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|    Message 41,144 of 41,475    |
|    COD Weather Processor to wx-storm@lists.illinois.edu    |
|    HVYSNOW: Probabilistic Heavy Snow And Ic    |
|    09 Feb 26 07:35:02    |
      TZUTC: 0000       MSGID: 169344.weather@1:2320/105 2df159bc       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 090734       QPFHSD              Probabilistic Heavy Snow and Icing Discussion       NWS Weather Prediction Center College Park MD       234 AM EST Mon Feb 9 2026              Valid 12Z Mon Feb 09 2026 - 12Z Thu Feb 12 2026                     ...Pacific Northwest through Northern Rockies...       Day 1...              A shortwave trough crossing the area will be positioned atop the       interior Northwest to start the period, and then translate rapidly       eastward through D1. This feature will likely shear out into the       westerlies as it advects into the High Plains in response to rapid       ridging building in its wake, but there has been a subtle trend of       increased amplitude of this feature tonight. This shortwave will       work effectively with an intensifying upper jet streak to overlap       mid-level height falls with LFQ diffluence, leading to sufficient       ascent to produce a wave of low pressure along a cold front south       of the region.              Additionally, this jet streak will result in increasing mid-level       frontogenesis, especially within the 700-500mb layer, which will       produce impressive omega directly into the DGZ. Although ascent       will be temporally modest, cross-sections indicate a high threat       for CSI within any snow bands that develop, and this could (30-60%       chance) produce 1-2"/hr snowfall rates. The heaviest snowfall is       likely in the terrain of the Absarokas and near Yellowstone NP due       to upslope enhancement, but anywhere across southern MT and       northern WY could see bands of heavy snowfall which will accumulate       rapidly despite marginal thermals in the low- levels. The high-res       guidance has trended upward significantly, as have many of the       globals, so confidence has increased in significant snowfall       accumulations, which is now reflected by WPC probabilities that       indicate a high risk (>70% chance) for at least 4 inches, with more       than 12 inches possible in the higher terrain including the Lewis       Range and Tetons.                     ...Sierra Nevada to the Central Rockies...       Days 2-3...              A closed mid-level low will approach central California from the       west on Tuesday before slowly filling into an open, positively       tilted trough Wednesday as secondary vorticity energy digs towards       Baja. This slow evolution will result in pronounced S/SW flow       aloft, which will combine with a strengthening jet streak to spread       moisture onshore CA and then expand eastward towards the Central       Rockies by late Wednesday. This prolonged, albeit relatively       modest, moisture plume/IVT will bring much needed precip to the       Great Basin and central Rockies through midweek.              Snow levels will be at or just below 7000ft along the Sierra Nevada       on Tuesday in the onshore flow, dropping to around 6000ft Tuesday       night under height falls. Great Basin/Rockies snow levels will       generally remain 6000-7000ft through midweek.              2-day snow probabilities from WPC suggest a near certainty (>90%)       of at least 8 inches across much of the Sierra with locally as much       as 2 feet possible (30% chance) in the higher Sierra. Additional       snowfall totals exceeding 8 inches are possible (50-70%) for parts       of the Uintas, Colorado Rockies, and northern CA ranges.                     ...Northern Great Lakes and Northeast...       Days 1-3...              A closed mid-level low will elongate and track from the Northern       Great Lakes to across New England mid-week, exiting to the Gulf of       Maine by Thursday morning. This upper feature will be accompanied       by an extended vorticity lobe on its south side, helping to produce       strong ascent through height falls/PVA across the region. As this       develops, pronounced warm air advection (WAA) will develop to its       south as a surface low /clipper type/ races southeast beneath the       upper trough. This will produce two rounds of ascent: first with       the intensifying WAA south of the surface low, and then second with       post-clipper CAA/upslope flow.              While the ascent within the WAA will be impressive, it will also be       of short duration, generally 6-12 hours, so although snowfall rates       will likely be intense (50-70% chance of 1+"/hr), the total       snowfall accumulations will be tempered as reflected by WPC       probabilities that are around 30% for 4+ inches across the U.P. of       MI D1, and then 30-70% on D2 for Upstate NY and northern/central       New England. Despite that, some more significant snowfall       accumulations are likely across the Tug Hill Plateau, the       Adirondacks, and the Greens where a combination of CAA for lake       effect snow (in the Tug Hill) and upslope snow (Adirondacks and       Greens) will lengthen the duration of accumulating snowfall. In       these areas, locally more than 8 inches of snow is possible       (10-30%, highest across the Tug Hill Plateau).              Finally, as the closed low moves into the Gulf of Maine, a surface       low will deepen offshore in response. While direct impacts from       this surface low are not expected to be significant, the guidance       is hinting at a lingering inverted trough pivoting back across       coastal Maine Wednesday. These inverted troughs can sometimes lead       to sneaky-heavy snowfall accumulations, so although current WPC       probabilities are around 50-70% for 4+ inches of snow, this will       need to be monitored for any upticks as the event gets closer.                     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: 154/110 700 203/0 218/700 840 220/10 20 90 221/1 6 360 226/18       SEEN-BY: 226/20 30 44 50 227/114 229/110 134 206 300 307 317 400 426       SEEN-BY: 229/428 470 664 700 705 240/5832 266/512 280/5003 291/111       SEEN-BY: 301/1 320/119 219 319 2119 322/757 762 326/101 335/364 341/66       SEEN-BY: 342/200 396/45 423/81 460/58 633/280 712/848 902/26 2320/0       SEEN-BY: 2320/105 304 3634/12 5020/400 5075/35       PATH: 2320/105 154/10 221/6 1 320/219 229/426           |
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