I can't conclude anything without seeing the time-scale evolution. However, I did look at a time-loop of WSR-88D base reflectivity for April 20 and noticed very small scale convection. There are very small (spatially) returns of >40dBZ just off the coast of Delaware. I personally would guess it to be a fully condensed updraft. Note the wider condensation base at the surface. Now as to explain this theoretically, perhaps a cross between lake-effect and vertical instability. Synoptic maps show a closed low overhead. Put relatively warm ocean water under cold environments and you get lake/ocean effect. Unlike lake-effect, CSI was not the player but instead vertical instability by itself.