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In May of 1994, we were on a monster storm (and we rarely use that
term) near Littlefield, TX. It was an HP storm that, if you simply
look at the synoptic observations around the storm, one would never
know what really happened. Obs around the area only showed winds at
around 5 to 10 knots. The storm deepened significantly on the mesoscale,
and created winds up to 45 knots on our anemometer. There were some
tornado warnings with the storm, and it certainly had some mesocyclone-type cloud features, but there was no way to get very close to the updraft
area of this storm. Large hail and flooding rains were also reported.
The state police saw us chasing the storm and pulled us over. We figured
we had done something wrong. It turned out that they were spotting, and when they saw us going in
the opposite direction away and ahead of the storm, they figured they had better follow us. They asked us where we
were headed, and then gave us a POLICE ESCORT, with one trooper ahead of us and
one trooper behind us.
Picture of the beaver's tail
The updraft region and wall cloud that
continually got undercut by cold outflow. This wall cloud is for the
most part on the leading edge. You can see some of the inflow bands
leading into the storm.
The storm as it becomes/develops into
a squall line