Quantitative Precipitation Forecast
Issued by NWS
Issued by NWS
138 FOUS11 KWBC 150723 QPFHSD Probabilistic Heavy Snow and Icing Discussion NWS Weather Prediction Center College Park MD 223 AM EST Sat Nov 15 2025 Valid 12Z Sat Nov 15 2025 - 12Z Tue Nov 18 2025 ...California... Days 1-3... A pair of upper lows are forecast to impact much of the central and southern Sierra Nevada with heavy snow over the next few days. The first upper low is expected to situate off the coast of southern California to start the period. This system will also be particularly deep early Saturday, with 500mb heights around the 0.5th climatological percentile over the eastern Pacific per the 18z ECMWF. This closed upper low is forecast to swing inland during the day 1 period while also weakening. This will provide a surge of moist southerly flow into the central/southern Sierra. This flow will not be ideally orthogonal to the Sierra off the Pacific, but the upper low placement overhead and PWs near the climatological maximum for November (per the NAEFS) will allow for gradually falling snow levels, ample lift, and widespread moderate precipitation. Snow levels will once again start out above 9k feet, but gradually fall to around 7k feet by Sunday morning ahead of another rapidly approaching upper low early Monday. This second upper low is expected to be rather progressive, but could contain IVT above 400 kg/m/s for a brief period of time oriented primarily into the central Sierra Nevada. In total, an additional 1-2 feet of snowfall (and even up to 3 feet locally in portions of the southern Sierra) is possible above 8k feet elevation. The latest WPC 72-hr snow probabilities >24" across the high terrain of southern Sierra Nevada remain very high (80-99%) above 9k feet, and moderate (40-60%) above 8k feet. ...Interior Northeast... Days 1-3... Persistent troughing remains across New England and southeast Canada to start the period and will be reinforced by a potent shortwave dropping southeast into the region by Sunday before deepening into a strong vertically stacked low through the end of day 2. This will provide for warm air advection driven precipitation Saturday night into Sunday as cold low-level air ahead of this system produces a CAD setup across northern New England, with strong cold air advection returning across the Northeast on days 2 and 3. The associated surface low is forecast to slide from southeast Ontario to coastal Maine and allow for the low- level cold air to only very slowly retreat north. A wintry mix with pockets of freezing rain is most likely to impact the Adirondacks into the Green and White Mts of VT/NH/ME, beginning as early as Saturday evening after a brief period of moderate to heavy snow. As the surface low matures near southeast ME, deformation banding within a developing trowal is possible across northern ME and could produce pockets of 1"/hr snowfall rates on Sunday. The transient nature of the WAA should limit the ice threat somewhat. For this region, WPC 24-hr probabilities (12z Sat - 12z Sun) for at least 0.1" of ice generally range between 40-70% (though are now as high as 75-95% for portions of the Adirondacks in Essex County) and low chances (<30%) for more than 0.25". This is still enough freezing rain to cause slippery untreated roads and sidewalks. Snowfall will remain the predominant precip type across far northern NY, VT, NH and into central/northern ME where QPF may also be limited enough to prevent a major snowfall event, but some heavier snowfall rates are possible with the initial precipitation onset when 700 mb fgen is strongest and the mid-level low crosses over the region. WPC probabilities for at least 8" are between 30-50% in this region through Day 2, and locally are as high as 80% across portions of the northern Greens/Whites and northern ME where CAA upslope helps add to the totals on Day 3. The best upslope heavy snowfall is likely to be located across the northwestward facing Adirondacks and Green Mts. Once this system deepens across southeast Canada Sunday night into Monday, very strong west-northwest flow will develop across the Great Lakes and open up the potential for lake effect/upslope snow into the Interior Northeast. Specifically, a multi-lake connected snowband is possible extending from Lake Superior, Huron, and Erie into far western NY and northwest PA given the strong northwesterly flow. The latest WPC probabilities for at least 4" of snow across portions of western NY and northwest PA have increased to 30-50%. However locally higher amounts are possible should banding remain stationary for several hours. Snell $$