A remnant QLCS is emerging east of the Appalachians,
where it is showing some early signs of re-intensification. Farther
east, a disorganized band of thunderstorms is also evolving over
parts of western VA into NC. While overall convective evolution is
not clear, these storms will continue spreading eastward into a
destabilizing air mass (around 500-1000 J/kg MLCAPE). Despite the
somewhat limited buoyancy, strong low/deep-layer shear characterized
by clockwise-curved low-level hodographs (see GSO 12Z sounding) will
favor a mix of organized line segments and supercells, with a risk
of damaging wind gusts and a few tornadoes (some potentially
strong). A watch issuance is likely for this activity.