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ANALYSIS OF SYNOPTIC FOR DATASELECTED HAlL DAYS IN NORTHEASTERN COLORADO, 1961
by
Richard A. Schleusener
Civil Engineering Section Colorado State University Fort Collins, Colorado
Final Report, NSF Grant G-1 7964
Research supported by the Atmospheric Sciences Program National Science Foundation
August 1963 C'..v'.OR...,, ~OQL.u. CER63RAS34 ': 1 N1v J,SIT'.1, • ~ .. o IV
INTRODUCTION DATA AND METHODS
TABLE OF CONTENTS
Selection of days for study Synoptic Data . . . . . RES UL TS AND CONCLUSIONS . .
Mean values of synoptic parameters Severe hail days
Moderate hail days . . . . Days with no hail . . . .
Parameters with no apparent correlation with hail intensity Mean soundings SUMMARY OF PROJECT APPENDIX Page 2 2 2 2 2 3 5
ANALYSIS OF SYNOPTIC DATA FOR
SELECTED HAIL DAYS IN NORTHEASTERN COLORADO, 1961
INTRODUCTION
The successive objectives of the research on hail being conducted at Colorado State University are:
1. To obtain the climatology of hailfalls and rainfalls in the High Plains, a region of high frequency of hail
2. To determine the environmental factors
which favor the occurrence of hail
3. To design and conduct an experiment in hail modification by cloud seeding.
Work done under National Science Foundation
Grant NSF G 17964 was directed at the second of these objectives. This report presents an analysis of synoptic data for selected days with hail in North -eastern Colorado during 19 61. A summary of mean values of the various synoptic parameters examined and a discussion of their relative importance are given in the body of the report. The appendix includes data for case studies of six days of severe hail, six days on which hail of moderate intensity occurred, and six days on which no hail occurred during the period 1 May - 31 July 1961.
DATA AND METHODS
Selection of days for study - - Five criteria were used to classify hail intensity for each day during the 1961 hail season from 1 May to 31 July, using data from the Colorado State University network. These criteria were: 1) the number of reports of hail occ ur-rence received from cooperative observers; 2) maxi-mum stone size; 3) maximum energy number; 4) the
largest "most common" stone size; 5) the number of damaged hail indicators.
Using these criteria, the following dates were chosen as being a representative sample of hail days of the intensities indicated: Severe--May 13, May 16,
May 31, June 2, July 1, and July 14; Moderate- -May 21, May 24, June 8, June 13, June 28, and July 8; None--May 22, June 21, June 26, July 3, July 17, and July 23.
Synoptic data - - For each day, the following in -formation was obtained:
1. Surface synoptic patterns gathered from data collected a: 1100 and 2300 MST. The surface
weather maps for this report were taken fr om the Daily Weather Map prepared by the U. S. Weather
Bureau
2. 500 mb contour patterns at 1700 MST, also taken from the Daily Weather Map.
3, The jet stream configuration and isotach
analysis at 1700 MST, obtained from 300 mb facsi
-mile charts.
4. A mean wind profile over the area, obtained
by averaging upper wind reports from LND, DEN, BFF, LBF, GLD from the ground surface to the tro -popause.
5. Wind profiles along the mean wind direction for each respective upper-air station in the vicinity, including Lander (LND), Denver (DEN), Scottsbluff (BFF), North Platte (LBF), and Goodland (GLD).
6. Vertical air mass structures, obtained from plotted raob soundings (Skew-T, log P diagrams) at
0500 and 1 700 MST.
7. A precipitable water and stability index chart, taken from USWB facsimile charts.
8. A chart showing the forecast size of hail-stones at stations in and near northeastern Colorado
by the Fawbush-Miller method, using the 1700 MST raob soundings.
9. Diagrams showing the daily rainfall amounts and hail occurrences, compiled from reports by co
-operative observers and hail indicators in the hail
network.
These synoptic data are presented in the appen
-dix for each of the 18 days selected for study. RESULTS AND CONCLUSIONS
Mean values of synoptic parameters - - Table I
gives average values of selected synoptic parameters for days classified as having severe, moderate and no hail.
Table 1 shows little difference in the stability index and precipitable water for the three categories
of hail intensity. On the other hand, a faster mea!l
jet stream speed and high mean wind speed are asso -ciated with the severe hail days. A further
distinc-tion between severe and moderate hail lies in the orientation and location of frontal systems with re
Table I. Mean synoptic parameters for days with hail of three intensity classifications. Values given are means with six days per category.
-
-
-
-
---
-Hail Showalter Precipitable Jet Stream Mean Wind, Fronts
Intensity Stability Water, Category Index, Inches
Deg. C
- -
-
-
-
_
___,!
SevereI
o.o .76 Moderate I 0.5 .76 None o. 6I
.64These observations from Table 1, based on mean values, are substantiated by examination of data from individual days.
Severe hail days - - In examining the severe days, the existence of a jet maximum overhead of about
55-60 knots indicates a day of severe rather than
moder-ate or no hail. Values for moderate and "none" days
were approximately 35-40 knots. For severe days,
the value of the jet maximum ranged between 30 and
I 05 knots.
One of the best correlations was found to be the position and orientation of the surface front over the
region. In all six severe cases, the front was
posi-tioned to the southeast of the area. No distinction
was made in this analysis between mP and cP air
masses causing the fronts.
The presence of a low pressure system to the
south of the area favored the occurrence of severe hail. On 5 of the 6 days studied, low pressure systems
were noted to the south of the area, and three of these proved to be of substantial strength producing hall as
the low pressure area moved to the east. The average position of low pressure areas was in WSW Kansas
(120oz).
Moderate hail days - - Days with hail of
moder-ate intensity exhibited no strong preference for any of
the parameters studied. The mean frontal positions
for these days was with an orientation N-S, a distc..nce of about 205 miles to the WNW of the center of the forecast area. This might lead to the conclusion that the storms producing moderate hail were associated
with pre-frontal activity. Only one out of the six days
had a front which had already passed the area by 120oz.
The idea of the dew-point front might be suggested as a cause for hailstorms of moderate intensities,
since the most intense storms frequently occur after the frontal passage or as the dry denser air behind the
front and aloft over the mountains displaces the res
i-dual moist air remaining behind the front. Occassi on-ally, low pressure systems were noted SE of the
Speed Surface to Tro
-Knots popane, Direc-
IN
. Mi
. Distance2
tion and Speed, Orien- and Direction Knots tation __
¥ ~.e.iw..m:.L
NNE-57 260 /33 .SSW
I
188 SE I 40 27 0 /25 N-SI
205 NW 38 I 310 /26--
-I
---forecast area, but these were static and sluggish systems.
