The exact position of the surface low didn’t end up mattering as much as the upper air features. The 850 low, which is both broad and late developing, is basically over DC allowing the warm air to flood in. We always want an 850 track to the south of DC by a fair margin.
Really impressed with the staying power of the snow. At least .75” liquid on top of 1.5” of snow and it is largely still around. There is still snow on our lighter colored car (not the darker one).
It looks like the two low situation is due to a meso-low from the NC thunderstorm complex on the 3km NAM. Not sure that it plays a huge role in the thermal profile up by us.
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.