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|    Message 40,869 of 41,475    |
|    COD Weather Processor to wx-storm@lists.illinois.edu    |
|    HVYSNOW: Probabilistic Heavy Snow And Ic    |
|    30 Jan 26 18:35:55    |
      TZUTC: 0000       MSGID: 169066.weather@1:2320/105 2de4c47c       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 301835       QPFHSD              Probabilistic Heavy Snow and Icing Discussion       NWS Weather Prediction Center College Park MD       135 PM EST Fri Jan 30 2026              Valid 00Z Sat Jan 31 2026 - 00Z Tue Feb 03 2026                     ...Southern Appalachians, Mid-Atlantic, & Southern New England...=20       Days 1-2...              ...A major winter storm is expected to produce heavy snowfall and=20       blizzard conditions across the southern Mid-Atlantic...              The synoptic evolution continues to support a major winter storm,       primarily focused over the Carolinas, but questions about the       details continue.              The event begins this evening, as snow breaks out across the       southern Appalachians of NC/TN. This initial development of snow       will be in response to increasing synoptic ascent within strong       mid-level divergence downstream of a pivoting shortwave digging out       of the Great Lakes. As this shortwave dives southward out of the       Great Lakes, it will rapidly deepen into an impressive closed low       by 12Z Saturday over the Tennessee Valley, and then continue to       dive southeast, reaching the GA/SC coast by 00Z Sunday. This will       produce extreme anomalies of more than -5 sigma with respect to       500mb heights according to NAEFS across the Southeast/Gulf Coast,       indicative of how rare and extreme this setup will be. As the upper       low deepens and drops southward, forcing will intensify in response       to not only the mid-level divergence noted above, but additional       robust height falls, and increasing jet-level diffluence as a       downstream subtropical jet streaks strengthens across the Gulf and       then begins to arc poleward along the Southeast coast. This will       help generate surface cyclogenesis along the coast of the       Carolinas, with dual low-pressure systems progged, each one       deepening along the intense baroclinic gradient positioned offshore       owing to the recent extremely cold air blanketed across the eastern       CONUS.              The secondary surface low, which is likely to be the more intense       feature as it explosively intensifies Saturday night into Sunday       (maybe reaching into the 960s offshore) is progged to pivot more       east than northeast along the coast, so the heavy precipitation       should be generally confined to the Carolinas, southern VA, and       maybe Cape Cod as it pulls away. While there is continued       uncertainty into the exact amounts of precipitation due to dry air       aloft and intense mesoscale ascent that will drive bands of heavy       snow, there is high confidence in this overall synoptic evolution,       resulting in high confidence in the most impacted areas.              The column will be extremely cold, so other than possibly some       light rain along the coast to start the event, this will be an       all-snow scenario with above-climo SLRs, a rarity for this part of       the country. As noted above, the snow begins across the       Appalachians Friday evening and then expand rapidly to the south       and east as the upper low dives towards the Gulf and low pressure       development occurs offshore. This expansion of precipitation will       be driven primarily by increasing 850mb easterly flow, tapping into       the growing theta-e ridge offshore, with the resultant WAA leading       to the expanding snow shield, Some of this WAA could be intense as       reflected by strengthening 925-700mb fgen, well aligned into the       deep DGZ (>70% chance of at least 100mb of DGZ depth according to       the SREF). This will support not only expanding snowfall, but       intensifying snowfall such that by 00Z/Sunday at least moderate       snowfall rates should encompass nearly the entirety of the       Carolinas and into northeast GA and southern VA.=20              After 00Z Sunday is when the heaviest snow and most notable impacts       are expected as the low offshore deepens rapidly. This will pivot       winds to more N/NE across the region, and as a deformation axis       pivots west of the surface low and the cold conveyor sets up across       the Atlantic and into the eastern Carolinas, more intense ascent=20       and greater moisture should result in extreme (for this region)=20       snow rates. Cross-sections indicate a broad region of favorable=20       conditions for CSI, or even CI (thundersnow), and the HREF snow-=20       rate probabilities peak above 50% for 1"/hr suggesting at least a=20       potential for 2"/hr within a pivoting band somewhere in eastern NC=20       or SC, and this is additionally supported by the WPC prototype       snowband tool. These heavy snow rates will be accompanied by=20       strong winds that may gust 35-50 mph, higher at the coast and in=20       the mountains, suggesting near blizzard conditions in many areas.