NAM comes in hot and heavy. 18z R/S line is about DCA and then it blows north by 21z. In that period, however, there is ~0.5” precip. The longer that the transition holds off, the better we can do on the front end.
The problem, though, is that it really comes together so late that we don't get a huge benefit from it sliding to our S anyway. Without the 850 low cranking up earlier, we are just awash in warm air advection.
3k tracks the low west of Norfolk too.
Problem is that the 850 low runs north of DC.
There is a realistic potential that areas inside the DC Beltway get non-accumulating snow on the front end and miss the deformation on the back end. Trace is absolutely in play.
I think for Staunton down to Roanoke, it is simply a matter of this being a later developer. One way to visualize is to go to: https://weather.cod.edu/forecast/
Choose the GFS, and then under precipitation go to the 24 precip accumulation. You can see that tomorrow's system is a fully formed event with a nice stripe of precipitation coming from MS/AL/TN. Whereas Wednesday's storm really doesn't all come together until it is on top of us.
Agree. I don't see a lot of front-end love for the 95 corridor before it flips, but if we can get some deformation band help that will soften the blow of missing this one. I'm personally always a bit worried that the band will set up in the more favorable (cough, MD) areas.
Nice visualization from CoolWx for the GFS. You have Omega (effectively upward motion), -12 and -18 °C contours to highlight the dendritic region, and the freezing line.
http://coolwx.com/cgi-bin/getbufr.cgi?region=VA&stn=KDCA&model=gfs&time=2020121306&field=omega