo Io JIO oo oo oo o tD 8UFFRLO RRPT X 73 10 12 700 BUFFRLO RRPT 73 10 12 1900 srERLrHo F e RUN fo 49 73 10 12 660 srERLfNO F RUH fo Sa 73 10 12 1000 STERLING F + RUH ro S2 73 10 12 1346 srERLrNo F x RUN ro 64 73 10 12 1720 I '1 I 1 I I I I I I \\ 1 I 1 I I I I I 1 \\ l \\ 1 \\ \\ 1 I I I I I I I I I I \\ I 'I I 1 / I / / I I o 'b.oo lo.oo 2o.ao so.oo 4o.oo sa.oo 60.00 70.00 80.00 90 F 00 100 00 TEMPERATURE OEG. F
CIO lA OO O lO OO OO O Cl lO ~ C9 o "O O ~ O ~o b ILI)~o ~o Q OO ~CO C). I O I-o ~to CC OO D OO O tO 1 ll llll 1'Lll 11 1 1 1 I 1 1 1 1 1 1 1 1 '1 1 1 1 1 1 1 \\ 1 1 1 1 \\ \\ 1 1 \\ \\ BUFFALO ARPT X 74 4 24 700 BUFFALO ARPT 74 4 24 1900 STCRL1NO RLH 10 84 4 24 1430 OO b.00 10.00 20.00 30.00 40 F 00 50.00 60.00 70-00 80.00 90.00 100.00 TEMPERATURE DEB. F
o o IO oo O ID oO oo Oo ID CO O >oO ~O ~o 4 ~o Oo CL ~ ~R cu 4J)go ~o +Oo ~OJ O ~o I-o ~ID CL o ID CIo Oo ID 8UFFRLO RRPT X 73 10 13 700 BUFFRLO RRPT 73 10 13 1900 STERLfHO F 19 RUH fp SS .73 10 13 700 Sl'ERLfHO F RUH fp 66 73 10 13 1016 srEPLIHO F + RUH fp SO 73 10 13 1400 srERLfHO F x RUH fp 69 73 10 13 161S 'Pf 11 'I l I \\ I \\ I I I I I I I I I I I I I I l I I I. I I I I I I . I I oo P b.pp Ip.pp 20.00 30.00 40.00 SO.OO 60.00 70.00 60.00 90 00 100 F 00 TEMPERATURE DEG-F
o oo I/J oo o JCJ BUFFALO ARPT X 74 4 2S 700 61'ERL IHO RUH IO 86 74 4 26 600 oo o oo D CCJ Fl C) xoo ~ o I p> IJ IJJ I-"Io go ~ JCJ IJJ)~o ~o (70 Cl CV oD I o Io J CCJ CC oo Clo oo o CIJ )f ll l \\ \\ l l l l 1 \\ 1 \\l l l 'l l \\ l 'l \\l 1 I 1 l 1/ l )f \\ ll l I I I I I I I I / / BUFFALO ARPT 74 4 26 1900 BARKER ROA RUH IO 89 74 4 2S 1310 STERL IHO RUH IO 91 74 4 25 1800 oo b.00 10.00 20.00 30.00 40.00 SO.OO 60.00 70.00 80.00 90-00 100.00 TCMPERATURE OEG F
O OO CD OO ID CDO OO CD CD Ci C) O ~ OO t-n 1C 4J)()O @O Q OO C4 C7 t-O ~o I O ~tD Ct: BUFFRLO RRPT X 73 10 16 700 BVFFRLO RRPT 73 10 15 1900 STERLING F Et RUtt 10 60 73 10 16 646 STERLfttG F RUtt 10 62 73 10 IS 1416 STERLfttG F + RUtt 10 64 73 10 15 1700 \\ 1 1 \\ '1 '1 \\ 1 1 1 1 1 1 1 1 1 1 I 1 I 1 I 1 I 1 I 1 1 '1 1 '1 1 1 1 CD OO OO CD CD 1 I CDO b.00 10.00 20 00 30.00 40.00 SO.OO 60.00 70.00 80.00 90 00 100 00 TENPERFlTURE OEG. F
oo lQ oo o lO o oo o D lD C) Xoo ~ o I-cg IL. ~o Oo cu LLI)D Oo (Q ~ Q:o M C) I D I-D ~ F7 (Z oo Do D lO 1 1 \\ \\ \\ 1 1 1 1 1 1 1 1 1 1 1 1 '1 1 '1 1 1 1 1 \\ 1 1 1 1 1 1 1 1 1 1 1 1 \\ \\ \\ '1 1 \\ 1 '1 1 BUFFALO ARPT X 74 4 26 700 BUFFALO ARPT 74 4 26 1900 STERLINO RUN IO 92. 74 4 26 6.15 S IONANS RUN IO 93 74 4 26 1200 SIONAMS + RUN IO 95 74 4 26 1400 SIOtIANS RUN IO 97 74 4 26 1500 STLRL INO RUN ro 96'4 4 26 1720 Do b-00 10 ~ 00 20 ~ 00 30.00 40.00 50.00 60.00 70.00 80.00 90-00 100 ~ 00 TEMPERATURE DKG F
O oO lO oo o lD oo oO o O EOii) D "O O ~ OO Ipp 4 ~O Do CC O cv hJ)Do ~o QoO D I O 0 I-O ~ill CL \\ 1 1 1 \\ 1 1 1 1 '1 1 BUFFALO ARPT 74 4 27 700 BUFFALO ARPT 3X 74 4 27 1900 STERLING 6 RUN fO 99 74 4 27 515 SNAKE SM RUth IO 0 74 4 27 1140 SHAKE SN + RUH IO 1 74 4 27 1310 SOUTIIIIES X RUN IO 2 74 4 27 1350 STERL IHO RUN IO 3 74 4 27 1455 STERLING + RUN IO 4 74 4 27 1900 oO oO O lD 1 1 1 1 1 \\ 1 1 1 OO b 00 10-00 20.00. 30.0D 40 F 00 50-00 BO.DD 70.00 80.00 90 00 100.00 TENPERRTURE BEG-F}}