Summary of Daily Weather
Date Being Summarized:  10 April 1995

The strong system moving out of the Rockies slowed its digging during the day
and was beginning to lift out over the central plains by 00Z on the 11th.  A
convective system began early in the morning in the western parts of north TX,
and continued through the day and on into the night.  Some strong new convection
developed around 0130Z in south TX behind the surface front, apparently associ-
ated with a short wave moving through the base of the trough.

A couple of targetable storms developed ahead of the morning squall line in the
warm sector in the early afternoon.  These storms, around Corsicana and Waxa-
hachie, TX, had shallow mesocyclones on the leading edge of the precip echoes,
but apparently did not produce any tornadoes.  The tornadic storms were near
Beaumont, TX and in southwestern LA around 2045Z.  There was considerable severe
weather across KS, OK, and north TX, but there were no tornadoes reported.  Most
of the reports were of the wind damage and moderately large hail variety.

The warm sector of the system was complex, with suggestions of short waves ro-
tating around the base of the trough.  This structure may have been caused by
the active convection rather than the convection beingf caused by the "ripples."
The high lapse rates over the southern states were being processed rapidly by
the convection, but persisted to the east of the active convection.  The very
cold air aloft resulted in residual instability behind the trough, but with no
residual moisture, nothing of significance developed with this instability.

	Doswell