Probabilistic Heavy Snow and Icing Discussion NWS Weather Prediction Center College Park MD 300 PM EST Sat Feb 12 2022 Valid 00Z Sun Feb 13 2022 - 00Z Wed Feb 16 2022 ...Great Lakes... Days 1-3... Persistent mid-level troughing across the Great Lakes will maintain favorable CAA for LES across the lakes, with enhanced ascent possible at times through weak PVA as shortwaves rotate through the mean flow. On D1, mean northerly flow combined with some land breeze confluence across Lake Michigan should pivot a band of snow along the eastern shore of the lake into parts of SW Michigan. The DGZ is quite shallow and forcing is modest, but WPC probabilities suggest a moderate risk for 4+ inches before flow becomes more westerly and dries out to bring an end to the LES. Late D2 into D3, a potent shortwave moving across the eastern Great Lakes will be followed by more impressive CAA and unidirectional westerly flow across Lake Ontario and Lake Erie. With deepening inversion depths and an impressive DGZ, snowfall rates may become intense, especially east of Lake Ontario, with upslope enhancement into the Tug Hill aiding in snow accumulations. WPC probabilities for 4+ inches are already above 80% in the Tug Hill, with high probabilities also present for more than 8 inches. Lake Erie is almost entirely ice covered according to GLERL data, so LES will be much more muted east of that lake on D3. ...Mid-Atlantic/Northeast... Days 1-2... Shortwave pivoting through a longwave trough across the eastern CONUS will produce height falls and PVA across the Mid-Atlantic and Northeast. At the same time, a poleward arcing jet streak intensifies into New England placing favorable RRQ diffluence across the east coast, with a secondary jet streak producing some coupled ascent late on Sunday. The overlap of these forcings will drive modest cyclogenesis along the coast from VA to off Cape Cod, with moist advection producing an expanding area of precipitation NW of this feature. For D1, the primary ascent mechanism across the Mid-Atlantic will be enhanced fgen through the sharpening baroclinic gradient behind a surface cold front, combined with the ageostrophic response of the upper jet streak. While the best ascent may be just beneath the DGZ, it still appears favorable for some brief heavy snow rates approaching 1"/hr, with the best chance in the higher terrain near Shenandoah NP and the Allegheny Front. Here, WPC probabilities for 4+ inches are more than 50%, with local maxima above 6" likely. Further to the northeast along the I-95 corridor from Washington, D.C. to Baltimore and Philadelphia, 1-2" with locally heavier amounts are possible. Into D2, as the low pressure deepens modestly off the coast and lifts northeast, precipitation will spread into New York and New England. This wave of low pressure will help enhance ascent which will already be robust through the coupled jet streak and enhanced fgen, but the rapid motion of the system will somewhat limit accumulations. However, guidance suggests an inverted trough will try to linger back into southeast MA, with some OES possible into the Cape and Islands as well. WPC probabilities for 4+ inches are more than 50% southeast of Boston near Plymouth, MA, but are generally 10-30% elsewhere from eastern Long Island through the immediate coast of Maine. ...Pacific Northwest through Northern Rockies... Days 2-3... A potent closed low will dive out of the Gulf of Alaska D2 and shift across the Pacific Northwest before sharpening over the Great Basin Tuesday evening. This feature will create robust height falls and drive a cold front and at least subtle waves of low pressure southeast across the area. The elongating upper trough will drive coupling of dual jet streaks across the Great Basin by D3, further enhancing ascent as moisture begins to increase into the region. Ascent on D2 is likely to be modest, but should increase dramatically as the synoptic forcing begins to overlap on D3. For D2, the heaviest snowfall is likely to be confined to the WA and OR Cascades, and generally above 5000 ft, although lowering with time as the front digs southeastward. This should prevent any significant accumulations at the Cascade Passes, with WPC probabilities for 6 inches only above 20% in the far northern Cascades and around Mt. Rainier. For D3, the moderate to heavy snow will shift eastward into the Absarokas, Northern Rockies, and ranges of NW WY. Once again, snow levels will initially be around 5000 ft but will fall to around 3000 ft behind the cold front, and WPC probabilities for 6 inches are confined to the higher terrain of these ranges. For Days 1-3, the probability of significant icing is less than 10 percent. Weiss