SYNOPSIS FOR 05/09/94 - VORTEX-94
A deep upper level low pressure system remained stationary over Arizona
throughout the day. A minor wave rotated around the upper low and
enhanced instability over southwestern Texas early in the day. A convective
cluster propagated eastward and weakened over central Texas by late
morning. A weak tornado occurred around 830 AM CDT south of SJT
with the convective cluster. The wave rotated northeastward around the
upper low, and enhanced upper level divergence aided convective
development over southern Colorado, northern New Mexico, and the
northern Texas Panhandle during the afternoon hours. A Canadian cold
front entered northern Oklahoma and the northern Texas Panhandle early in
the day and advanced southward very slowly to near a line from AMA to
BVO by late afternoon. East to northeast winds at 15 to 20 mph with higher
gusts persisted behind the boundary. Dewpoints behind the boundary
remained in the upper 50s, and the strong east winds resulted in a
reasonable hodograph even though mid level winds were very weak.
Intense thunderstorms developed over the northern Texas panhandle and
produced prodigious amounts of hail in Dallam County. The Texas
Highway Patrol reported "two" tornadoes in Dallam County. The AMA
WSR-88D detected a persistent mesocyclone with rotational velocities of up
to 45 knots with the Dallam County storm.
Convection developed over the high terrain of southeastern New Mexico
around noon and moved toward the east-northeast into Texas west of
Lubbock. One of the storms exhibited a rotating updraft in New Mexico,
but the rotation dissipated as the storms moved into less favorable flow.
Other storms developed farther south in southwestern Texas, and a tornado
was reported south of Iraan. Softball-sized hail also accompanied that
storm. Mid level winds were substantially stronger over southwestern
Texas and southeastern New Mexico, but weak low level flow persisted
throughout the day. In addition, rain-cooled outflow advanced westward
late in the afternoon and assisted in the death of the storms west of Lubbock
before sunset.
A convective complex developed during the nighttime hours over eastern
New Mexico with increasing southeasterly low level flow after sunset.
Ruthi/Leduc
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