Days with no hail - - A primary difficulty in this study was an inability to find parameters which dis
-tinguished days of moderate hail from days of no hail
occurrence. As mentioned earlier, there was little
difference in the jet speeds, the value for both being 35-40 knots. Frontal and low pressure activity and
centers were indefinite for the no-hail days. One positive correlation did appear, however, on the
no-hail days. For days of no hail, the direction of the
mean wind speed from the surface to the tropopause was from the NW (310°), while the direction for the moderate and severe days was 270° and 260°, respec -tively.
Parameters with no apparent correlation with hail intensity - - Some of the parameters showed no correlation with hail intensity. The.Showalter
Sta-bility Index and the Precipitable Water Amounts were such parameters. The respective values were as
follows: Severe--SSI = 0, with range of -3 to +4; precipitable water = • 67; Moderate--SSI = 0, with range of Oto +2; precipitable water = • 76; None--SSI
= 0, with range of Oto +4; precipitable water = • 64. Mean soundings - - Finally, computations were
made to determine mean soundings for the days in
question. By grouping all the days of severe, moder -ate, and no hail, respectively, three average sound -ings for the area were constructed to demonstrate a severe hail day sounding, a moder ate hail day so und-ing, and a "no-hail" day sounding. These soundings are given in Figures 1, 2 and 3. These average sound -ings were determined by taking the soundings for the
individual stations of LND, BFF, LBF1
, DEN, and GLD, for both 120oz (morning) and 0000Z (evening). After averaging for each station, a weighted average was determined for the six days of the study.
Figures 1 and 2 show remarkable similarity which suggests that they represent typical hail so und-ings without regard for intensity.
Examination of the soundings indicates no obvious
features such as, for example, the typical hail and tornado soundings of the middle West, studied by Faw-l::ush and Miller. It may be noted that the surface temperature tends to increase at OOOOZ when the hail intensity decreases. This could be attributed to the fact that on the severe.and moderate days a lower sur-face temperature may be caused by the presence of thunderstorms in and over the area, with the result-ing downdrafts coolresult-ing the region.
A lo° C dew-point spread was common for all levels of the severe hail sounding, increasing to I 0-15° C spread for moderate soundings, and finally to as much as 20° C spread for days of no hail. These
soundings indicate that the occurrence of no hail is related to the dry soundings, but to determine whether severe or moderate hail would occur cannot be deter-mined from the sounding. Analysis of the soundings also indicates that the mean severe sounding is some
4-5° C cooler from the surface to 400 mb than the
lapse rate for the mean no-hail sounding. This can not be attribi.:ted to the presence of thunderstorms, since both the morning and evening soundings for the severe day exhibit this temperature reduction. One important conclusion is that when analyzing the sound-ings for the CCL (using the 120oz for predicting pur-poses) and the convective temperature, Tc , which would initiate cumulus development by heating alone, the Tc lies below the reported surface temperature for the OOOOZ observation. Granting that this observation may take place after the afternoon maximum tempe ra-ture is realized, the meteorological events resulting in this conve tive activity are not caused by just reaching the Tc and then retreating. This observation leads to the conclusion that other effects must be active in causing rapid convective development.
Synoptic data are presented in the appendix to permit case studies of each day.
SUMMARY OF PROJECT Period: Personnel: May 1961 - December 1962 Richard A. Schleusener John D. Marwitz August H. Auer
Publications (prepared in whole, or in part with
sponsorship from Grant NSF G 1 7964).
l. Schleusener, R. A. On the relation of the latitude and strength of the 500-milli-bar west wind along 110 degrees west longitude and the occurrence of hail in the lee of the Rocky Mountains. Prepared for Amer. Meteor. Soc. Conference on Severe Storms, Norman, Oklahoma, Feb. 1962. Colo. State Univ., Civ. Engg. Rpt. CER61RAS46.
3
2. Sch_eusener, R. A., and T. J. Henderson Hail genesis areas in and near north-eastern Colorado. Colo. State Univ. Civ. Engg. Rpt. CER61RAS58, Oct. 1961.
3. Schleusener, R. A., and L. 0. Grant Characteristics of hailstorms in the Colorado State University Network,·
1960-61. Proc. Ninth Weather Radar Conf. , Oct. 19 61.
4. Schleusen.er, R. A., and T. J. Henderson Observational data on the position of hailfalls with respect to precipitation cells. Presented at Amer. Meteor. Soc. Conference on Severe Local Storms, Norman, Oklahoma, Feb. 1962. Colo. State Un-iv. Civ. Engg. Rpt. CER62RAS1.
5. Schleusener, R. A. "Hailstorm c haracteri-zation and the crystal structure of hail. Pending publication in Amer. Meteor. Soc. Monograph on Severe Local Storms
Colo. State Univ. Civ. Engg. Rpt. CER62RAS9, Feb. 1962.
All times
4Fig.I Mean sounding for severe hail days
.
Fig. 2 Mean sounding for moderate hail days
.
APPENDIX
Data for Case Studies of Selected Hail Days in Northeastern Colorado, 1961
Hail Intensity Category
Severe Moderate None 5 Dates May 13, 16, 31 June 2 July 1, 14 May 21, 24 June 8, 13, 28 July 8 May 22 June 21, 26 July 3, 1 7, 23
Ha
i
l reports
,
0
ESI0
()
I
0<E~
I
00
•
E> 100
Cose
of
•
Hail c loss if icot
ion
Number of rep
ort
s from
CSU network
1Mox
stone
siz
e
1Mox
E,
ft
-
lb
s
per sq ft
.
1Largest
"
most
co
mmon•
stone size
•
13 Moy 1961
Severe
72
I •
14
1552
Number of dam
ag
ed
i
ndicators, CSU network
190
oSIDNEY
Mox size of stone
,
i
~
el 06
HOLYOKE 0 OTISReports of Ho i I
E • impa
ct
energy,tt- lbs
per sqft.
S= max
st
one
size,·
inches.
M• missi
ng
data
.
Rain
fall
Depth
(Inches)
C WRAY
0
O<s::;f
6
4<S:52
I"
.1.'.'
0-
f'
<S$.
1119
l"<S:5 2
11-0
S>2"
Surface Synoptic Pattern
II AM
a
II PM MST
05CXJf1ST
Precipitable Water ( inches)
a
Stability Index
Cose
of
Hail Classification•
13 May 1961Severe
500
MB
Flow
1700 MST
Jet Stream 50
a
100 kt.
