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From | To | Subject | Date/Time | |||
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Mike Powell | All | Powerful Blizzard Storm |
March 4, 2025 6:51 PM * |
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FOUS11 KWBC 041921 QPFHSD Probabilistic Heavy Snow and Icing Discussion NWS Weather Prediction Center College Park MD 221 PM EST Tue Mar 4 2025 Valid 00Z Wed Mar 05 2025 - 00Z Sat Mar 08 2025 ...Central Plains through the Great Lakes and into the Northeast... Days 1-3.. ...Powerful storm to bring blizzard conditions to portions of the Central Plains and Upper Midwest... A rapidly strengthening surface low pressure is clearly evident on the WV imagery this morning across the Central Plains, and it is this feature which will bring a powerful blizzard to portions of the country through mid-week. This surface low will traverse northeast and begin to occlude tonight as the anomalous upper low (850-700mb height anomalies falling to nearly -5 sigma and below the minimum in the CFSR climatology according to NAEFS) stacks vertically and crawls northeast, reaching the Great Lakes by Wednesday aftn. Later Wednesday, this upper low will begin to fill and open into a negatively tilted trough, ejecting into Ontario Thursday morning, pushing the attendant cold front and accompanying post-frontal trough eastward through the Mid-Atlantic and Northeast. The intensity of this upper low will help sharpen a jet streak which will rotate through the base of the trough and then lift meridionally from near the Gulf states, placing the favorably diffluent LFQ atop the best height falls to result in maintaining strength of the surface low. This impressive synoptic ascent will also help to draw significant moisture northward from the Gulf, as an arc of PWs above the 97.5 percentile surges northward into the Upper Midwest. This moisture will push north within enhance isentropic ascent, and this is progged to lift into an impressive TROWAL, especially from IA through the Great Lakes on D1 /Tuesday night into Wednesday/. This TROWAL is likely to overlap with a strengthen deformation axis collocated with strong frontogenesis and a deepening DGZ (SREF 100mb depth probabilities 30-50%) suggesting a stripe of heavy snow is likely from NW MO through the western Great Lakes. This is additionally supported by the WPC prototype snowband tool indicating nearly a 100% chance of 1-2"/hr snowfall rates within this band. Significant moisture, plentiful ascent, and a deep low pressure all indicate that an impressive swath of precipitation will spread from the Central Plains through the western Great Lakes D1, with the primary challenge being where the snow/rain line will setup. Guidance suggests the precip will begin as rain along and southeast of a line from near Marquette, MI, to Minneapolis, MN, through all of Iowa and into eastern KS. However, as the low continues to deepen and pulls east, the resultant CAA combined with the ageostrophic flow into the low will transition rain to snow quickly, with the heavy snow then collapsing east through Wednesday. The heaviest snow accumulations will occur within this collapsing band of snow, and although amounts aren't expected to be extreme, impressive winds of more than 50mph will create major impacts due to blizzard conditions from snow that has a high chance (>70%) of exceeding 6 inches from far NW Iowa through the Twin Cities of MN and into the western U.P of MI. Locally 12+ inches of snow is likely in the U.P. As the low fills and moves more rapidly to the northeast and into Canada D2, the attendant cold front and post-frontal trough will race eastward producing a period of strong CAA on NW flow in its wake. This will likely result in periods of moderate to at times heavy snow, especially in the favored upslope regions in the Central Appalachians and Adirondacks. WPC probabilities for more than 4 inches of snow as moderate (30-50%) in the Central Appalachians, and 30-50% for 2+ inches along the Chautauqua Ridge and into the Tug Hill Plateau/Adirondacks. This system has prompted the issuance of Key Messages which are linked below. Then during D3 /Thursday night and Friday/ another potent surface low will emerge from the Central Rockies and race eastward as it becomes embedded within more confluent downstream flow towards the Ohio Valley. Ridging immediately downstream of this feature will somewhat limit moisture return from the Gulf, and the accompanying mid-level wave is progged to weaken rapidly into the flatter flow east. Despite that, a swath of heavy snow north of the low track is expected as some strung out 700-600mb fgen aligns west to east to enhance ascent from Nebraska through Iowa and potentially as far east as lower Michigan. There is considerable uncertainty and spread with both the timing and intensity of this second low, leading to lower confidence in the footprint of snow and resultant impacts. However, at this time, WPC probabilities for more than 4 inches of snow peak around 50% in northern Nebraska. ...California, Great Basin, Southwest, and central Rockies... Days 1-3... A progressive upper level trough will move into the West Coast Wednesday afternoon, then reorganize over the Rockies through Friday. As it reorganizes, its forward motion will slow considerably, allowing cold air to pool over the West as Pacific moisture advects into the region, resulting in areas of heavy snow. Multiple embedded shortwaves will rotate around the trough, which will support more widespread snow over several Western states. On Wednesday, a pair of jet streaks will further enhance the lift over California, with the southern Sierras in both the left exit region of one and the right entrance region of another. Ahead of the upper level trough, a surface cold front will move south and east off the Pacific and into the West Coast. The front will have a limited tropical connection, increasing the moisture flux into southern California. IVT values will peak around 400 kg/ms. That Pacific moisture will rising into the 99th percentile compared to climatology as it moves into southern California on Wednesday. As this moisture pushes inland, the southern Sierras will get the first opportunity to uplift that moisture in the form of heavy snow. WPC probabilities are the highest in this region, with a moderate (40-60%) chance of 18 or more inches of snow. As the trough moves inland, the moisture moving northeastward ahead of it will cause widespread mountain snow and valley rain and snow across much of the Intermountain West through Thursday. A surface low will develop over northeastern Nevada and move across Utah and southern Wyoming through Thursday in response to the forcing from the upper level trough and embedded shortwaves. The trough will become more consolidated as an upper level low tries to form within it on Thursday. This will increase the divergence in the left exit region of the jet which will have moved into the Four Corners region on Thursday. That jet streak will have embedded winds over 130 kt, so it will have plenty of energy for that surface low to work with. The highest probabilities through Thursday night east of the Sierras will be across the Uintas of northeast Utah and the Wind River Range of central Wyoming, where there's a high (70-90%) chance of 8 inches or more of snow. Lower (20-50%) chances of 8 inches of snow extending in a broad swath of the West from Nevada northeast through Colorado and Wyoming, including some lower elevations. Colder air associated with the trough will get time to settle as the upper level trough/low stalls and reorganizes. A surface low will develop over the Colorado Plains Thursday evening. This low will take over as the primary forcing for the heaviest snow as the snow shifts east across Nebraska along with the low. By Friday morning, all organized heavy precipitation will have moves east and out of the region. A secondary small low may cause a brief burst of heavy snow over northern Arizona during the day Friday for the higher elevations along the Mogollon Rim. Weiss/Wegman ...Winter Storm Key Messages are in effect. Please see current Key Messages below... https://www.wpc.ncep.noaa.gov/key_messages/La... $$ --- SBBSecho 3.20-Linux * Origin: capitolcityonline.net * Telnet/SSH:2022/HTTP (618:250/1) |
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