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|  Message 40037  |
|  COD Weather Processor to wx-storm@lists.illinois.edu  |
|  HVYSNOW: Probabilistic Heavy Snow And Ic  |
|  04 Jan 26 08:20:04  |
 TZUTC: 0000 MSGID: 168240.weather@1:2320/105 2dc1e9ed 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 040819 QPFHSD Probabilistic Heavy Snow and Icing Discussion NWS Weather Prediction Center College Park MD 319 AM EST Sun Jan 4 2026 Valid 12Z Sun Jan 04 2026 - 12Z Wed Jan 07 2026 ...Northern Plains/Upper Midwest/Great Lakes/Interior Northeast... Days 1-3... Some modest lake effect snow (LES) will continue through Sunday aftn, but primarily within a single band south/southeast of Lake Ontario with upstream connection to Lakes Huron and Superior. Additional snowfall across this region should be light as reflected by WPC probabilities for an additional 2+" of just 10-30%, although brief 1"/hr rates are possible (10-30% chance). Thereafter, the mid-level pattern flattens a bit as shortwave ridging expands from the west, leading to pinched and more progressive flow across the region. Within this flow, two back-to- back shortwaves will traverse the region bringing rounds of wintry weather. The first of these will emerge from the High Plains Sunday morning and push due east across the Great Lakes in a de-amplifying manner as it becomes absorbed into the pinched westerlies. Despite the weakening amplitude, height falls, PVA, and the left-exit region of a strengthening jet streak will produce deep layer ascent, and the intensification of this jet streak will likely result in enhanced omega despite the weakening amplitude of the shortwave. At the same time, increasing and impressive 925-850mb WAA will spread northeast ahead of this impulse, aligning with the best left-exit dynamics and the associated response to produce impressive fgen but with limited temporal duration. Since this feature will be of Pacific origin, the accompanying moisture will be impressive as reflected by NAEFS PWs that are above the 97th percentile, aligned with the strongest ascent. This suggests that as precipitation expands from MN through the U.P., and into the northern L.P., a narrow band of heavy snow will develop which has a 60-80% chance of producing 1"/hr snowfall rates. The duration of these will, again, be limited to the progressive nature of the wave, but WPC probabilities for 4+ inches are above 50% from the Arrowhead of MN eastward through the northern L.P. of MI, with locally 6-8" possible (30% chance) in portions of the eastern U.P. Additionally, south of this axis of heavy snow, a corridor of modest mixed precipitation, including freezing rain, is likely as the WAA surges a warm nose to around +3C at 850-800mb. The refreezing layer is quite deep, so this may manifest more as sleet than freezing rain, but hazardous travel is Sunday evening from MN through central WI where WPC probabilities for 0.01" of ice are 50-70%. This lead wave will continue to track into New England before exiting to the Atlantic Monday night, but additional snowfall is expected to be light, generally 1-3", although locally higher in the Tug Hill Plateau through lake enhancement, as ascent weakens. The next shortwave follows quickly in the wake of the first, and emerges from CA Sunday evening before racing to reach the Corn Belt by Tuesday morning. This impulse will track along the southern subtropical jet, which is progged to intensify over the Central Plains, reaching towards 140 kts. The favorable overlap of the LFQ and height falls downstream of the shortwave will likely lead to surface low pressure development Monday night near Iowa, with this low then tracking steadily northeast into Ontario by Tuesday evening. While there is still some spatial spread in the placement of this low according to the different ensemble clusters, the increasing ascent will lead to another round of wintry precipitation from Minnesota through the Great Lakes (where a mix of freezing rain and snow is likely), with additional mixed precipitation spreading into New England by the end of the forecast period. Total ascent with this secondary wave should be less intense than the lead wave, and the thermal evolution is quite complex due to potential secondary low development in the Gulf of Maine, but at this time WPC