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February 3-4 significant icing event for the interior, some sleet/snow possible. Coast mostly rain.


NJwx85
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CAA on a northerly flow is notorious for abrupt temperature drops along the HV and points south. Consider the topography of the Hudson River and the relatively unimpeded flow for air to funnel south. In contrast, when CAA is on a northwesterly flow, it must traverse higher elevations of the Catskills/Poconos, and points NW, leading to a more gradual transition, often with drying/downsloping. 

This is a classic Hudson Valley FROPA for the area - it's almost like a backdoor coldfront.

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