Probabilistic Heavy Snow and Icing Discussion NWS Weather Prediction Center College Park MD 414 AM EST Tue Dec 10 2019 Valid 12Z Tue Dec 10 2019 - 12Z Fri Dec 13 2019 ...Great Lakes... Days 1-3... Low pressure lifts away through eastern Canada today, leaving strong CAA in its wake. This CAA moving across the Great Lakes will produce periods of moderate to heavy Lake Effect Snow (LES) on W to NW flow. The moisture is shallow, but forcing is robust and prolonged with steep lapse rates and an 8kft inversion height. The heaviest snow on D1 /Tuesday/ is likely in the Keweenaw Peninsula where Lake Superior fetch and upslope combine, as well as NW parts of the L.P. of MI where the effective fetch length increases due to pre-saturation off Lake Superior. WPC probabilities on D1 are low to moderate for 6 inches. By day 2, the flow becomes more westerly, and the favored snow belt regions downwind of Erie and Ontario feature the highest WPC probabilities, which are high for 4 inches. On D3 /Thursday/ a clipper and associated jet streak will race southeast from central Canada and towards the Great Lakes. The combination of a very cold column, jet level diffluence, and subtle height falls will produce a swath of moderate snow despite rapid progression of this system to the east. WPC probabilities are moderate for 4 inches in northern WI and the U.P. of Michigan. ...Tennessee Valley through New England... Days 1-3... A strong cold front crossing the northeast and down through the southeast will bring much colder air to these regions Tuesday and Tuesday night. As this occurs, precipitation within a divergent region ahead of a southern stream shortwave will continue to spread northward in an anafrontal precipitation setup. Initially, the precipitation will all be rain, but as strong CAA continues the column will cool and p-type will transition to snow late Tuesday in the Southeast, and early Wednesday into the Northeast. While antecedent temperatures are very warm, and rainfall will be widespread Tuesday, some snow accumulation is likely. This is due to the likelihood for intense snowfall rates as a robust stripe of 7000-600mb fgen collocated with the RRQ of a 170+kt upper jet streak to produce intense and deep layer ascent into the cold air. The dynamic cooling of the column associated with heavy precipitation will further enhance snowfall possibilities, and HREF probabilities for 1"/hr have increased. The duration of forcing and cold enough temperatures overlap is short, so total snowfall should be limited. However, a few inches of snow are possible as evidenced by WPC probabilities for 4 inches eclipsing 20% in the terrain of WV/VA, with 10-20% across southern New England. In the I-95 corridor, a burst of heavy snow is likely, potentially coinciding with Wednesday morning rush hour. While the ground will be warm, heavy snow should overcome this briefly, and WPC probabilities for 1" are as high as 50% for the urban corridor. A secondary band of precip is progged by CAMs to cross the TN Vly later this evening. This precip is mainly snow over TN, but mainly ice on the higher portions of Smokey Mountains. This raises the risk for a quarter inch of ice on those peaks to 10% tonight. On day 3, a more pronounced southern stream low pressure may blossom and spread precipitation from the Gulf of Mexico atop a wedge of surface high pressure Thursday night. With cold surface temps, especially in the western Carolinas and SW VA, the precipitation may begin as freezing rain. There remains quite a bit of spread in guidance in the thermals, but some freezing rain is likely, and WPC probabilities for 1/4" are as high as 20%. ...Pacific Northwest... Days 2-3... Prolonged and robust Pacific Jet streak will angle into the Pacific Northwest beginning Wednesday. This jet streak will drive significant moist advection into the West, with small perturbations embedded within the zonal flow accentuating synoptic lift. Periods of heavy snow are likely on day 2 in the Washington Cascades, with widespread heavy snow spreading eastward as far as the Colorado Rockies and all ranges in between as the nose of the jet shifts eastward. WPC probabilities feature a high risk for 12 inches from the Washington Cascades and Oregon Cascades, into the Sawtooth, Northern Rockies, and Grand Tetons, with snow levels as low as 1000 ft near the Canada border, to as high as 5000 ft in Colorado. Total 2-day snowfall could eclipse 4 feet in the Washington Cascades, with more than 2 ft possible in the other highest terrain. Weiss