Both models trended deeper with the mid-level cyclone, developing a closed low by 06 UTC on the 23rd.
Both models trended deeper with the surface low, with little difference in intensity (988 mb) or location (southeast of Long Island) by 06 UTC on the 23rd.
The Eta continued to have more QPF, farther north than the GFS, possible due to slightly stronger mid-level frontogenesis, and a stronger lower branch (southeasterly flow) of the resulting circulation.
The best banding signals in our area appeared to be over northeast Pennsylvania and southern New York around 00 UTC on the 23rd.