Quantitative Precipitation Forecast
Issued by NWS
Issued by NWS
555 FOUS11 KWBC 161905 QPFHSD Probabilistic Heavy Snow and Icing Discussion NWS Weather Prediction Center College Park MD 205 PM EST Sun Nov 16 2025 Valid 00Z Mon Nov 17 2025 - 00Z Thu Nov 20 2025 ...Northeast/Great Lakes... Days 1-2... Amplifying closed mid-level low will continue its slow trek into the Canadian Maritimes tonight through Monday, but wintry precipitation will continue in earnest across portions of Northern New England and Upstate New York. While the primary warm conveyor will pivot well east and away from the United States, a modest TROWAL will persist into northern Maine bringing some pivoting/comma head snowfall with rates of 0.5-1"/hr at times. This combined with increasing northerly winds will bring moderate impacts to the north and east portions of the state, especially the first half of the period, before the DGZ dries out and precip wanes. WPC probabilities for additional snowfall exceeding 4" in northern/eastern Maine are generally 30-50%. The more significant snowfall is expected farther west into the terrain of central ME and across NH, VT, and Upstate NY. This will be in response to prolonged and impressive upslope flow as NW winds develop and strengthen behind the departing low pressure system. The guidance is in good agreement that unidirectional NW flow will persist D1 and into D2, bringing periods of heavy snow as ascent is forced into the deepening DGZ and moistening the lower half of the resultant column. This should provide an environment favorable for heavy snow into Tuesday, and with Froude numbers indicating critical flow, the focus should be along the crests of the higher terrain and just upwind. With snowfall rates from the HREF progged to exceed 1"/hr at times, this will produce heavy accumulations for which WPC probabilities are high (>70%) for an additional 6+ inches of snow in the northern Adirondacks, Greens, and portions of the Whites of NH and ME, with locally up to 1 foot of snowfall possible (10-30%). Precipitation will wane on Tuesday with snow likely ending Tuesday aftn. Finally, the pronounced CAA on NW flow behind this system will cross the Great Lakes and produce some narrow bands of lake effect snow (LES), especially downwind of Lake Superior and Lakes Erie/Ontario. While this direction is not ideal for elongated fetch across the lakes, the high-res guidance is in good agreement that an upstream connection will occur from Superior, to Huron, to Erie, with an additional upstream band from Georgian Bay to Lake Ontario. This should produce narrow corridors of heavy snowfall exceeding 1"/hr on D1, leading to accumulations for which WPC probabilities indicate have a 50-90% chance of exceeding 4 inches across the Chautauqua Ridge, the Tug Hill Plateau, and portions of the eastern Finger Lakes region, with the latter continuing through D2. ...California to the Central and Southern Rockies... Days 1-3... A pair of upper lows embedded within persistent troughing across the West will bring periods of high-elevation heavy snow to portions of the region. The first will be associated with a compact shortwave lifting across UT/WY/CO that will deepen into a closed feature as it moves into the Central High Plains Monday afternoon. The amplification of this wave will result in increased deformation to its west, aligning with modest upper diffluence as a weak jet streak develops in the vicinity. This paired ascent occurring within a moist column (PWs above the 99th percentile) will result in a transition to heavy snow through dynamic cooling, especially in the higher terrain of CO and WY above 7000 ft. WPC probabilities for more than 6 inches of snow are high (>70%) from the Wind Rivers through portions of the Uintas and into much of the CO Rockies, with locally as much as 12 inches possible in the Wind Rivers and the Park Range. Upstream of this feature, a more pronounced upper low will dig slowly along the CA coast, tracking into Baja Wednesday before finally beginning to eject eastward late in the forecast period. Downstream of this feature, another round of impressive IVT exceeding the 90th percentile according to NAEFS ensemble tables will surge eastward into CA and the Great Basin, reaching the Four Corners states Wednesday. Beneath the upper low, snow levels will fall to 5000-5500 ft, but within the plume of IVT and accompanying WAA, which is also where the heaviest precipitation is expected, snow levels will remain elevated at 7000-9000 ft. This will result in heavy snowfall, initially in the Sierra, then spreading east into the Great Basin and Four Corners terrain including the San Juans, Wasatch, and portions of the Mogollon Rim (White Mountains of AZ area). WPC probabilities D1-2 are high (>70%) for 6+ inches in the Sierra and the higher terrain of the Great Basin and into the Wasatch and San Juans, where locally 1-2 feet of snow is likely by the middle of the week. ...Central Plains/Upper Midwest... Day 2... Compact mid-level shortwave will close off as it crosses from Nebraska to the Great Lakes Monday night and Tuesday. Significant mid-level moisture advection ahead of this feature will spread precipitation northwards into the Dakotas and then eastward through the Upper Midwest. On the north side of this precipitation shield, soundings suggest the column will be marginally thermally favorable for snowfall. However, cross-sections indicate an increasing threat for CSI where theta-es decreases with height, directly into the DGZ to support intense snow growth. Additionally a deep isothermal layer beneath the DGZ indicates a favorable setup for aggregate maintenance and large snow flakes with efficient accumulation. The guidance, especially the available high- res, has become more aggressive with this development, and it is likely that this ascent will cause rapid dynamic cooling of the column to support a narrow band of heavy snowfall which will track slowly from near the Coteau des Prairies through far southeast Wisconsin. While there is still pronounced latitudinal spread and timing differences, confidence is increasing that a band of heavy snow, with rates of at least 1"/hr, will move across the area. This is supported by increasing snowfall probabilities in both the NBM and the AIFS, and the updated WPC probabilities for at least 1" of snowfall have increased to above 70%. Locally much heavier snow is possible, and future updates will need to be monitored for this potential. Weiss $$