Dangerous Surf and Rip Currents Along East Coast Beaches; Hazardous Heat in the West

Tropical storm conditions, storm surge flooding and coastal flooding will continue into Thursday across the Outer Banks and into portions of the Mid-Atlantic coastline. Life-threatening rip currents and high surf will continue to impact much of the Atlantic shoreline through the end of the week. Hazardous, record heat will continue across the Western U.S. through the weekend. Read More >

November 5, 2007
The Mini-Supercell / Marginal Hail Event of November 5, 2007

Overview: A quick-moving cold front moved across the ILN CWA during the afternoon of 11/5/07. A cool late-autumn airmass was in place ahead of the front (temperatures in the upper 50s and lower 60s), which inhibited any surface-based instability. However, very weak elevated instability existed above the stable boundary layer (MUCAPE <500 J/Kg lifted from 800 hPa). In addition, shear ahead of the front was high, with 0-6 km shear around 60 kt, and 0-3 km helicities ranging from 250-500 m²/s².
As the front entered ILN's CWA, numerous thunderstorms developed and quickly took the form of elevated mini-supercells. The cores of the storms were small and were generally confined to below 15,000 feet, and none of them extended above the -20 °C level. However, many of the storms exhibited weak midlevel rotation, and almost all storms with rotation ended up producing severe hail. The high 0-3 km helicity favored midlevel mesocyclones, which led to significantly stronger dynamically-induced updrafts. The air mass in place was cool and freezing levels were low, so these meso-induced updrafts grew within the hail-growth zone of -10 to -30 °C, and large hail was the result. Because of the low freezing levels, hail was able to make it to the surface without much melting.