·
isotochs
I
I
I
I
I
I 0 LNO 0~r
BFF LBF 2r
OENG1o
Mean Wind - Surface to Tropopause
(knots) 1700 MST
Il
LNO 0t
BFF 0 LBF I 8 0 OENG1o
Forecast Size of Stones (inches)
·
Cose of, 13 Moy 1961 Hail Classification, Severe
Lander North Platte
Denver
SKEW-T
Diagrams0S00MST
=
l200Z
l 700MST=0000Z
Cose of, 13 Moy 1961 H oil Cl a ssificotion, Severe
ro.-~---
- -
~ - -
-
- - - ~
r o ~ - ~ - - - -
-
- -
- -
-0 ..._
)
/
.-(.-,<..
\
J
,(,_ IQ 20 :30 40 50 60 7 Wind Speed ( knots)Lander 80
ro~.---
- - - -
---l
0·~--...
--·:::---..
·-
-~
.
.Y'-.
IQ 20 :30 40 50 60 70 a, Wind Speed (knots) Denver Legend Doy before• -·-·-Doy of severe hail= -Doy ofter•Hail Intensity Classification Doy before• Doy of, Doy ofter= Severe Severe Moderate
Wind Profiles Along Mean Wind Direction For 1700 MST
0 IQ 20 :30 40 50 60 7 80 Wind Speed (knots)
Surface Synoptic Pattern
II
AM
a
11 PM MST
Precipitable Water
( inches)
a
Stability Index
Cose
of
•
Hai I
Classification•
16 Moy 1961 Severe500
MB
Flow
1700 MST
Jet Stream 50 a 100 kt
.
isotachs
I
!14
LND I 0 BFF H B F ~ Ndfo
Mean Wind - Surface to Tropopause
(knots) 1700 MST
I 8 0 LND 0 I BFF 8 0 LBF I~
DENG1o
Forecast Size of Stones (inches)
Hail reports
,
0
ES.10
0
I0<E~I00
•
E> 100
Cose
of
,
Hail classif
i
cat
i
on
•
Number of reports
from
CSU network
•
Mox
stone
size •
Mox E,
ft
-
lbs per sq ft
.
,
Largest
•most common•
stone
size
•
Number of damaged indicators, CSU network
IcSIONEY
NEBRASKA
COLORADO6
el6
D RAYMER D FT.MORGAN D STERLING6
66
~
6
0 . . el C OTIS ~Reports
of Hail
HOLYOKEo
c
00
D WRAYE• impac
t
energy,ft-lbs
per sqft.
S= max
s
tone
size,·
inches
.
M•miss
in
g
data.u
NEBRA
S
KA
COLORADO D RAYMER D FT.MORGANRa
infall
.25 C OTIS Depthff
(Inches)
D WRAY~;,1
~
16 Moy 1961
Severe20
3"
4
301
3"
4
8
Max
sizeof stone ,
0
O<s~f
6
I"
J.'.'
4<S~
.
2
0-
f'
<S$.
111Q
1"<S$.
2
11-0
S>2
11Case of, 16 May 1961 Hail Classification= · Severe
ro
ro.---,c---+-0 ~40 C: 5! :,i
30 C: ~20 > .!! LLI 0 / /I
/
/ IO 20 30 4 0 5 0 6 0 7Wind Speed (knots)
Lander
80
o,'---;I0~-::;2~0-,30/;.;---,4t:.o:---•50~----;;6l;,;O-¾-.dd
Wind Speed (knots)
Denver
Legend
Day before=
-·-·-Day of severe hail= -Day after,Hail Intensity Classification Doy before , None
Day of= Severe Day after= None
Wind Profiles Along Mean Wind Direction For 1700 MST 0 ~40 C: 5! :,
i30
20 30 4 0 5 0 6 0 7 80Wind Speed (knots)
North Platte
Case of, 16 Moy 1961 Hail Classification , Severe
Lander North Platte
Denver
SKEW-T
Diagrams
0S00MST
=1200Z
Hail reports
•
0
E~IO
()
IO<E~IOO
•
E>IOO
Cose
of •
Hail classification
1Number
of re
ports
from
CSU network
1Max stone
s
ize •
Max E,
ft-
lbs
per
sq ft
.
,
Laroest
•
mos
t common•
stone size
•
Number
of da
maged in
dicators, CSU network
,
NEBR
ASKA
COLO
RADO
0 RAYMER 0 FT.MORGAN ® cSIDNEY - A\J-~o
""
-()
<te-()
•
0 STERLING.
ensReports
of Ho
iI
6
C HOLYOKE 0 WRAYE • impact
energy,
ft- lbs
per sq ft.
S=
max
stone
size,
inches.
M• miss
ing
data.
- 2 ~
- ~
NEBR
ASKA
( t j ]
COLOR
AOO
0 RAYMER 0 FT.MORGANRainfall
0 STERLING.
ens Depth C HOLYOKE(Inches)
0 WRAY 31 Moy 1961Severe
17 1" 260 ~II4
7Max size of stone
,
0
O<s~f
6
I"
.1.'.'
4<S~
.
2
0-
f<s~1"
Q
l"<S~ 2
11-0
S>2"
I/NI
llll
Surface Synoptic Pattern
II
AM
a
II PM MST
Precipitable Water { inches)
a
Stability Index
Cose
of
•
Hai I Classification,
31 Moy 1961 Severe500
MB
Flow
1700 MST
!7COMST
Jet Stream 50
a
100 kt. isotochs
~NO
'l
~FF 0 LBF ~ NGio
Mean Wind - Surface to Tropopause
{knots) 1700 MST
0 0 LNO 0 I B1-F 8 0 LBF I 8 0 OENGio
Forecast Size of Stones {inches)
{Fawbusha
Miller)1700MST
60~-
- - - f
C120
> .!! LLI 0--
~
K) 20 30 4 0 5 0 6 0 7 80Wind Speed (knots)
Lander G Q , ~ - - - -- - - 1
.,
.! 50 0 ~40 5! :>!30
C~
20 > .!! LLI 0 K> 20 30 4 0 5 0 6 0 7 80Wind Speed (knots)
Denver
Case of• 31 May 1961 Hail Classification• Severe
Legend
Day before• • • -Day of severe hail• -Day after•
Hail Intensity Classification Day before, Severe
Day of• Severe Day after• None
Wind Profiles Along Mean Wind Direction For 1700 MST 0 C ~20 > .!! LLI 10 0 K> 20 30 4 0 5 0 6 0 7 80
Wind Speed ( knots)
Case of•
Hail Classification,
31 Moy 1961 Severe
Hail
reports ,0
ES.10
() I0<ES.100
•
E>
1
00
Case
of
,
Ha
i
l
cl
as
s
if
i
cati
on
Number of repo
rts
from
CSUnetwork ,
Max
stone
siz
e
•
Max
E,
ft- lbs
p
er sq ft
. ,
Largest
•
most
com
mon•
stone size
•
Number of dam
aged
indicators,
CSUnetwork
•
' NEBRASKA COLORADO ct-() <al ()
~
• . ~~ME~J
••
STEiLINGi
....