probabilities for 2+ inches of snow are just 10-30% in the higher elevations of Upstate NY and northern New England. For the freezing rain, WPC probabilities indicate a high risk (>70% chance) of at least 0.01" of ice from central MN near the Twin Cities through much of WI and MI, and into central and northern New England. The greatest risk for at least 0.1" of ice is likely in parts of northern WI, northern MI, and the higher elevations of the Catskills, Adirondacks, and southern Greens. ...Western U.S. Mountain Ranges... Days 1-2... The active west continues into early next week as an anomalous trough persists just off the Pacific coast through Tuesday morning before amplifying into a closed low which then undercuts towards Baja by the end of the forecast period. Downstream of this trough, nearly continuous S/SW flow will shed spokes of vorticity onshore, with the accompanying height falls/PVA leading to rounds of precipitation across much of the western CONUS. At the same time, a subtropical jet will amplify and waver from CA through the Central Plains, providing additionally enhanced ascent. The combination of persistent SW mid-level flow with the wavering jet stream will surge periods of elevated IVT onshore, resulting in PW plumes that occasionally exceed the 90th climatological percentile. While there may be periods of enhanced ascent locally across different regions, in general the next 48 hours appear to be synoptically forced with broad large-scale ascent, locally enhanced through PVA where the vorticity lobes stream overhead, and through upslope enhancement. The strongest upslope flow continues to be appear focused over the Sierra where snowfall will be prolific, but heavy snow is likely through Monday night across much of the region. With broad SW flow encompassing the region, the accompanying WAA will surge snow levels to as high as 6000-8000 ft in the Great Basin and Rockies D1 (but generally 3000-5000 ft elsewhere), before steadily falling through D2 as a cold front pushes eastward and the trough axis finally swings farther east to the coast. By 12Z Tuesday, snow levels are expected to be generally 1500-2500 ft in the north, to 5000-6000 ft in the south. 2-day WPC probabilities (12Z Sunday through 12Z Tuesday) feature a high risk (>70% chance) for 12+ inches in the Sierra, northern CA ranges, Uintas, Tetons, Wind Rivers, and portions of the Salmon River/Sawtooth/Bitterroots, with lesser snowfall expected at the other regional terrain. In the Sierra, 2-4 feet is possible in the higher elevations. ...Cascades... Day 3.. Mid-level flow across the Northern Pacific will become pinched and zonal Tuesday, while a weak impulses approaches the coast and may move onshore overnight into Wednesday morning. This zonal mid-level flow will be topped by a strengthening Pacific jet streak which will drop gradually southward such that the overlap of PVA/height falls will match the greatest LFQ diffluence to provide ample ascent. This will be aided by upslope enhancement into the terrain thanks to the westerly flow, producing brief but impressive deep layer lift into IVT that has a >80% chance of exceeding 250 kg/m/s. While westerly IVT does not usually result in as impressive of precipitation as that with a S or SW component, a fully saturated column with steepening lapse rates will result leading to a period of heavy snow in the Olympics and Cascades of OR and WA. Snow levels will be generally 2000-3000 ft during this time, so pass level impacts leading to hazardous travel are expected. WPC probabilities for more than 8 inches of snow reach 70+%, with more than 1 foot possible at the passes (Snoqualmie and Stevens included). 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: 19/10 104/119 105/81 106/201 114/10 120/302 128/187 129/14 SEEN-BY: 153/757 7715 154/10 30 50 110 700 218/700 840 220/10 20 30 SEEN-BY: 220/70 90 221/1 6 360 226/17 18 30 44 50 227/114 229/110 SEEN-BY: 229/134 206 275 300 307 317 400 426 428 470 664 700 705 266/512 SEEN-BY: 267/800 291/111 301/1 320/219 322/757 335/364 341/66 342/200 SEEN-BY: 396/45 460/58 633/280 712/848 770/1 100 340 350 772/210 220 SEEN-BY: 772/230 902/26 2320/0 105 304 3634/12 5020/400 5075/35 PATH: 2320/105 154/10 221/6 218/840 770/1 633/280 229/426 |
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