Scattered thunderstorm development will be possible along/ahead of
the front from the Carolinas/Mid Atlantic into New England during
the afternoon. Wind fields will generally be stronger with northward
extent. Depending on the extent of destabilization, supercells and
organized clusters will be possible across parts of New England and perhaps the northern Mid Atlantic, which would pose some threat of
all severe hazards. Farther south into the southern Mid Atlantic and
Carolinas, deep-layer shear will be weaker, but favorable low-level
moisture, strong buoyancy, and modest midlevel southwesterlies will
support outflow-driven clusters capable of damaging winds and
possibly some hail. The organized severe threat will tend to decrease with southwestward
extent, due to weaker deep-layer flow. However, favorable low-level
moisture and buoyancy could support a few strong to locally severe
storms along the trailing cold front into parts of the Southeast
during the late afternoon and evening