®-6
·
®
()
6
~f
C>-oQ FT.MORGAN~ ® C OTIS cSIDNEY C HOLYOKE D WRAYReports of Hai
I
E • impac
t
energy,ft-
lbs
per sqft
.
S= max
ston
e size,
inches
.
M
•
missi
ng
data
.
Rainfa
ll
Depth(inches)
2 June
1961
Severe49
1¼"
776
3"
4
65
Max
sizeof
stone •0
O<s~f
6
I"
.l.'.'
4<S~2
0-
f'
<SS I"
Q
l
11<SS 2
11-0
S>2"
Surface Synoptic Pattern
II AM
a
11PMMST
Precipitable Water ( inches)
a
Stability Index
Case
of
·,
Hai I Classification,
2 June 1961
Severe
500
MB
Flow
1700MST
700!'1ST
Jet Stream
50a
100kt. isotachs
L ~3 0 BFF
3
\\\_.-fBF
jN
,
lfo
8Mean Wind - Surface to Tropopause
(knots)
1700 MST
Ia
0 LND 0 I BFF 8 0 LBF I 8 0 DEN I 8dto
Forecast Size of Stones ( inches)
(Fawbush
a
Miller)
1700MST
Lander
Denver
Cose of• H oil Clossifi cation •
~ June 1961 Severe
SKEW-T
Diagrams Goodland0500MST
=120oz
1700MST
=
0000Z
6(),--
- - - ;
.
o
0
l 0 2 0 2 0 4 0 5 0 6 0 7 80
Wind Speed (knots)
Lander
IO 20 20 40 50 60 7
Wind Speed (knots)
Denver 80 Case of• Hail Classification, Legend Day before• • • -Day of severe hail• -Day after,
Hail Intensity Classification Day before, None
Day of= Severe Day after• Moderate
2 June 1961
· Severe
Wind Profiles Along Mean Wind Direction For 1700 MST 60 .; .. 50 0 ~40 C 5! :,
i30
C 0 ·~ 20 > .!! w 10 0.,
.! 50 0 ~40 C 5! :,i30
C ·~ 20 > .!! w 0 IO 20 20 40 50 60 7 80Wind Speed (knots)
North Platte
10 20 20 4 0 5 0 6 0 7 80
Wind Speed (knots)
Hail
reports,0
E~I0
() I0<E~I00
•
E>
100
Case
of •
Hail classification •
Number
of repor
ts
from
CSU network
,
Mox stone
size •
Mox
E,
ft-
lbs
per sq ft.
,
Loroest •most
common•
stone size
•
Number of domooed indicators,
CSU network
NEBRASKA
COLORADO
C RAYMER C FT.MORGAN oSIONEY el ~ d.lNGe>@
e>
•
() 0 OTIS••
..
Reports
of Ho
iI
() 0 HOLYOKE C WRAYE
• impact
energy,ft-
lbs per sqft.
S• max
stone
size,inches.
M•
missing
data. oSIDNEY NEBRASKA COLORADO~
(:) C RAYMER 0 HOLYOKE6
C FT.MORGAN C WRAY Rainfall Depth (inches)July 1961
Severe13
I •
14
2660
1" 6Mox
0
6
Cr
Q
-0
sizeof stone
,
O<s~f
I"
.L'
4<S~2
f<s~ In
l
11<S~ 2
11S>2"
Surface Synoptic Pattern
II AM
a
II PM
MST
Precipitable Water { inches)
a
Stability Index
Case
of
•
I July 1961
Hail Classification
•
Severe
500
MBFlow
1700 MST
/700MST
Jet Stream 50
a
100 kt. isotochs
. !J..1.-0 7 LND
~
_.El BFF, ~
LBF l½iNt
Mean Wind - Surface to
.
Tropopause
{knots) 1700 MST
0 LND I T 0 I BFF T 0 LBF I~
DEN Ie
G<tDForecast Size of Stones { inches)
{Fawbush
a
Miller) 1700MST
Case of• 1July1961 Hail Classification• Severe
60,~---.~ - - - 1
~~
0 C ~20 > .!! w ~ 0 60 ~ 50 0 {!l 40 C 5! ::,i30
C ~20 > .!! w 10 0~=---
--...::-
.
...
-._
IO 20 Zl:l 40 50 60 7Wind Speed (knots)
Lander
BO
IO 20 Z() 40 50 60 7 80
Wind Speed (knots)
Denver 0 C
~
20 > .!! w 0 IO 20 Zl:l 40 50 60 70 80Wind Speed 'knots)
Scottsbluff
Legend
Day before•
-·-•-Day of severe hail• -Day after•
Hail Intensity Classification Doy before, Moderate
Day of• Severe
Day after• None
Wind Profiles Along Mean Wind Direction
For 1700 MST 6 0 ~ - - -- -- - - ;
.,
~ 50 0 0 60 C~
20 > .!! w 0 IO 20 Zl:l 40 50 60 7Wind Speed ( knots)
North Platte
80
Zl:l 40 50 60 7 80
Wind Speed (knots)
Lander
Denver
Cose of•
H oil Clossifi cation 1
s
Cott
s bluff I July 1961Severe
SKEW-T
Diagrams0S00MST 120oz
l 700MS T
=
0000Z
GoodlandHail reports
,
0
ES.IQ
() I0<ES.100
•
E> 100
Case
of •
Hail
cl
as
si
f
ica
tion ,
Number of reports
f
rom
CSU network •
Max stone
size ,
Mox E,
ft
-
lbs pe
r
sq ft.
•
Laroest •most com
m
on•
stone size •
14
July 1961
Severe
18
3"
4
233
Number of damaged
i
ndicators, CSU network •
20
NEBRASKA
COLORADO
0 ®ct®
•
D (t FT,MORGAt,I ® 0()-6
0 STERLING oSIDNEY D OTISR
eports of Hail
0 HOLYOKE D WRAYE • Impact e
ne
rgy,
ft-
lbs per sq ft.
S
=
max s
t
on
e
size,inches
.
M•
missing
data.oSIDNEY
Rainfall
Depth
(Inches)
Mox
0
6
0-Q
-0
sizeof stone
•
O<s~f
I•
J..'.'
