Probabilistic Heavy Snow and Icing Discussion NWS Weather Prediction Center College Park MD 354 PM EST Sun Feb 17 2019 Valid 00Z Mon Feb 18 2019 - 00Z Thu Feb 21 2019 ..Lower Great Lakes and PA to the Northeast... A mid to upper level trough is expected to move east and gradually deamplify as it moves east across New York/PA and New England. Low to mid level theta-e advection and frontogenesis supports a stripe of light to moderate snows extending from the lower Great Lakes to New York and southern New England on Day 1. A second low pressure center develops south of New England near the 40n 70w benchmark, resulting in an enhanced frontogenesis and locally higher amounts in southeast New England. A wintry mix is expected further south with light icing possible in northeast Ohio and much of PA and northwest NJ, southeast NY and southern CT. The warm advection turn snow over to mixed sleet/freezing rain from Long Island NY to southern CT, RI, and adjacent southern coastal MA. ...Southwest to the Southern Rockies... Tonight into early Monday, shortwave energy moving into the base of a broad upper trough centered over the southwestern U.S. is expected to support significant snowfall totals from higher elevations of the mountains of Southern California, where amounts have increased today in the proximity of the 30 mb jet crossing the ranges this evening, downstream into the mountains of AZ northeast into southern UT and southwest CO. Bolstered by low to mid level frontogenesis favorable difluence aloft, some of the heaviest two day totals are forecast to focus along the Mogollon Rim into the White Mountains of central Arizona, as well as the San Juan and Sangre de Cristo mountains in Colorado and New Mexico. On day 2, the upper trough crosses AZ into NM, with persistent upper divergence in the ranges of NM favoring continued snows the first half of the period before ending as the upper trough moves out on to the Plains. 2 day totals of 1-2 feet are expected. Additional light accumulations are expected to continue across portions of the central and southern Rockies into late Tuesday, diminishing by early Wednesday as the upper trough lifts northeast into the Plains. ...Central Plains into the Lower Missouri and Mid-Upper Mississippi Valleys and adjacent western Great Lakes... Probabilities for significant snows increase across the region late Tuesday through Wednesday as the upper trough ejects east northeast from the Rockies into the central Plains. As the 700 mb low treks east across CO, downstream southerly flow provides warm/moist advection and convergence on the high plains of Co to adjacent KS/NE Mon night to Tue. As the low moves northeast on Tue, the swath of warm/moisture advection moves across the rest of KS/NE into IA Tue night and then northern IL and WI on Wed. Several inches of snow are expected from eastern NE across northwest MO, IA, and then southwest WI. The models still differ as to how far west the snow axis extends in NE/SD/MN. Probabilities indicate a Moderate to High Risk for accumulations of 4-inches or more on day 3 across Iowa and adjacent MO/NE/MN/WI. ...Southern and Central Appalachians Day 3... As as strong area of high pressure shifts east into the Northeast, models show a well-defined cold air damming signature developing over the East. Strong low to mid level theta-e advection and convergence ahead of the trough moving into the central U.S. will support precipitation spreading north over this shallow dome of cold air, producing mixed precipitation with the potential for several inches of snow followed by sleet and then significant ice accumulations across the region late Tuesday night into Wednesday. WPC Day 3 probabilities indicate a Moderate Risk for snow accumulations of 4 or more inches in eastern WV/western VA and ice accumulations of 0.25 inch or more extending from western North Carolina into western Virginia to eastern West Virginia. ...Pacific Northwest... After a respite, the next upper level jet maxima dives southeast from the northeast Pacific into OR around 12z Wed according to the ECMWF, reaching northern CA thereafter. This places the Wa/Or Cascades into the favored left exit region of the upper jet. The models show 700 mb convergence maxima, aiding upslope flow in producing a sustained period of snow. The longer duration lift could lead to locally heavy snow in the southern Wa Cascades, OR Cascades, and then the Blue Mountains. Petersen