INITIALLY SOME OF THIS ACTIVITY SHOULD BE
DISCRETE, YIELDING FAST-MOVING SUPERCELLS, SOME LEFTWARD/
ANTICYCLONIC, WITH LARGE HAIL. POTENTIALLY SIGNIFICANT AND
DESTRUCTIVE HAIL OVER 2 INCHES IN DIAMETER IS POSSIBLE OVER THE
NEWLY OUTLINED AREA, GIVEN THE STRONG SHEAR, EARLY SUPERCELL MODES,
STEEP LOW/MIDDLE-LEVEL LAPSE RATES, AND FAVORABLE INFLOW-LAYER WATER
CONTENT. A FEW TORNADOES ALSO ARE POSSIBLE, ALONG WITH SEVERE
GUSTS.
STEEPENING MIDLEVEL LAPSE RATES AND MOISTENING BOUNDARY LAYERS,
WARMED BOTH BY WARM ADVECTION AND MUTED DIABATIC HEATING, WILL
REMOVE MLCINH AND YIELD SURFACE-BASED INFLOW PARCELS WITH MLCAPE
500-1000 J/KG IN CENTRAL NM, AND 1000-2000 J/KG OVER SOUTHEASTERN NM
DOWN THE PECOS VALLEY. STRENGTHENING WINDS ALOFT (AS NOTED ABOVE)
WILL YIELD EFFECTIVE-SHEAR MAGNITUDES 55-75 KT ACROSS THAT CORRIDOR.
MEANWHILE, VEERING FLOW WITH HEIGHT SHOULD CONTRIBUTE TO 200-400
J/KG EFFECTIVE SRH, LOCALLY HIGHER.