4<S~2
f<~I"
l"<S~ 2
115>2"
Surface Synoptic Pattern
II AM 811PM
MST
Precipitable Water ( inches)
a
Stability
IndexCase
of
,
Hai I Classification•
14 July 1961 Severe500
MB
Flow
1700
MSl
,,,,,.-25170011ST
, ,Jet Stream 50
a
100 kt.
·
isotochs
-~ LND 0
~
BFF 9~ LBF9
,
' DEN 0 G DMean Wind - Surface
to
Tropopause (knots)1700
MST
IB
LNO I I) 0 ..L BFF 8· 0 LBF I8
DEN I T G~DForecast Size
of
Stones (
inches) (Fawbusha
Miller)1700
MST•
,! 50 0 0 0f
40 Iii :,!30
C ~20 > .!! LI.I IO 0 10 20 ~ 40 50 60 7 80Wind Speed ( knots)
Lander
IO 20 ~ 4 0 5 0 6 7 80 Wind Speed (knots)
Denver Cose of• Hail Classification• 14 July 1961 Severe 6 Q . . . - - ' . . - ~ - - - j C ~20 > .!! LI.I 0 IO 20 ~ 4050 80
Wind Speed (knots)
Scottsbluff
Legend Doy before, • • -Doy of severe hail• -Doy ofter,
Hail Intensity Classification Doy before, Moderate
Doy of, Severe Doy ofter• None
Wind Profiles Along Mean Wind Direction For 1700 MST
60~---+
•
.. 50 0 .. 40i
:,~30
C ~20 > .!! 10 0 ~ 4 0 5 0 6 80Wind Speed {knots)
North Platte
6Q1.---..,...---f
0 IO 20 ~ 4 0 5 0 6 Wind Speed (knots)
Lander
Denver
Case of, 14 July 1961 Hail Classification • Severe
Scottsbluff
SKEW-T
Diagrams0S00MST 120oz
1700MST
=
0OO0Z
North Platte GoodlandCase
of
•
Hail
classification
,
Number of reports from
CSUnetwork ,
Mox stone
size
,
Max
E,
ft-
lbs
per sq
fT
.
,
Laroest •most
common•
stone size •
21 May 1961
Moderate
I"
4
r,,lumber of damaoed
indicators,
CSUnetwork
,
None
Hail occurred at Fort Collins
Reports of Ha
II
Surface
Synoptic
Pattern
II
AM 8
11PM MST
Precipitable Water ( inches)
a
Stability Index
Case
of
•
21May
1961Hai I Classification,
Moderate
500
MB
Flow
1700 MST
!700M5T
Jet Stream 50
a
100 kt.
·
isotochs
~ND 0 BFF ~ B F M N G<r_D
Mean Wind - Surface to Tropopause
( knots) 1700 MST
I'!
LND 0 BFF <.!. 8 0 LBF I!
DEN G1DForecast Size of Stones (inches)
Case of• 21 May 1961 Hail Classification• Moderate
r o - - - 1
r o , - - - ~
0 IO 20 30 40 50 60 7 80
Wind Speed (knots)
Lander
r o , - - - -
---1
0 IO 20 30 4 0 5 0 6 0 7 80
Wind Speed (knots)
Denver
Wind Profiles Along Mean Wind Direction For 1700 MST
0 IO 20 30 4 0 5 0 7 80
Wind Speed (knots)
Case of, 21 May 1961 Hail Classification, Moderate
Lander North Platte
Denver
SKEW-T
Diagrams0S00MS T
=
1200Z
Hail reports,
0
E~I0
0
I0<E~I00
•
E> 100
Caseof •
Hail
classification
1Number of reports from
CSUnetwork
1Max stone
size
,
Max
E,
ft- lbs per sq
ft
.
•
Largest
•most common
•
stone
size
•
Number of damaged indicators
,
CSUnetwork
•
NEBRASKA
COLORAl
C RAYMER C FT.MORGAN C STERLING cSIDNEY 6.
OTIS 0 HOLYOKE 0 WRAYReports of Hai
I
E • impact energy.
tt- lbs
per sq ft.
S11max
ston
e
size,
inches.
M•
missing
data.
cSIDNEY
0
OTIS
Rain
fall
Depth6
0 HOLYOKE(Inches)
C WRAY24 May 1961
Moderate
5
3"4
248
Max size of stone
0
O<s~f
6
I"
.1'.'
4<S~2
0-
-f<s~ 1"
Q
l
11<S~ 2
11-0
5>2
11Surface Synoptic Pattern
11 AM
a
11 PM MST
Precipitable Water ( inches)
a
Stability Index
/
I'
Cose
of
•
Hail Classification•
24 Moy 1961
Moderate
500
MB
Flow
1700 MST
,__
170011ST
Jet Stream 50
a
100 kt
.
isotochs
I l I i I
~
LND 0 BFFII---,
LBF P-~NGio
Mean Wind - Surface to Tropopause
(knots) 1700 MST
<.L 8 0 LND 0 BFF I 4 0 LBF <..!._ 8 0 DENGio
Forecast Size of Stones (inches)
Cose of• 24 Moy 1961 Hail Classification• Moderate
6 ( ) 1 , - - - j 6 ( ) 1 , - - - +
0
0 ! 0 2 0 3 0 4 0 5 0 6 0 7 BO
Wind Speed (knots)
0 ! 0 2 0 3 0 4 0 5 0 6 0 7 80 Wind' Speed (knots)
Lander North Platte
6()1,-- - - +
0 !0 2 0 3 0 4 0 5 0 6 0 7 80
Wind Speed (knots)
Denver
Wind Profiles Along Mean Wind Direction For 1700 MST
Case of, 24 May 1961 Hail Classification, Moderate
Land er North Platte
Denver
SKEW-T Diagrams
0500MST= 120oz
Hail reports,
0
ES.10
()
I0<ES.100
•
E> 100
Case
of
•
Hail
classificati
on
Number
of
repor
t
s
from
CSU
network
Max
stone
size
,
Max E,
ft- lbs
per
sq
ft
.
•
Laroest
•most
common•
stone
size
•
Number of damaged indicator
s, CSU network
•
NEBRASKA COLORADO D RAYMER D FT.MORGAN C STERLING cSIONEY
6
D OTIS C HOLYOKE C WRAYReports
of
Hai
I
E• impact
energ
y, ft-lbs
per sq ft.
Si:: max
stone
size,
inches
.
M• missing
data.
NEBRASKA COLORADO D RAYMER0
D STERLING6
D OTISRainfall
Depth
C HOLYOKE(inches)
C WRAY8 June 1961
Moderate
2
6
Max size
of stone
•
0
O<ss.f
6
I"..1'.'
