Probabilistic Heavy Snow and Icing Discussion NWS Weather Prediction Center College Park MD 348 AM EST Wed Dec 23 2020 Valid 12Z Wed Dec 23 2020 - 12Z Sat Dec 26 2020 Day 1... ...Central Plains to the Upper Midwest... After several runs of struggling to reach a consensus, the 00Z model runs have moved into better agreement -- offering a strong signal for moderate to heavy snows developing from eastern Nebraska and southeastern South Dakota to northwestern Minnesota, northwestern Wisconsin and the western U.P. of Michigan. A powerful surface low centered over South Dakota this morning is forecast to move into the upper Mississippi valley later this morning. As a well-defined shortwave moving through the base of the associated upper trough begins to lift northeast from the central Plains into the upper Mississippi valley, a developing comma head of moderate to locally heavy snow is expected to develop on the west side of the low. Low-to-mid level frontogenesis is expected to help support banded precipitation, with the 00Z HREF showing several members suggesting snowfall rates of 0.5-1 in/hr within these bands as they move east across the region on Wednesday. This snowfall along with strong, gusty winds is likely to result in reduced visibilities and blizzard conditions across portions of the region. Latest WPC PWPF indicates high probabilities for accumulations of 4-inches or more extending from northeastern Nebraska and eastern South Dakota to northwestern Minnesota and the western U.P. Within this area, high probabilities for 8-inches or more extend from south-central Minnesota to northwestern Minnesota and the western U.P. Some of the highest probabilities center along the Wisconsin and western U.P. shores of Lake Superior, where in addition to the synoptically driven snows, northerly flow on the backside of the system may provide some lake-enhanced totals. Day 2... ...Ohio Valley/Central Appalachians/Great Lakes... As the previously noted low moves north of the Upper Great Lakes, a sharp trailing cold front is forecast to move east across the Ohio and Tennessee valleys on Thursday. Rain changing to snow before precipitation ends is expected to produce mainly light snow accumulations across the lower Ohio and Tennessee valleys through Thursday. Then by Thursday afternoon, as a well-defined shortwave begins to move through the base of the associated upper trough, surface low pressure is forecast to develop and move north along the front into the central Appalachians -- raising the potential for significant snows to develop back in the cold air. While there is some uncertainty in the details given the timing of the cold air, significant accumulations look likely across portions of the southern and central Appalachians and Ohio valley Thursday night into early Friday. As a new upper low begins to develop over the Ohio valley, surface low pressure will continue to intensify as it moves north through the upper Ohio valley and Lower Great Lakes region early Friday. As the low moves north of the Lakes, northerly flow behind the departing system will support lake effect snow bands developing off of Lake Erie into northwestern Pennsylvania and northeastern Ohio Friday morning. Meanwhile, northwesterly flow across the Upper Great Lakes will support developing lake effect snow bands, with locally heavy accumulations likely across portions of the western and central U.P. of Michigan and along the eastern shores of Lake Michigan. Day 3... ...California and the Pacific Northwest... Following a few days of dry weather, precipitation is expected to return to the region late Friday into early Saturday. Models show a deepening surface low tracking northeast toward Vancouver Island with an occluded front moving inland across the Northwest and Northern California Saturday morning. A well-defined mid level shortwave/upper jet moving through the base of the associated trough is expected to support organized heavier precipitation across Northern California, including significant snows from the Klamath Mountains to the Sierra. For Days 1-3, the probability of significant icing (0.25-inch or greater) is less than 10 percent. Pereira