This feature is very interesting and I have never seen anything like this. A upper level low veers and comes on the back side of a storm system on that's on the Northeastern coast. The core of the upper level low is very cold, a minimum of 516/522 thickness value. 850 temps low as -15c (5f)
With 850mb temps being that cold, there would be snow growth. So, this ULL can bring flurries and snow showers for a good portion of the southeastern states. If there would be an increase of moisture associated with this ULL, this thing would bring considerable amounts of snow. Right now, the GFS is showing that the moisture would be minimal with this ULL feature. I'm not sure why the moisture content is minimal, perhaps it's due to the very dry air that would be in place.