Wpc
An area of low pressure developing across the Mid-Atlantic will lift northeast Thursday along a slowing cold front. This low will strengthen in response to rapid height falls as an anomalous mid-level trough advects east from the Great Lakes, and an intensifying divergence maxima within the RRQ of an upper jet streak. Large scale ascent will spread precipitation across the Mid-Atlantic and Northeast, but WAA ahead of the front suggests all precip will be rain initially. However, as the low deepens and the cold front drops slowly southeast, the column will cool rapidly to allow a p-type transition from rain to snow. This is likely to be additionally enhanced by robust fgen/deformation NW of the low. While there remains uncertainty into how much precip will occur as the column cools enough for snow, this enhanced ascent through the fgen should provide at least a burst of snowfall, enough to overcome the antecedent rain and warm conditions, especially in the terrain. WPC probabilities for 4 inches are as high as 30-40% in the Adirondacks and Tug Hill where post frontal upslope flow will enhance snowfall, and 10-20% across much of Upstate New York and into Vermont.