As of this writing we have a deepening surface cyclone slowly lifting northeast across southern Quebec province. This is aiding in a northward progression of rich low-level theta-e air with strengthening wind fields in response. There is also a plume of modified elevated mixed-layer air moving across the region. In closer proximity to the surface cold front and surface trough, numerous thunderstorms have developed across upstate New York with mixed modes containing discrete cells and the organization of a squall line. The environment is plenty conducive for numerous strong-to-severe thunderstorms containing damaging winds and/or large hail with the potential for a few tornadoes. In addition, combination of upscale linear growth with slow southeast advancement as the system becomes parallel to the upper-level flow will result in long-duration torrential downpours yielding the risk for flash flooding - perhaps significant in some spots.
As we move deep into the evening, this line should advance across New England, however, as we will lose the diurnal heating this line will be weakening. Enough wind shear and elevated CAPE will keep the low probability for some localized severe weather into the overnight.
Given the system becoming parallel to the upper-level flow, the progression of the cold front will slow. This is starting to become better identified within forecast model guidance. This will likely allow the development of numerous showers and thunderstorms Friday. While the environment will not be as prime as it is today, the risk for strong-to-severe thunderstorms with al hazards will be in place. Flash flooding will also be possible Friday and some significant flash flooding is possible.