On all of the runs that were crushing my area around 495 (and other interior SNE folks east of the river), the southern stream was stronger so it was the focal point of baroclinicity even up at the 850 level. The trend today was decidedly weaker with that southern stream vort and the northern stream decided to slice in a bit quicker too…so it was forcing the baroclinic zone further NW, and we saw that with that shape of the sfc low too looking almost like an IVT extending into SE NY. Mid-levels responded too with a more SE flow look whereas those runs with the southern stream being stronger and making the wider turn, the midlevel flow was turning more out of the east quicker which of course shuts off the WAA faster.