Probabilistic Heavy Snow and Icing Discussion NWS Weather Prediction Center College Park MD 307 PM EST Wed Jan 13 2021 Valid 00Z Thu Jan 14 2021 - 00Z Sun Jan 17 2021 ...Upper Midwest... Days 1-2... A potent trough digging out of western Canada will evolve into an anomalously deep upper low across the Midwest Thursday night and then stall briefly, before ejecting to the east/northeast into Saturday. As this upper low deepens, a potent jet streak will rotate through the base of the amplifying longwave trough, and the combination of the diffluent LFQ of this jet streak with height falls and PVA will produce a surface low over WI Thursday night, which will then pivot nearly in place, possibly retrograding SW briefly into Friday before lifting away through D3. Two rounds of precipitation will accompany this feature, with moderate to heavy snow likely, as well as some light freezing rain. Round 1 will involve a period of WAA precipitation spreading eastward ahead of a cold front as mid-level flow backs to the SW and divergence supplies ascent. As the precipitation expands northeastward, the WAA aloft will drive a warm nose atop cold surface temperatures. This suggests, and there exists good model consensus on this, that a narrow band of freezing rain is likely to move eastward which may accrete a few hundredths of an inch from central MN through eastern IA and much of WI. As the cold front pushes eastward and forcing begins to intensify, precip may mix with or transition to snow, but accumulations on D1 are likely to be primarily light, with WPC probabilities for 4 inches less than 30%. Round 2, which will lag significantly from Round 1 in some places, but may just evolve in place across eastern MN and WI, is expected to be more significant. As the upper low closes off and stalls, spokes of vorticity will rotate cyclonically around it. The interaction of these features will lead to some enhanced mid-level deformation, which is evident on most of the guidance which has come into better positional agreement this aftn. At the same time, a ridge of higher theta-e air (TROWAL) will rap all the way around the upper low and drop southward across MN, coincident with some WAA from the north (an indicator of how wrapped up this system becomes). While the overall column cools, the combination of the TROWAL, deformation axis, and mid-level WAA will produce briefly intense ascent, but also deepen the DGZ while driving an isothermal layer within the DGZ. This could enhance SLRs across parts of MN and into northern IA, and snowfall forecasts have increased this aftn. While most of the snow will likely be light to moderate, a long duration of snow combined with at least periods of heavier snow has led to WPC probabilities increasing for the area. There is now a high risk for 6" from just north of the Twin Cities southwest into the Coteau des Prairies and the Buffalo Ridge. It is this area that has the best potential for some heavier snowfall, and a longer duration of pivoting snowfall, and local amounts to 10" are possible. Elsewhere, WPC probabilities are moderate for 4 inches surrounding the higher 6" probs, and extending into the U.P. of Michigan. ...Central Appalachians and Northeast... Day 3... The closed low from the Midwest will broaden and begin to lift east/northeast Friday into Saturday, spreading waves of precipitation eastward both along the front and associated with vorticity impulses rotating around the gyre. The primary surface low is expected to occlude over Michigan, with a secondary wave developing along the triple point to the east near New England. Height falls to steepen lapse rates beneath the mid-level vortex will combine with waves of energy to produce periods of snow showers over the Central Appalachians, with increasing NW flow driving upslope flow into the favored windward slopes of WV and PA. WPC probabilities are low for 4" on D3. Further east, precipitation spreading northward on WAA ahead of the secondary low will move across upstate NY and New England. Much of this precipitation is expected to be rain, or briefly snow changing to rain, except in the terrain of the Adirondacks, Greens, and Whites, where snow levels may rise above 3000 ft. Above these levels, especially in the White Mountains, heavy snow is likely. WPC probabilities are high for 4 inches in the Adirondacks and White Mountains of NH. For Days 1-3, the probability of significant icing (0.25-inch or greater) is less than 10 percent. Weiss