GIVEN THE ENVIRONMENT, STRONGEST STORMS WILL BE CAPABLE OF PRODUCING
VERY LARGE HAIL, WITH AT LEAST SOME UPSCALE CONVECTIVE GROWTH
THROUGH THE EVENING CONTRIBUTING TO POTENTIAL FOR DAMAGING SURFACE
GUSTS. TORNADIC POTENTIAL REMAINS MORE UNCLEAR, DUE TO THE FORECAST
VEERED NATURE OF THE LOW-LEVEL WIND FIELDS, AND RESULTANT LACK OF
MORE PRONOUNCED CLOCKWISE TURNING WITH HEIGHT IN THE LOW-LEVEL
HODOGRAPHS.