Newest day 3
THERE REMAINS NOTABLE SPREAD WITHIN THE LATEST MODEL OUTPUT
CONCERNING THE FRONTAL PROGRESSION AND WHERE THE STRONGER FORCING
FOR ASCENT DEVELOPS WITH THE EVOLVING WAVE. A CONGLOMERATE
CONVECTIVE OUTFLOW BOUNDARY MAY ALSO INITIALLY PRECEDE THE FRONT
ACROSS THE NORTHERN GULF COAST STATES THROUGH ARK-LA-TEX AT THE
OUTSET OF THE PERIOD. EVEN SO, GUIDANCE SUGGESTS THAT A CORRIDOR OF
MODERATE TO STRONG POTENTIAL INSTABILITY WILL AGAIN DEVELOP ALONG
THE FRONTAL ZONE ACROSS PARTS OF THE SOUTHERN GREAT PLAINS INTO MID
SOUTH, AND PERHAPS NORTHEASTWARD THROUGH PORTIONS OF THE OHIO
VALLEY. AIDED BY FAVORABLE VERTICAL SHEAR NEAR THE SOUTHERN FRINGE
OF THE WESTERLIES, THIS ENVIRONMENT COULD BECOME CONDUCIVE TO THE
DEVELOPMENT OF SUPERCELL STRUCTURES AND ORGANIZING CLUSTERS WITH
POTENTIAL TO PRODUCE DAMAGING WIND GUSTS, LARGE HAIL AND PERHAPS A
RISK FOR TORNADOES.