Good synopsis from Mount Holly this morning-
00Z Guidance retains rather impressive run-to-run consistency with respect to timing, track, and associated thermal profiles with the low, and this is perhaps helped by the progressive hemispheric pattern which tends to favor more predictability than amplified blocking patterns. Consequently despite considerable uncertainty regarding the details of this system (more on that below) do have higher than average confidence that at least portions of our area will see potentially significant impacts from this system. The one thing to point out is that the mid-lvl wave associated with this system is still over the Pacific which does favor at least some caution in becoming too confident although modern Data Assimilation is fairly robust even in regions of observational sparsity.
Unfortunately (or fortunately if you look at it from my perspective) it is too early to get specific about ptypes and snow amounts, as the low`s track near to the coast will almost certainly result in some ptype transition zone. Furthermore this transition zone will likely ebb and flow as mesoscale lift (e.g. FGEN) results in dynamical cooling. That being said the antecedent airmass does look primed for wintry precipitation, with pre-storm dewpoints likely in the single digits or low- teens which should support some fairly notable wet-bulbing with the first batch of precip. The question then becomes can the intensity of the precipitation and associated dynamical cooling become enough to offset the increasing warm advection associated with the low? The next question is how robust will precipitation be on the back side of the low Wednesday night as it pulls away from the area, and cold advection begins? We should have more answers to these questions in the next couple days we enter the Mesoscale model window.