Quantitative Precipitation Forecast
Issued by NWS
Issued by NWS
757 FOUS11 KWBC 050755 QPFHSD Probabilistic Heavy Snow and Icing Discussion NWS Weather Prediction Center College Park MD 255 AM EST Wed Nov 5 2025 Valid 12Z Wed Nov 05 2025 - 12Z Sat Nov 08 2025 ...Pacific Northwest through the Central Rockies... Days 1-3... An active pattern across the Pacific will continue through the week as a closed low lifts slowly into British Columbia, leaving persistently confluent W/SW flow across the Pacific and channeled into the West Coast. This fosters an extend period of impressive moisture advection and IVT surging onshore, and probabilities for a strong atmospheric river (AR) moving onto the coast exceed 80% from both the GEFS and ECENS ensemble systems on D1. The intensity of this moist advection is additionally reflected by NAEFS IVT percentiles that exceed the 99.5 percentile across CA Wednesday afternoon. This suggests an impressive precipitation plume will push from CA/OR northeast Wednesday aftn through Thursday aftn, with precipitation spillover reaching as far as the Northern and Central Rockies. However, most of this precipitation will fall as rain as the accompanying WAA surges snow levels to 7000-8000 ft, keeping any snow well above pass levels through Thursday. A secondary surge of precipitation associated with another disturbance embedded within the confluent onshore flow will lower snow levels at least slightly, to around 5000 ft, with additional heavy precipitation. At this time, impactful snow will likely occur at some of the higher passes, especially Washington Pass in the WA Cascades before Friday morning, before a final impulse shifts east causing precip to wind down across the Cascades but continue, in lighter fashion, across the Northern and Central Rockies. WPC probabilities D1 are moderate (50-70%) for >6" inches of snow in the northern WA Cascades, before expanding and shifting east into Salmon River/Sawtooth ranges, the Tetons, and Northern Rockies, while at the same time continuing across the northern WA Cascades. On D2 and bleeding into D3, the heaviest snow is expected across the WA Cascades where WPC probabilities reach above 70% for 8+ inches above 5000 ft, with moderate probabilities (30-50%) for 6+ inches continuing across portions of the Northern Rockies and higher elevations of ID and NW WY. Cumulatively through Friday night, 3-day snowfall probabilities show some moderate chances (40-60%) for snowfall totals to eclipse 12" in the tallest reaches of the northern WA Cascades, the Sawtooth, and Tetons. ...Northern New England and the Adirondacks... Day 1... A rapidly intensifying clipper-type low pressure will move progressively E/SE from Ontario, across New England, and then out to sea south of the Canadian Maritimes by Thursday afternoon. This low will spread significant moisture eastward on robust low-level FGEN leading to a pronounced TROWAL pivoting across Northern New England. The accompanying WAA will help spread significant moisture into the area, but the WAA will also drive snow levels up to 4000-5000 ft, suggesting that except for the highest peaks of northwest Maine, the pre-low precipitation will be all in the form of rain Wednesday afternoon. However, as the low tracks towards the New England coast, rapid CAA in its wake, aided by impressive isallobaric flow into the deepening system and topographically- enhanced upslope flow, will cool the column dramatically, reflected by snow levels falling to 500-1000 ft by 12Z Thursday. This results in a period of moderate to heavy snowfall in the higher terrain, with light snow gradually spreading into the lower elevations of VT/NH/ME and Upstate NY before the DGZ dries and precipitation dissipates Thursday afternoon. The heaviest snowfall is likely to unfold above 2000ft in the Adirondacks and Whites, although some moderate accumulations are also likely in the highest Greens. This is reflected by WPC probabilities which indicate a moderate risk (50-70% chance) for more than 4 inches of snow, with locally as much 8 inches in the highest Presidential Range peaks. Light accumulations of a dusting or more are likely elsewhere from Lake Ontario through central Maine, except across the Champlain Valley, resulting in the first notable snow of the year in some of the lower elevations of northern New England. The probability of significant ice across the CONUS is less than 10 percent. Mullinax/Weiss $$