Probabilistic Heavy Snow and Icing Discussion NWS Weather Prediction Center College Park MD 313 PM EST Sat Dec 29 2018 Valid 00Z Sun Dec 30 2018 - 00Z Wed Jan 02 2019 ...Pacific Northwest through the Southern Rockies and Southwest... Days 1-3... A shortwave and associated Pacific Jet will drop southward along the West Coast before shifting inland towards the Great Basin. Beneath these features, a surface cold front will push southeast into the Rockies, while a wave of low pressure drops towards the Northern Plains. The combination of these features will support heavy snow across the terrain from the Washington Cascades east and south through the Northern Rockies and into NW Wyoming. WPC probabilities are high for 8 inches of snow, and more than 12 is possible, in the Cascades, Bitterroots, and Northern Rockies. Elsewhere across the northwest, accumulating snow will occur as low as 1000-2000 feet as snow levels fall behind the front, and WPC probabilities are high for 4 inches across much of the area. This system will then progress slowly southward through the Great Basin and towards the Four Corners and reinforce a deep but positively tilted longwave trough. As this occurs, the aforementioned surface cold front will drop through the Plains and into the Southwest. This will spread snowfall across the Central Rockies on day 2, but the heaviest snow is likely once again across the Southern Rockies and southwest into New Mexico. Here, the best combination of jet level diffluence, low-level convergence and moist advection, and upslope enhancement will combine to produce heavy snowfall from Southern Colorado through much of New Mexico and into eastern Arizona. The heaviest snowfall is likely in the southern Sangre De Cristos, as well as the mountains in western New Mexico/SE Arizona, where WPC probabilities are high for 8 inches and more than 12 inches is possible. Heavy snow is likely at the lower elevations as well, and WPC probabilities feature a high risk for 4 inches across much of New Mexico. ...Central and Northern Plains, Northern Mississippi Valley, Great Lakes,and New England... Days 2-3... Complex split flow pattern creates a challenging forecast for the central part of the CONUS to start 2019. A northern stream shortwave will eject eastward from MT during day 2 aiding in ascent produced by a potent jet maximum moving across southern Canada. This will likely produce a swath of snow where the best upper divergence, height falls, and low level convergence along a surface cold front combine. This feature is likely to lift quickly eastward and is somewhat moisture starved, so total snow accumulations are likely to be modest, with WPC probabilities 30-50% for 4 inches from near the Black Hills of SD, northeast through the area around Lake Superior. Further south, a southern stream shortwave lifting out of the Southwest will move northeast while inducing surface cyclogenesis near the Gulf Coast. This surface wave will move quickly to the northeast into the eastern Great Lakes by the end of Day 2, and robust ascent due to warm advection and forced synoptic lift beneath a jet maximum will produce widespread precipitation across the east. Much of the area will be too warm for snow. However, it is likely that on the northern and northwest side of the precipitation shield, enough cold air will be present either initially (north/northeast) or advect in (northwest) to produce freezing rain or snow. The best chance for freezing rain will be across the Southern Great Lakes, but accretions are likely to be minimal. Further northwest from Kansas northeast into Lower Michigan, enough cold air behind the front combined with lift within a deformation zone may produce a few inches of snow accumulation, and WPC probabilities are low to moderate for 4 inches. There remains considerable spread in the guidance into how much phasing of the northern and southern streams will occur, with the ECMWF producing more snow further north due to more interaction of the two streams than much of the other guidance. A general compromise was used for this iteration of the forecast, so while some snow accumulation seems likely, the large spread prevents higher probabilities for accumulation. Further northeast, as the southern stream impulse and surface low lift further northeast, interaction with the northern wave is expected. This will produce more widespread precipitation from the Mid-Atlantic into New England. The column will initially be cold enough for snow across northern New York and New England where several inches of snow are likely. Lesser amounts are forecast further south and in the lower terrain, with a few inches of snow possible before the transition to freezing rain, and eventually rain, occurs across most of the area by Tuesday morning. The probability for significant freezing rain (0.25 inches or more) is less than 10 percent. Weiss