4<S~2
Crf<ss. 1"
Q
l"<SS. 2
11-0
S>2
11Surface
Synoptic
Pattern
IIAMS 11PM MST
Precipitable Water ( inches)
a
Stability Index
Cose
of
=Hai I Classification•
8 June 1961
Moderate
500
MB
Flow
I /so
I I!700MST
1700 MST
Jet Stream 50
a
100 kt. isotochs
~
; LND 0,,
BFF LBF'\
I DEN 2~0 IMean Wind - Surface to Tropopouse
( knots) 1700 MST
'
<!
LND 0 <_!_ BFF 8 0 LBF <.!. 8 0 DEN <_!_ 8G1o
Forecast Size of Stones (inches)
6 0 1 . . - - - 4
0 10 20 30 40 50 60 7 80
Wind Speed (knots)
Lander
f,()1,--- - - - ,
0 IO 20 30 4 0 5 0 6 0 7 80
Wind Speed (knots)
Denver Wind Case of• Hail Classification• 8 June 1961 Moderate
Profiles Along Mean Wind Direction
For 1700 MST 6 0 , , - - - + 0 <:: ~20 > .!! LLJ 10 North Platte 6 0 . . - - - ; 0 IO 20 30 40 50 80
Wind Speed ( knots)
Lander Denver Case of• Hail Classification • 8 June 1961 Moderate SKEW-T Diagrams 0500MST= 12002 1700 MST=0000Z Goodland North Platte
Hail reports,
0
E~I0
()
I0<E~I00
•
E>
100Case of •
Hail classification
Number of reports from CSU network , Mox stone size ,
Max
E,
ft- lbs per sqft
.
,
Largest "most common• stone size ,
Number of damaged indicators, CSU network •
NEBRASKA COLORADO C RAYMER C FT, MORGAN C STERLING cSIDNEY
or,S
6
Reports of HaiI
0 HOLYOKE C WRAYE •
impact energy,ft-
tbs
persq
ft. S = max stone size , inches .M• missing data. cSIDNEY NEBRASKA COLORADO C RAYMER
6
&
C STERLING(!JJ
HOLYOKE C FT.MORGAN Rainfall~
2.5" 0,£ffj
OTIS ~ Depth (Inches) C WRAY13
June1961
Moderate2
-r
13
1."
4
Max0
6
0-9
-0
size of stone ,O<s~f
I"
.L'
4<S~2
f<s~ 1"
l"<S~ 2
11S>2"
Surface Synoptic Pattern
11
AM
a
11 PM MST
/700MST
Precipitable
Water (inches)
a
Stability Index
Cose
of
,
Hai I Classification•
13 June 1961
Moderate
500
MB
Flow
1700 MST
Jet Stream 50
a
100 kt. isotochs
LNO 4 BFF i fBF 2 ~ N 4 0
Mean Wind - Surface to Tropopause
(knots) 1700
MST
(.L 8 0 LNO Ig
J_ BFF 2 0 LBF I 8 0 OEN¾
G
1
o
Forecast Size of Stones (inches)
6 0 - - - 1
0 l 0 2 0 3 0 4 0 5 0 6 0 7 80 Wind Speed (knots)
Lander
60,.----
- - - -
- - - l
.,
~ 50 0 C ~20 > ~...,
0 l 0 2 0 3 0 4 0 5 0 6 0 7 80Wind Speed (knots)
Denver
Case of• 13 June 1961 Hail Classification• Moderate
60---
-
- - - - -
---1
.,
., 50 0 ~40 C 5! ::,!30
C 0'E
20 > ~...,
10 0 l 0 2 0 3 0 4 0 5 0 6 0 7 80 Wind Speed (knots)Scottsbluff
Wind Profiles Along Mean Wind Direction
For
1700
MST60
0 l 0 2 0 3 0 4 0 5 0 6 0 7 80
Wind Speed (knots)
North Platte
60....---
- - - -
-4-0 C~
20 > ~...,
0 10 20 30 40 50 60 7 80Wind Speed (knots)
Lander
Denver
Case of, 13 June 1961
Hail Classification I Moderate
Scottsbluff SKEW-T Diagrams 0500MST= 120oz 1700 MSTs00OOZ Goodland North Platte
Hail reports
10
E~I0
0
I0<E~I00
•
E> 100
Cose
of
1Hail
classification
Number of
reportsfrom
CSU network
1Mox stone
size
,
Mox E,
ft- lbs per sq
ft.
1Largest
•most
common•
stone size
1Number of damaged
indicators,
CSU network
•
NEBRASKA COLORADO C FT.MORGAN 0 STERLING oSIDNEY
.
OTIS 0 HOLYOKE 0 WRAYReports of Ho
iI
E• impact
energy,tt-lbs
per sq ft.S• max stone
size,inches.
M• missing
data
.
NEBRASKA COLORADO(:)
FT.MORGAN 0 STERLINGRainfa
ll
oSIDNEY.
OTIS Depth C HOLYOKE(Inches)
0 WRAY28 June 1961
Moderate
2
16
. .L'
4
None
Mox
0
6
0-Q
-0
size of stone
•
O<s~f
I"
.1'.'
4<S~2
f'
<S~ 1
11l"<S~ 2
11S>2"
Surface Synoptic Pattern
II AM
a
11PM MST
Precipitable Water ( inches)
a
Stability Index
Case
of
•
Hai I Classification,
28 June 1961
Moderate
/9200 ,t"~..::.l' ,/ j [}{} ,: ,' -•--J, \J'!_'lt}9-- .,'500
MB
Flow
1700 MST
/7WMST
Jet Stream 50
a
100 kt
.
isotachs
l ND BFF 6
ll-t
eF
I 0 N 3 8 G DMean Wind - Surface to Tropopause
(knots) 1700
MST
<.' ""8" 0 LND <....L. 8 0 <.l. BFF 8 0 LBF I 8 0 DEN I 8 G<?_oForecast Size of Stones (inches)
6 0 - - - 1 0 ~40 C 51 :,
!30
Cl20
> .!! w 10 0 IQ 20 30 4 0 5 0 6 0 7Wind Speed (knots)
Lander
G O r 1
-0 IQ 20 30 4 0 5 0 6 0 7
· Wind Speed (knots)
Denver
-
....
