Probabilistic Heavy Snow and Icing Discussion NWS Weather Prediction Center College Park MD 423 AM EDT Fri Apr 24 2020 Valid 12Z Fri Apr 24 2020 - 12Z Mon Apr 27 2020 ...North-Central Rockies... Day 1... A shortwave trough digging southeast along the leading edge of a 110kt Pacific jet streak will dive into the Central Plains this evening bringing an end to the regional forcing for ascent. The strongest ascent through this afternoon will be associated with the LFQ of the upper jet and collocated height falls, which are expected to be focused in the CO Rockies. Moisture across the region is modest, but the forcing should wring out precipitation efficiently, and this will be snow above generally 7000 ft. High probabilities for 4 inches are confined to a small portion of the CO Rockies, with lower probabilities extending from the southernmost Absarokas of MT, to as far SE as the Front Range in CO. ...Northeast... Day 3... A shortwave trough swinging across the Ohio Valley Saturday will close off early on Sunday before lifting towards New England late on D3. A surface low beneath this feature will occlude out to secondary low development near the Virginia Tidewater, and this low is expected to then lift rapidly to the E/NE, with this double-barreled structure forecast to move south of New England towards Monday morning. Outside of the GFS/GEFS which are displaced NW and warm, the remaining guidance is pretty well clustered around this solution. As some modest coupled jetting develops, the primary surface low should intensify, which when combined with Canadian High pressure over Ontario will allow cold air to funnel southward into New England. While the column may initially be marginal for anything but rain, as the latter half of D3 develops, increased forcing and column cooling is likely to cause a p-type changeover from rain to snow. First this will occur in the terrain, and by the end of the forecast period, snow is possible even down into the valleys if forcing is strong enough to cause dynamic cooling of the lowest levels. The heaviest snow is likely in the higher elevations, generally above 2000 ft, in the southern Adirondacks, Greens, and Whites, and WPC probabilities in these areas suggest a low chance for 6 inches. Moderate WPC probabilities for 2 inches extend into most of the other terrain including the Catskills and Berkshires. The evolution of this system will need to be monitored as late season snow is possible even into the lower elevations of New England, upstate New York, and into parts of northern PA. For Days 1-3, the probability of significant icing (0.25-inch or greater) is less than 10 percent. Weiss