Excessive Rainfall discussion for the MA from WPC-
Activity on Thursday was widespread and quasi-organized on larger scales. On Friday we may see lesser coverage and/or lesser longevity of individual storm clusters, as the upper trough continues to fill, experiencing height rises at its base over the Ohio Valley and mid Atlantic today. Sufficient heating of the still tropical airmass, however, is likely to lead to scattered initiation along sea breezes, over the mountains, and near a quasi-stationary front and inverted surface trough sitting over DE/MD/PA. Hi-res model consensus places the greatest concentration of rainfall over Maryland and southern PA to southern NJ, thus near and north of the surface front where both mid level and jet level forcing should contribute to somewhat greater lift compared to areas farther south. Models generally agree, and especially the various HRRR runs, that a flash flood threat could develop early in the morning as the tail end of a jet entrance region interacts with the CAPE gradient north of the front in Pennsylvania. Coverage of storms will then increase elsewhere by midday, with HREF odds of inch per hour rates peaking after 22Z in MD/DC/VA. The environment and model signal certainly support local rain rates nearing 2 inches per hour. Much of this region is quite saturated, to say the least, in the wake recent widespread heavy rain events. Once again, a lack of sustained forcing and the expectation of lesser coverage today is what keeps this event in the Slight Risk category, but wherever multi-inch rainfall occurs in urban areas or other sensitive basins, an isolated significant flash flood is possible.