Cose of• 28 June 1961 Hail Classification= Moderate
6 0 - - - ! C ~20 > .!! w 0 IQ 20 30 40 50 60 7 BO
Wind Speed (knots)
Scottsbluff
Wind ,..Profiles Along Mean Wind Direction For 1700 MST 6 ( ) , ~ - - - f 0 ~40 C 51 :,
!30
C 0 '; 20 > .!! w 0 IQ 20 30 4 0 5 0 6 0 7 BOWind Speed (knots)
North Platte
6 ( ) , ~ - - - +
0 IQ 20 30 40 50 BO
Wind Speed (knots)
Lander
Denver
Cose of, 28 June 1961 H oil Clossifi cation , Moderate
Scottsbluff SKEW-T Diagrams 0500MST= 12002 1700 MST,.00002 Goodland North Platte
Hail reports,
0
E~I0
() I0<E~I00
•
E> 100
Cose
of
1Hail
classification
,
Number of reports
from
CSU network
1Max stone
size
1Mox
E,
ft- lbs per sq ft
.
1Largest
"most
common•
stone size
18 July 1961
Moderate
Number of damaged
indicators,
CSU network
INone
NEBRASKA COLORADO C RAYMER C FT.MORGAN
6
oSIONEY C STERLING.
OTIS HOLYOKE C WRAYReports
of Ho i
I
E• impact
energy,ft-lbs
per sqft.
S= max stone size,
inches.
M• missing
data.
Rainfall
Depth(Inches)
Max size of stone,
0
O<s~f
6
I"
.1'.'
4<S~2
Crf<S~I"
Q
l"<S~ 2"
-0
S>2"
Surface Synoptic
PatternII AM
a
11PM MST
/700MST
Precipitable
Water ( inches)a
Stability
IndexCase
of
•
·
Hai I Classification•
8 July 1961
Moderate
L
,iooo
~9{XX)
18800 \ ' \ I / ' \ I____
.... \ /8800 ... ----J,,:--=:::::,....:::::__----.jL,' ''
\
'----mar'500
MB Flow1700 MST
25--OSOOMST
I I I IJet Stream 50
a
100 kt.
·
isotochs
e LND BFF 9 ~ LBF I ~ DEN
Mean Wind - Surface to Tropopause
(knots)
1700
MST
i
0 LND I 8 0 3 BFF 4 0 LBF I 8 0 DEN I 8 G<r_DForecast Size of Stones (inches)
( Faw bus
_
h
a
Miller) 1700 MST
0
-..,
C i ::,!30
C ~20 > .!! w C 0 ~20 > .!! w 0 () 20 ~ 4 0 5 0 6 0 7 80 Wllld Speed (knots) Lander () 20 ~ 4 0 5 0 6 0 7 80·wind Speed (knots)
Denver
Cose of• 8 July 1961
H oil Cl a ssificotion • Moderate
601...---i
5 0 , , - - - +
~40 C 5l ::,!30
C 0 i; 20 > ..!! w 0 () 20 ~ 4 0 5 0 6 0 7 80Wind Speed (knots)
Scottsbluff
Wind Profiles Along Mean Wind Direction
For
1700
MST0 0 20 ~ 4 0 5 0 6 80
Wini! Speed (knots) North Platte
601...--- -- - - +
0 0 20 ~ 4 0 5 0 6 0 80
Wind Speed (knots)
Lander Denver Cose of• H oil Classification • Scottsbluff 8 July 1961 Moderate SKEW-T Diagrams OOOOMST= 120oz 1700 MST•00OOZ North Platte Goodland
Cose
of
•
Hail classification
,
Number of reports
from
CSU network •
Mox stone
size ,
Mo• E,
ft- lbs per sq ft
.
•
Largest •most
co
mmon•
stone size
•
22
Moy 1961
None
None
None
None
None
Number of domaoed
i
ndicators, CSU network
None
oSIDNEY
NEBRASKA
COLORADO
0
d
6
D D6
RAYMER STERLING 00
HOLYOKEd
6
c:39
D FT.MORGAN.
OTIS D WRAYSurface Synoptic Pattern
II AM
a
11PM MST
050011ST
Precipitable Water ( inches)
a
Stability Index
Cose
of
,
22 May 1961
Hai I Classification
I None500
MB
Flow
1700
MST
!700MST
Jet Stream
50
a
100
kt. isotachs
~
LNO 0 I BFF[
LBF I~ DEN G<r_oMean Wind - Surface to Tropopause
( knots)
1700 MST
0 LNO 0 BFF , 1-8 0 LBF ,...Ls
DEN G<r_oForecast Size of Stones (
inches)
s o , ~ - - - ;
'S {; 40 C g :,!
30
C ~20 > .!! LI.I 0 IO 20 30 40 50 60Wind Speed (knots)
Lander
6 ( ) 1 , - - - +
0 IO 20 30 40 50 60
Wind Speed (knots)
Denver
Case of• Hail Classification•
22 May 1961 ·None
Wind Profiles Along Mean Wind Direction For 1700 MST
s o ~ - - - 1
0 l 0 2 0 3 0 4 0 5 0 7
Wind Speed (knots)
Case of, 22 May 1961
Hail Classification • None
La n d er North Platte
Denver
SKEW-T Diagrams
OOOOMST= 12002
Case
of
•
Hail
classification ,
Number of reports
from
CSU network
•
Max
stone
size •
Max
E.
ft- lbs per sq ft
.
•
Laroest
•most
common•
stone size
•
Number of damaoed
indicators,
CSU network
•
21 June 1961
None
None
None
None
None
None
Surface Synoptic Pattern
II
AM
a
11
PM MST
!700MST
Precipitable Water (
inches)
a
Stability Index
Cose
of
,
.
21 June 1961Hai I Classification•
500
MB
Flow
1700
MST
\.170011ST '- - -
-None
Jet Stream
50
a
100
kt.
·
isotachs
I I
I
I
I
I
'~
LNO z,~z\
I BFF LBF I I ~ I OENz
\o
Mean Wind
-
Surface to Tropopause
(knots)
1700
MST
<g
LNO l. ~ BFF .l 8 0 LBF½
0 DEN .1. G~DForecast Size of Stones (inches)
(Fawbush
a
Miller)
1700
MST
•
.! 50 0-g
40 Iii ::t!30
C ~20 > Jl! Ill IQ 0•
.! 50 C ~20 ~ Jl! Ill IQ 0 I() 30 4 0 5 0 6 0 7Wind Speed (knots)
Lander
10 20 30 4 0 5 0 6 0 7 BO
Wind Speed (knots)
Denver Case of• Hail Classification• 21 June 1961 None 6 ( ) , ~ - - - -- - - - ---, 0 IO 20 30 40 50 60 7
Wind Speed (knots)
Scottsbluff
Wind Profiles Along Mean Wind Direction
For
1700
MST 60•~---0 .;g 40 C 5! ::ti30
C 0i5
20 > .!! Ill 10 0 IO 20 30 4 0 5 0 6Wind Speed (knots)
North Platte
r o ~ - - - -
-..
