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From | To | Subject | Date/Time | |||
Mike Powell | All | HVYSNOW: Probabilistic He |
November 12, 2024 10:03 AM * |
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FOUS11 KWBC 120820 QPFHSD Probabilistic Heavy Snow and Icing Discussion NWS Weather Prediction Center College Park MD 320 AM EST Tue Nov 12 2024 Valid 12Z Tue Nov 12 2024 - 12Z Fri Nov 15 2024 ...Western U.S... Days 1-3... An active period of winter weather continues across the Western CONUS this period as dual shortwave trough cross the region., The first of these will be moving from the eastern Great Basin this morning into the Central Plains by Wednesday evening, with minimal amplitude gain. The combination of the progressive nature of this feature with modest PW surge (at least until the Plains when thermals support only rain) will somewhat limit snowfall potential D1. However, sharp height falls downstream of the short-wavelength trough combined with low-level convergence along the accompanying cold front and post-frontal upslope flow into terrain features will still support rounds of moderate to heavy snow. The greatest potential for significant accumulations will be across the Wasatch and Colorado Rockies, including the Park Range, where WPC probabilities for more than 6 inches are above 70%, and locally up to 10 inches is possible, primarily above 5500 ft. Brief shortwave ridging blossoms across the Northwest behind this first trough, but is quickly replaced by a more impressive impulse digging along the Pacific Coast as it drops from the Gulf of Alaska. Downstream divergence and accompanying WAA/moist advection will begin to spread precipitation back into the Pacific Northwest late tonight. Unlike its predecessor, this secondary trough will be very slow to move east as it gets repeatedly reinforced just off the coast by renewed lobes of vorticity swinging cyclonically around it. This will have the two-pronged effect of driving waves of ascent and persistent moisture onshore, while also keeping the primary trough axis positioned just west of the region until Friday when a more pronounced vort max swings through the base and pushes the trough onshore CA late in the forecast period. Within the most impressive WAA, a narrow channel of IVT exceeding 750 kg/m/s is likely, focused into the WA/OR and northern CA coast late D2 into D2 before weakening with inland extent. This channel /AR/ will also provide the highest increase in snow levels, reaching as high as 7000 ft. However, dual cold front progged to push onshore, one Wednesday morning and another Thursday morning, driven east by periodic shortwaves, will cause gradual lowering of snow levels to as low as 3000 ft by Friday morning across the Cascades, and 4500 ft into the Interior Northwest and northern CA. The lower snow levels will be accompanied by weaker forcing and more transient moisture however, so heavy pass-level snow is still not anticipated at this time. Despite that, heavy snow accumulations are likely, especially on D2 when WPC probabilities for more than 6 inches spike above 90% in the Cascades, Shasta/Trinity region, the Okanogan Highlands, Selkirk Mountains, and Blue Mountains. Some of these areas could receive as much as 2 feet of snow D2, and 6-12 inches is possible at some of the elevated passes including Washington Pass. By D3, the snow intensity wanes across most of the NW, but an increase in WPC probabilities for 6+ inches reaching 30-50% in the Sierra as the trough finally pushes onshore into CA. The probability of significant ice across the CONUS is less than 10 percent. Weiss $$ --- SBBSecho 3.20-Linux * Origin: capitolcityonline.net * Telnet/SSH:2022/HTTP (618:250/1) |
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