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Quantitative Precipitation Forecast
Issued by NWS
Issued by NWS
050 FOUS11 KWBC 221908 QPFHSD Probabilistic Heavy Snow and Icing Discussion NWS Weather Prediction Center College Park MD 208 PM EST Sat Feb 22 2025 Valid 00Z Sun Feb 23 2025 - 00Z Wed Feb 26 2025 ...Pacific Northwest through the Northern Rockies... Days 1-3... The overall synoptic evolution forecast remains pretty consistent among guidance as of the 12z NWP suite. A closed mid- level low tracking slowly south of the Aleutians will continue shedding lobes of vorticity eastward and onshore the Pacific Coast, spreading precipitation from the Pacific Northwest through the Northern Rockies into early next week. Generally W to SW flow will persist across the Pacific during this time, with enhanced confluence south of the Aleutian Low enhancing moisture advection and IVT as an atmospheric river (AR). Both ECENS and GEFS probabilities indicate that IVT will almost certainly (>90%) exceed 500 kg/m/s, with 3 consecutive days of IVT exceeding 250 kg/m/s surging onshore beginning this evening. Within this moisture plume, PWs are progged by NAEFS to exceed the 99.5 percentile of the CFSR database, especially late D1 through the end of D2 from the WA/OR coasts to as far inland as the Central Rockies. Shortwaves/vorticity spokes rotating within this flow will cause periodic enhancement to ascent leading to heavier and more widespread precipitation. Although the timing of these features is not fully agreed upon by the guidance, consensus suggests bouts of heavier precipitation are likely beginning late D1 and again late D2. While this will result in heavy snow in higher terrain features across the region through the period, snow levels will climb steadily within the AR/accompanying WAA. Snow levels begin the period around 4000-6000 ft, then climb to as high as 7000-9000 ft, especially during D2. This will keep most significant snow accumulations above area pass levels. As me move into D3, a tertiary shortwave trough will pivot underneath the prominent gyre to the north generating a more significant height fall pattern as we step into Tuesday morning. Snow levels that rose considerably in the periods prior will see them decrease rapidly as the advancing shortwave trough allows for colder temps to seep down into the previous 4000-6000 ft range culminating in more widespread heavy snowfall across the Northern Cascades and higher elevations of the Olympics in WA. Steady progression of colder air mixing further into the column will protrude areas east of the coastal ranges with areas inland towards northern ID and northwestern MT seeing an uptick in snowfall for the 12-00z time frame Tuesday into Wednesday. Heaviest snow will still be confined to the Cascades, but some areas east of the mountain chain will see >4" of snowfall, namely over the Bitterroot Range extending northeast towards the Cabinet Mtns., and southeast into the Absaroka Range. The heavy snow footprint continues to be most prominent in that D2 to D3 time frame with the highest probs (>70%) for >4" located over the ranges above. Additional high probs over 70% will exist in the highest elevations of the Olympics by D3 due to the incoming disturbance. Totals >8" are split between the remainder of D1 with a break between D1 and part of D2, but will pick up significantly in both magnitude (50-80%) and spatial coverage of the higher probs across the PAC Northwest by the end of D2 into D3 within the vicinity of the Cascades, Olympics, and Bitterroot Ranges. This will culminate in the highest elevations encountering several (4+) feet of snow over the next 72 hrs. with 1-3 feet forecast for areas between 4000-7000 ft MSL. Additionally, some light icing is expected in the Columbia Basin, as well as parts of eastern OR where WPC probabilities D1 into early D2 reach 10-30% for up to 0.1" of ice. Weiss/Kleebauer ...Tug Hill through Northern Green & White Mountains... Day 1-2... Shortwave trough analyzed over the northern Great Lakes will continue pushing downstream into neighboring Quebec with the southern fringes of the energy bisecting Upstate NY through Northern New England by this evening. Sufficient low-level buoyancy generated by modest delta-T`s over Lake Ontario will create a moderately strong singular band that will align downwind of the lake with the fetch aimed into the Central and Southern Tug Hill Plateau. Combined moisture fetch and local upslope component will allow for a targeted area of heavy snow to those areas within the band placement. High probs of 70-90% for >4" exist within the window of 00-18z Sunday with a very small area of 40-70% probs for >6" intersecting the Tug Hill area between Watertown to Pulaski and points inland. This is the primary zone for heavy snow within the Northeastern U.S, but some upslope snows within the Northern Green and White Mountains of VT/NH also point to some modest probabilities of >4", especially as you enter the Greens from Mount Mansfield and points north. Kleebauer $$