The CheyenneTornado
July 16 1979
Jonathan D. Finch
Historical Tornado Cases for the Boulder Warning Area
Historical Tornado Cases for the Cheyenne Warning Area
Historical Tornado Cases for the United States
April 23 1960 Cheyenne Ridge Tornado
May 7-8 1965 Front Range Tornado
June 14-17 1965 Front Range Superstorm
High plains and front range topo maps
Overview
On July 16, 1979, the most damaging tornado in Wyoming history touched down 3 miles west-northwest of the
Cheyenne airport. This strong tornado
moved east or east-southeast across the northern part of Cheyenne,
causing $22 million in damage and 1 fatality.
140 houses and 17 trailers were destroyed. 325 other houses were
damaged. Four C-130 aircraft and National
Guard equipment sustained $12 million damage. Municipal hangars
and buildings suffered another $10 million damage.
There were no hail reports with this storm or any other storm
that day in Wyoming. A woman was killed instantly by lightning after climbing to the top of Pingora Peak (11884 ft)
about 28 miles west of Lander.
Meteorological Discussion
A strong shortwave trough moved across the northern
plains on July 14. This helped push a cold front from
northern Wyoming on the 14th to northern New Mexico
on July 15. But with the jet remaining across the northern
plains, the front underwent frontolysis late on July
15 and into July 16. Frontogenesis occurred from far western
Wyoming into Kansas and southern Missouri on July
16. At midday July 16 (19UTC) the front was located
immediately north of Laramie and Cheyenne. This
boundary sagged south through Laramie by 20 UTC, but was
still immediately north of the Cheyenne airport. The
southward push of the front was possibly due to
thunderstorm
outflow as storms developed along the boundary by
late morning and early afternoon. The first indication of a
tornado was 3.5 miles west-northwest of the Cheyenne
airport at 335 pm MDT(2135 UTC). The 22 UTC
surface chart shows the front just south of Laramie.
The T/TD were 71F/56F. At this time the tornado was probably
just finishing its rampage across northern
Cheyenne. By mid-summer standards
in the central or eastern USA this would be a very
cool temperature and a low dewpoint such as would be
found behind a strong cold front. However, the
elevation of Laramie is 7270ft. The author of this page
believes that the theta-e was similar near Cheyenne
and Laramie on the immediate cool side of the boundary.
Despite the T/TD being 12F/16F lower at Laramie than
Topeka, the theta-e was actually slightly higher at
Laramie than at Topeka. The surface based CAPE was
around 2800 j/kg at Laramie at 22 UTC. I
made an approximate sounding for Laramie based on 00 UTC 700-200mb charts/soundings and the
22 UTC surface observation at Laramie. 71/56
at Laramie would give the same theta-e as 77/57 near
Cheyenne. At Cheyenne it was 81F in the early
afternoon. But immedialtely north of Cheyenne it was
surely cooler with much higher dewpoints. In fact,
the dewpoint jumped to 56F at Cheyenne by 22 UTC,
but the temperature was cooler due to nearby
thunderstorms.
01 UTC |
Elev(ft) |
Pres.(mb) |
SLP(mb) |
T(F) |
Td(F) |
MR(g/kg) |
theta(F) |
theta-e(K) |
Laramie
|
7270
|
788 |
1023.3
|
71 |
56 |
8.3 |
98.3
|
354.3 |
Topeka |
881 |
991 |
1020.6 |
83 |
72 |
11.2 |
80.8 |
353.6 |
The mid level warm plume shifted east from July 15
to July 16, with 700mb temps warming to +18-19C
across parts of southwest and south central Wyoming
and adjacent northern Colorado. A strong sfc-700mb
baroclinic frontal zone was apparent across Wyoming.
The 00 UTC 17th Denver sounding showed +14C
700mb. However, this sounding was contaminated by
convection. Since Denver mixed out completely by 20
UTC with a surface temperature of 93F, the 700mb
temperature was surely 17C just before the cool outflow
arrived. The 700mb temperature at Grand Junction at 00 UTC July 17 was 17C. The maximum temperature
was 97F. If you lift a parcel dry adiabatically from
the surface(856mb) to 700mb you get 18C. This is why
it is typically better to subtract 3F from the high
temperature before lifting to 700mb (when determining 700mb
temperatures). This is especially true in light wind
situations. In strong wind and very dry situations, the
maximum temperature would give a closer
approximation. I used the maximum temperatures at several stations
to augment the 700mb chart.
01 UTC |
Elev(ft) |
Pres.(mb) |
MaxT(F) |
MaxT(F) -3 |
700mb T |
Rock Springs
|
6760 |
800 |
88 |
85 |
18
|
Rawlins |
6813 |
799 |
88 |
85 |
18 |
Jackson Hole |
6560 |
805 |
87 |
84 |
16.5 |
Yellowstone |
6640 |
803 |
83 |
80 |
15 |
Eagle |
6540 |
809 |
91 |
88 |
18 |
Rifle |
5540 |
835 |
93 |
90 |
17 |
Denver |
5300 |
841 |
93 |
90 |
16.5 |
Grand Junction |
4858 |
856 |
97 |
94 |
17 |
Vernal |
5280 |
841 |
92 * |
93 |
16.5 |
A jet streak also slowly moved east from 12
UTC July 15 to 00 UTC July17 across the northern plains.
Southeast Wyoming was located in the right rear
quadrant of this jet on the afternoon of the 16th.
By the afternoon of July 16, a well defined frontal
boundary extended from east of Yellowstone to east
of Jackson Hole to west of Lander to near Rawlins,
to near Laramie to near Cheyenne.
Upper air charts:
7-15-79 00 UTC 700 500 250
7-15-79 12 UTC 700 500 250
7-16-79 00 UTC 850 700 500 400 300 250 200
7-16-79 12 UTC 850 700 500 400 300 250 200
7-17-79 00 UTC 850 700 500 400 300 250 200
Surface charts 21 UTC 14 06 UTC 15 09 UTC 15 12 UTC 15 15 UTC 15 18 UTC 15 21 UTC 15 00 UTC 16
03 UTC 16 06 UTC 16 09 UTC 16 12 UTC 16 16 UTC 16 17 UTC 16 18 UTC 16 19 UTC 16
20 UTC 16 21 UTC 16 22 UTC 16