.! 50 0 .;g 40i
::ti30
C ~20 > Jl! Ill IO 0 10 20 30 40 50 BO -Wind Speed ( knots)Lander
Denver
Cose of,
H oil Closs ifi cation •
21 June 1961 None Scottsbluff SKEW-T Diagrams 0500MST= 120oz 1700 MST=0000Z Goodland
Case
of
IHail classification
,
Number of
reportsfrom
CSU network
Max
stone
size ,
Max E,
ft- lbs per
sq
ft
.
,
Largest •most common•
stone
size •Number of damaged indicators,
CSU
network , -NEBRASKA COLORADO D RAYMER D FT.MORGAN D STERLING Rainfall oSIONEY.
OTIS Depth C HOLYOKE D WRAY (inches)26
June1961
None None None None None NoneSurface
Synoptic
Pattern
II AM
a
II PM MST
Precipitable Water (
inches)
a
Stability Index
Case
of
•
26
June
1961
Hail Classification•
None
I ' I ' , , 191()()..,,✓,'
500
MB
Flow
1700 MST
/700MST
Jet Stream
50
a
100 kt.
isotochs
0 LND
1
4
'---'El\
BFF LBF\
DEN 2 ~DMean Wind
-
Surface to Tropopause
( knots)
1700 MST
0 0 LND 0 0 (J__ BFF 8 0 LBF 0 0 DEN 0 G1DForecast Size of Stones ( inches)
(Fawbush a
Miller)
1700 MST
0
60,.---
-
---4
0 IO 20 30 40 50 60 ·wind ed ( knots Denver Case of• Hail Classification• 26 June 1961 Noni,60.---__)
0 l 0 2 0 3 0 4 0 5 0 6 0 7 80Wind Speed (knots)
Scottsbluff
Wind Profiles Along Mean Wind Dire.cti on For
1700
MST 60...---➔..
.! 50 0i
'I() Iii :,!30
C ~20 > .!! LI.I 0 IO 20 30 40 50Wind Speed (knotW
North Platte
60...---+
0 IO 20 30 4 0 5 0 6 7
Wind Speed (knots)
Lander
Denver
Case of, 26 June 1961
Hail Classification, None
Scotts bluff SKEW-T Diagrams 0500MST= 120oz 1700 MST=0000Z Goodland North Platte
Case
of
•
Hail classification ,
Number of reports
from
CSUnetwork
•
Max stone
size •
Max
E,
ft- lbs
per
sq ft. •
Laroest
•most
common•
stone
size
•
Number of
domooed
indicators,
CSUnetwork
•
cSIDNEY
NEBRASKA
COLORADO
D C RAYMER STERLING CeJJ
.
HOLYOKE C FT.MORGAN 0 OTIS C WRAYRainfall
Depth(Inches)
3
July 1961
None
None
None
None
None
None
Surface Synoptic Pattern
II AM
a
11PM MST
170011ST
Precipitable Water
( inches)
a
Stability
Index
Cose
of
•
3
July
1961
Hail
Classification•
None
500
MB
Flow
1700 MST
..50
1700 MST
Jet
Stream 50
a
100 kt.
isotochs
8 ~
DEN
BFF I ~
LBF
Mean Wind - Surface to Tropopouse
(knots) 1700 MST
0 0 LND(!
BFF (J_ 8 0 LBF <J_ 8 0 DEN<i
G1DForecast Size of Stones (
inches)
Case
of
I3 July 1961
Hail
classification
,
None
Number of reports
from
CSU netwo
rk
INone
Mox stone
size ,
None
Max
E,
ft- lbs per sq ft
.
INone
Largest
•most
common•
stone s
ize
INone
Number of damaged
indicators,
CSU
network
,
None
oSIDNEY
NEBRASKA
COLORADO
0 C RAYMER STERLING 0 5(3)
HOLYOKE 0 FT.MORGAN.
OTIS 0 WRAYSurface Synoptic Pattern
II AM
a
11PM
MST
!700t15T
Precipitable Water
( inches)
a
Stability Index
Cose
of
13
July
1961
Hai
I Classification,
None
500
MB
Flow
1700 MST
.50
1700 MST
Jet
Stream 50
a
100 kt. isotochs
4LND
BFF I ~
LBF
8 ~ DEN
Mean Wind - Surface to Tropopouse
( knots) 1700
MST
0 0 LND'i
BFF ,.L 8 0 LBF ,.L 8 0 DEN,t
GiDForecast Size of Stones {inches)
60 .; ~ 50 0 ~ 40 C 5l :, i30 w 0 IO 20 30 40 50 60 70 80
Wind Speed (knots)
Lander 60 .; ~ 50 0 ~40 C 5l :,
i30
C 0 f; 20 > .!! w 0 IO 20 30 40 50 60 70 80Wind Speed (knots)
Denver Wind 60 .; ~ 50 0 ~40 C 5l :, i3o C 0
g
20 .!! w 0 IO Cose of• H oil Cl a ssificotion • 20 30 40 50 60 3 July 1961 None 70 80Wind Speed (knots)
Scottsbluff
Profiles Along Mean Wind Direction For 1700MST 60 .; ~ 50 0
-g
40 0 "' :, 0 :!: 30 C 0 f; 20 > .!! w 10 0 IO 20 30 40 50 60 7 80Wind Speed (knots)
North Platte 60 .; ~ 50 0 ~ 40 C 5l :, 0 :!: 30 0 IO 20 30 40 50 60 7 80
Wind Speed ( knots)
Lander
Denver
Case of, 3 July 1961 Hail Classification, None
Scottsbluff SKEW-T Diagrams 0500MST= 120oz 1700 MST=0000Z Goodland North Platte
Cose
of
•
Hail
c loss if icotio
n
,
Numbe
r
of reports
from
CSUnetwork
,
Mox stone
size ,
Mox
E,
ft- lbs
pe
r
sq
ft
.
,
Loroest
•mo
st
common•
stone size
,
Number of
domaoed
indi
cators,
CSUnetwork
,
NEBRASKA
COLORADO
0 RAYME 0@
I FT.MORGAN D STERLINGRainfall
cSIONEY6
.
OTIS Depth C HOLYOKE 0 WRAY .(Inches)
17 July 1961
None
None
None
None
None
None
Surface Synoptic Pattern
II AM
a
11PM MST
Precipitable Water
(
inches)
a
Stability Index
Cose
of
•
17 July 1961
Hai
I
Classification•
None
, __ ---19KJO _______ _
500
MB
Flow
1700 MST
ZS
!700MST
Jet Stream 50
a
100 kt. isotochs
0 LND 0 0 BFF