Probabilistic Heavy Snow and Icing Discussion NWS Weather Prediction Center College Park MD 420 AM EDT Thu Mar 21 2019 Valid 12Z Thu Mar 21 2019 - 12Z Sun Mar 24 2019 ...The West... Days 1-3... An active pattern returns to The West as two mid-level impulses bring widespread mountain snow from the Sierra, to the Cascades, the Northern Rockies, and southward through Colorado and into New Mexico. The first of these impulses is a potent negatively tilted shortwave lifting onto the California coast this morning. This will be accompanied by a modest Pacific Jet and moist advection, with height falls and jet level diffluence producing heavy snowfall from the Great Basin eastward into the Southern Rockies. The heaviest snow Day 1-2 is expected in the Sierra, as well as the San Juans of Colorado where upslope flow is enhanced as 700mb flow becomes due south around the elongated trough. WPC probabilities show a high risk for 12 inches in the San Juans, with 1-2 feet possible. Probabilities across the other ranges south of 40N latitude are moderate for 8 inches, with snow levels primarily remaining above 5000 ft. Saturday into Sunday, the next shortwave and accompanying surge of 700 mb warm/moist advection and ascent through jet level diffluence and height falls leads to likely accumulating snows from the Sierra Nevada, extending across the Siskiyous and north into the southern Cascades. As the wave moves further inland, a period of snow is expected in the ranges of southern ID and then into northwest WY, as well as the mountains of central NV. Although widespread heavy accumulations are not expected, WPC probabilities indicate a slight risk for 8 inches from the Blue Mountains of OR into the Sawtooth range and eastward into NW WY. ...Central Appalachians into New England... Days 1-2... Complex upper pattern featuring the interaction of no less than 3 shortwaves will spawn a deepening surface low near the Delmarva today which will move northeast into Maine on Friday. Further interaction with the final shortwave phasing into a closed low over the northeast will help to occlude and vertically stack the system, producing very slow movement to the northeast through Saturday. Despite very good model agreement in the interaction of the three shortwaves and that effect on the surface low evolution, this remains a challenging snowfall forecast. As the first two shortwaves phase and cause a negative tilt to the upper pattern over the Mid-Atlantic, this will spread anomalously high moisture into New PA/NY/New England on a strong LLJ/WAA. Column RH rises quickly today across PA/NY and western New England which will be wrung out as precipitation due to intense height falls and increasing upper diffluence. 850mb temps climb above 0C all the way to the Canadian border by tonight as the low tracks inland, suggesting terrain-dependent precipitation type, with snow expected above 2-3 kft and a mix or rain below that level. Snow levels will remain near the surface across Maine, but that area will be under the influence of the anticyclone and lower RH today so little snowfall is expected. In this setup, the highest probabilities for 4 inches of snow are just above 50% across the Adirondacks and Catskills. There is likely to be significant snowfall gradient in the terrain however, especially in the Champlain Valley of VT. As the low moves into Maine Friday, a tertiary shot of northern stream energy will dig into the negatively tilted trough to enhance diffluence and height falls, close off the mid-level circulation, and cause the surface feature to stall. At the same time, cold air will wrap quickly southward as NW winds through the column increase, which also enhances upslope snowfall. Falling snow levels combined with more robust forcing including increasing 850-700mb fgen and mid-level deformation W of the 700mb low will produce heavy snowfall from the Adirondacks and points east into the Green and White Mountains, as well as into northern ME. WPC probabilities show a moderate to high risk for 8 inches of accumulation in the highest terrain, with light accumulations expected down into the Valleys as snow levels crash. An additional caveat is the potential for a heavy band of snow to develop from central PA into the Poconos and Catskills and potentially into the Berkshires as shown by much of this mornings suite. This band is due to a collocation of pivoting low-level fgen and enhanced deformation near the low center. Despite good model agreement and HREF mean accumulations of over 6" in many areas, the strongest forcing remaining below the DGZ, a warm nose above 0C, and rapid northward advance of the TROWAL suggests this snowfall may be overdone. Have trended upward to show moderate probabilities for 4 inches in these areas, but the potential exists for much more if the column cools more quickly during the period of heaviest precipitation. As the low pulls away slowly, NW flow will be favorable for upslope snow as far south as the highest NC/TN mountains where light accumulations are possible, and in the high terrain in WV where WPC probabilities are up to 30% for 4 inches. The probability of significant freezing rain is less than 10 percent. Weiss