nickgrillo
EF5
Widespread thunderstorms are now initiating near the warm front as large-scale ascent associated with amplifying mid-level shortwave begins to move into moistening/destabilizing warm sector. Currently elevated thunderstorms should become rooted in the boundary layer as effective inflow parcels begin to become surface-based or at least NEAR surface-based as forcing for ascent continues to remove large amounts of CINH. Increasing low-level WAA and moisture advection northwasrd (associated with 50-60kt SW LLJ) and steepening mid-level lapse rates associated with the intense mid-level trough is contributing to increasing MLCAPES of 250-500j/kg across the area... BL-6km shear supports supercells (with at least 40-50kt deep shear) while extreme low-level shear supports potential for tornadoes (including a strong tornado or two across western KY/southern IN by the mid-morning) with any sustained storms (0-1km SRH at least 450m2/s2).
A start of a great day...
A start of a great day...