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|    Message 39,979 of 41,475    |
|    COD Weather Processor to wx-storm@lists.illinois.edu    |
|    HVYSNOW: Probabilistic Heavy Snow And Ic    |
|    02 Jan 26 07:53:18    |
      TZUTC: 0000       MSGID: 168181.weather@1:2320/105 2dbf406c       PID: Synchronet 3.21a-Linux master/123f2d28a Jul 12 2025 GCC 12.2.0       TID: SBBSecho 3.28-Linux master/123f2d28a Jul 12 2025 GCC 12.2.0       BBSID: CAPCITY2       CHRS: ASCII 1       FORMAT: flowed       FOUS11 KWBC 020753       QPFHSD              Probabilistic Heavy Snow and Icing Discussion       NWS Weather Prediction Center College Park MD       253 AM EST Fri Jan 2 2026              Valid 12Z Fri Jan 02 2026 - 12Z Mon Jan 05 2026              ...Great Lakes...       Days 1-3...              Ongoing lake effect snow (LES) Will continue in earnest today,       especially across the eastern U.P., and downwind of Lakes Erie and       Ontario. This LES will be driven by persistent CAA across the       lakes, leading to steep lapse rates and inversion depths that climb       towards 800mb, leading to 500-750 J/kg of lake-induced instability.       While the mean low-level flow will be a bit more W than NW, this       will help tap an upstream connection from Superior, across Huron,       and towards Lake Ontario, indicating the heaviest snowfall will       likely be along and south of the Tug Hill Plateau through D1 and       into D2 before winding down in response to brief shortwave ridging.       While periods of heavy snow are also likely in portions of the       northern L.P. and along the Chautauqua ridge, the persistence and       intensity of this snowfall should be less. This is reflected by WPC       probabilities for 4+ inches on D1 that area 30-50% in the eastern       U.P. and along the Chautauqua Ridge, but above 90% east of Lake       Ontario, where locally 2+ feet is likely on D1. During D2 the       intensity and coverage of LES wanes, but WPC probabilities for 4+       inches remain above 50% near Oswego, NY.              After a brief respite in response to the aforementioned shortwave       ridging, two separate, but fast moving, shortwaves will crest the       ridge to the west and dive rapidly from Saskatchewan/Alberta across       the Great Lakes. The first of these will race southeast Saturday       aftn/night, and while some enhanced ascent and subtly increased       moisture will result in light synoptic snowfall, additional       accumulations from eastern MN through western NY should be minimal.              A more substantial impulse will then drop southeast in a similar       fashion Sunday night, but this impulse will be accompanied by       greater moisture as it originates from the Pacific and ejects from       the Northern Plains rather than central Canada. This will again be       fast moving, but will have more pronounced synoptic lift in       response to height falls, PVA, LFQ jet diffluence, and more robust       850mb WAA leading to enhanced fgen. At this time, the speed of the       system is expected to limit total snowfall, but briefly heavy snow       rates thanks to idealized ascent into the DGZ could produce a       narrow swath of more than 4 inches as reflected by WPC       probabilities that are as high as 50-70% for 4+ inches from near       Duluth, MN eastward through much of the U.P and the neighboring       portions of WI.                     ...Western U.S. Mountain Ranges...       Days 1-3...              An active period of weather continues across much of the West as       Pacific moisture repeatedly surges onshore in response to       persistent troughing offshore.              For D1, a brief period of ridging will blossom along the Pacific       Coast, but downstream into the Intermountain West a shortwave with       Pacific origin will lift steadily northeast while de-amplifying.       This will result in a stripe of precipitation arcing from the       Northern to the Central Rockies, and falling as snow above       6000-7000 ft. WPC probabilities D1 reach above 70% for 6+ inches       near the Tetons of WY and the Park Range of CO, with more       widespread elevated probabilities for 4+ inches across much of the       rest of the terrain in this region.              Then beginning late D1 and continuing into D3, much more pronounced       moisture begins to pivot onshore the Pacific Coast. This will be in       response to an impressive trough aligned just offshore, from which       a surface low will track northeast towards WA state by Sunday       morning, with a secondary wave tracking towards northern CA Sunday       aftn. While these surface lows will help enhance local ascent, in       general moisture will be pronounced across much of the West due to       increasing southerly flow downstream of the primary trough axis       pushing IVT well onshore with magnitudes above 500 kg/m/s. As is       typical with strong IVT plumes, they will be driven both by Pacific       jet energy and warm advection, resulting in elevated snow levels       climbing to 7000-9000 ft ahead of the first wave, and while they       will rise again with the secondary wave, they will generally be       much lower, 5000-7000 ft on D3, even lower, around 3500 ft, in the       Cascades and interior Northwest.              Any ascent forced through synoptic features or upslope enhancement       will cause rounds of heavy snowfall above these elevations both       Saturday and Sunday. WPC probabilities steadily increase and expand       through the weekend, with widespread high chances (>70%) for 4+       inches reaching from the Olympics, along the entirety of the       Cascades, the Shasta region, the Sierra, and through much of the       Northern/Central Rockies and into the Wasatch, by Monday morning.       While the heaviest snowfall is likely in the Sierra where many       locations above 6000 ft could experience 2-5 feet of snow, much of       the higher terrain of the West could receive 1-2 feet before       coverage wanes just beyond D3. This will likely bring considerable       impacts to the higher elevations due to generally low SLR snow,       with difficult travel likely across the Sierra Passes.                     ...Central Plains...       Day 1...              A fast moving clipper rounding the western ridge and dropping       southeast over the Central Plains today will be of subtropical       origin. Although this feature will be progressive and of modest       amplitude as it weakens, it will produce sufficient ascent into a       moistening column to produce a narrow corridor of mixed       precipitation in the vicinity of northeast Nebraska. While total       precipitation will be modest, WPC probabilities indicate a 70-90%       chance of at least 0.01" of freezing rain, with locally up to 0.1"       of ice possible leading to hazardous travel.                     Weiss                            $$              = = =       To unsubscribe from WX-STORM and you already have a login, go to       https://lists.illinois.edu and use the "Unsubscribe" link. Otherwise email       Chris Novy at cnovy@cox.net and ask to be removed from WX-STORM.              --- SBBSecho 3.28-Linux        * Origin: Capitol City Online (1:2320/105)       SEEN-BY: 1/19 100 16/0 19/10 37 104/119 105/81 106/201 114/10 120/302       SEEN-BY: 123/130 128/187 129/14 142/104 153/757 7715 154/10 30 50       SEEN-BY: 154/110 700 201/0 203/0 218/700 840 220/10 20 30 90 221/1       SEEN-BY: 221/6 360 226/18 30 44 50 227/114 229/110 134 206 275 300       SEEN-BY: 229/307 317 400 426 428 470 664 700 705 240/5832 266/512       SEEN-BY: 280/5003 291/111 301/1 320/119 219 319 2119 322/757 762 326/101       SEEN-BY: 335/364 341/66 342/200 396/45 423/81 460/58 633/280 712/848       SEEN-BY: 902/26 2320/0 105 304 3634/12 5020/400 5075/35       PATH: 2320/105 154/10 221/6 1 320/219 229/426           |
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