=20       While uncertainty remains into how dry air in the mid- level may=20       impact snow amounts on the broad scale, locally very significant=20       snowfall accumulations are likely, especially within these bands,=20       during D2. By Sunday afternoon the low will pull away bringing an=20       end to the snowfall and leaving just cold windy conditions in its=20       wake.              The exception will be across far southeast Massachusetts and onto=20       Cape Cod and the Islands where, despite a subtle southeast trend in       today's model guidance, periods of moderate snow are still expected       due to onshore flow and sufficient synoptic ascent into the       moistening column. A period of moderate snowfall is likely, with       some local enhancement south of Boston and on the Outer Cape due to       ocean influences, Sunday aftn/eve.              WPC probabilities for the event are quite robust for both the       Appalachians and eastern North Carolina, where they are above 50%       for 8+ inches, and 30-50% for 12+ inches. The greatest potential=20       for more than 12 inches appears to be eastern NC where the=20       deformation band may pivot, but a widespread 4-8" snowfall appears=20       likely from southern VA through northern SC, with impactful=20       accumulations expected in areas like Richmond, VA, Charlotte and=20       Raleigh, NC, Columbia, SC, and even into Atlanta, GA. Farther=20       northeast, WPC probabilities are 30-50% for 4+ inches across the=20       Cape and Islands.              Key Messages are in effect for this storm, and are linked below       (Key Message #2).=20                     ...Great Lakes...       Day 1...              Potent shortwave diving southward within broad cyclonic flow into=20       the Tennessee Valley Saturday morning will rapidly sharpen the       eastern CONUS trough leaving pronounced CAA on northerly flow in       its wake. This will result in continued lake effect snow (LES),       especially in the favored north snow belts south of Lake Ontario       and especially south of Lake Michigan where the long fetch of the       lake will be maximized to produce a narrow band of heavy snowfall.       Although the lakes are cooling and have much higher ice coverage       than a week or two ago, frigid 850mb temperatures moving overhead       will create strong delta-Ts to support snowfall rates that have a       30-40% chance (from the HREF) of exceeding 1"/hr, greatest across       NW Indiana. While some light accumulations are likely south of Lake       Ontario, WPC probabilities for 4+ inches are confined to NW IN       where they reach 30-50%.                     ...Northern Plains through the Upper Midwest and Great Lakes...=20       Days 1-3...              A shortwave emerging from the Pacific will crest the ridge over the       Pacific Northwest and then dive slowly southeast into the Northern       Plains and then amplify into a deeper trough as it moves into the       Great Lakes and then elongate towards the Tennessee Valley. This       feature will generally be of modest amplitude and remain       progressive, so large scale forcing for ascent will be modest and       driven by mid-level divergence downstream of the trough overlapping       modest warm advection/isentropic ascent. The result of this will be       axes of both light freezing rain and snow in many areas from       eastern MT through the western Great Lakes. WPC probabilities for       2"+ of snowfall are as high as 30-50% D2 across central/northern       MN, and similar for parts of the U.P. and western L.P. of MI D3.       For freezing rain, WPC probabilities are as high as 30% for 0.1"=20       in western ND on D1, but are generally less than 10% elsewhere=20       through the period. However, light freezing rain accreting above=20       0.01" is possible for much of Montana and the Dakotas.              Weiss                            ...Winter Storm Key Messages are in effect. Please see current=20        Key Messages below...              https://urldefense.com/v3/__https://www.wpc.ncep.noaa.gov/key_messages/Late=       stKeyMessage_1.png__;!!DZ3fjg!_zv2HEUaCxHmrxcjxPpQ_d45hb_EFdwDQXzo01Egj7qkP=       UXe0KoqO0O81tc8GJAqH6nRw9ZPdRN7lhhSqjXZph7rlAQ$=20              https://urldefense.com/v3/__https://www.wpc.ncep.noaa.gov/key_messages/Late=       stKeyMessage_2.png__;!!DZ3fjg!_zv2HEUaCxHmrxcjxPpQ_d45hb_EFdwDQXzo01Egj7qkP=       UXe0KoqO0O81tc8GJAqH6nRw9ZPdRN7lhhSqjXZerjYTzs$=20                            $$              =3D =3D =3D       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 70       SEEN-BY: 220/90 221/1 6 360 226/17 18 20 30 44 50 227/114 229/110       SEEN-BY: 229/134 206 300 307 317 400 426 428 470 664 700 705 266/512       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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