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Mike Powell | All | HVYSNOW: Storm Key Msgs |
February 10, 2025 9:13 AM * |
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FOUS11 KWBC 100843 QPFHSD Probabilistic Heavy Snow and Icing Discussion NWS Weather Prediction Center College Park MD 343 AM EST Mon Feb 10 2025 Valid 12Z Mon Feb 10 2025 - 12Z Thu Feb 13 2025 ...Great Lakes... Days 1-2... Large surface high pressure stretching from the northern Plains through Mid-Atlantic creates enough of a pressure gradient across the Great Lakes to promote continuing westerly 850mb wind up to 35 kts at times thanks to a couple passing shortwaves. The first shortwave is racing across the Great Lakes and New England this morning with a third impulse speeding across the region Tuesday morning as flat/progressive flow persists across the CONUS. Each of these subsequent shortwaves will be accompanied by a weak cold front, driving enhanced CAA across the Great Lakes to support periods of lake effect snow (LES). On D1, 850mb temps fall to -15C or more, steepening low-level lapse rates sufficiently to lift inversion levels to nearly 10,000 ft, which with ascent maximizing into the lowering DGZ will cause bands of heavy snow with rates of 1"/hr or more across the U.P. of MI, as well as SE of Lake Ontario and into the northern Finger Lakes region early D1 before flow shifts more westerly into the Tug Hill by tonight. WPC probabilities D1 are moderate (40-60%) for 6+ inches along the SE lake shore of Ontario and Tug Hill, as well as across the Keweenaw Peninsula of the U.P. of MI. ...Mid-Mississippi Valley to the Mid-Atlantic... Days 2-3... Confluent mid-level pattern will maintain progressive flow across the CONUS as the next in this parade of storms develops over the Central Plains and Ozarks Monday evening. This system will strengthen in response to vorticity energy shedding from the base of a longwave trough initially over Baja, combining with the RRQ of a southern stream jet streak which begins to amplify and arc meridionally, leaving favorable diffluence atop the mid-level PVA/divergence. The downstream confluence of the northern and southern streams should result in suppression of this wave, keeping it fast and generally flat from west to east, but will also result in significant ascent and a prolonged period of precipitation as isentropic ascent from the Gulf surges northward and spokes of vorticity continue to lag back to the SW leaving a long duration of ascent. The north-south trends with this system appear to have stabilized as most upper features settle into place with only subtle changes in the forecast expected at this point. This aims the heaviest axis of overlapping QPF and subfreezing thermals from northeast KY, through central VA into the Delmarva. Based on current guidance, this is beginning to look like a significant winter event containing snow and sleet and freezing rain, generally from the Ozarks almost due east into the Central Appalachians and the I-95 corridor from Richmond, VA to Baltimore, MD. The downstream confluence of the mid-level pattern will force this generally west-to-east axis of heavy precipitation, with 290-295K isentropic ascent and accompanying WAA fueling the elevated PWs progged by NAEFS to exceed the 90th climatological percentile as far north as the TN VLY and southern Mid-Atlantic (NC/VA border). This will supply plentiful moisture for heavy precipitation, and the sharpening baroclinicity on the WAA leading to impressive 850-700mb fgen will help to concurrently enhance ascent. This suggests that precipitation rates will be heavy at times, although in areas with snow the DGZ appears elevated and the best fgen is well below that, which when combined with modestly "warm" temperatures should keep SLRs low and this could be a heavy and wet snow for most of the area. The end of the latest 00z HREF depicts the potential for snowfall rates up to 1"/hr in the heaviest band. Current WPC probabilities are high (>70%) in northeast KY, the central Appalachians, central VA into southern MD and the central Delmarva D2 for 4+ inches of snow. Medium probs (40-70%) expand northward through northern VA, MD, DE, and southern NJ, with a very tight gradient expected along the northern and southern fringes. This places the highest potential for significant snow between Richmond, VA and Washington, D.C. Farther to the south, there is likely to be a transition zone from rain to snow which will include axes of moderate to heavy freezing rain, especially in the higher elevations around the Ozarks, as well as across portions of the Central Appalachians from eastern KY through SW VA. There remains a lot of uncertainty as to the amounts of icing, especially noting that rates could be heavy at times which don't efficiently accrete, and with the general synoptic uncertainty continuing, but there is high confidence (>70%) for warning-level icing (above 0.25" |
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