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From | To | Subject | Date/Time | |||
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Mike Powell | All | HVYSNOW: Probabilistic He |
December 15, 2024 9:34 AM * |
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FOUS11 KWBC 150727 QPFHSD Probabilistic Heavy Snow and Icing Discussion NWS Weather Prediction Center College Park MD 227 AM EST Sun Dec 15 2024 Valid 12Z Sun Dec 15 2024 - 12Z Wed Dec 18 2024 ...Pacific Northwest through the Northern Rockies... Days 1-3... An active period of weather will bring periods of of heavy snow to much of the region through the middle of next week. The period begins with a broad longwave mid-level trough centered over the Rockies. Within this trough, a modest shortwave impulse and accompanying vorticity maxima will be shedding northeast into the Northern Rockies, interacting with modest downstream moisture reflected by near-normal PWs according to NAEFS. This will spread a swath of precipitation across ID/WY/MT the first half of D1 before an approaching shortwave ridge brings an end to the precipitation. Most of this precipitation will be light, with the exception likely in the vicinity of NW WY/Tetons where upslope flow and some enhanced fgen will drive heavier rates and greater snowfall accumulations. WPC probabilities D1 for more than 8 inches of snow are high, above 70%, in the Tetons and adjacent Absarokas to the north. Behind this first shortwave, the aforementioned shortwave ridging will cause a brief respite to precipitation in the Pacific Northwest, but this will come to an end by the start of D2 as another amplified closed low drifts eastward across the Pacific Ocean. Downstream of this low, mid-level divergence will approach the coast Monday morning, with periodic PVA through shedding vorticity lobes helping to enhance ascent. The downstream SW/WAA ahead of this feature will surge moisture back onshore as well, reflected by IVT approaching the 97th percentile as both GEFS and ECENS probabilities for IVT of 500 kg/m/s reach 20-30%. This will spread heavier precipitation back onshore the Pacific Northwest, with snow falling above generally 3000 ft in the Cascades, and spilling into the interior Northwest where snow levels will be even lower, around 1500 ft. This will result in moderate to heavy snow from the Shasta/Siskiyou/Klamath region of CA northward along the Cascades and as far inland as the Blue Mountains and Salmon River range. Across these areas, WPC probabilities are moderate to high (50-70%) for at least 8 inches of snow, and locally more than 12 inches is likely (>70%) in the highest terrain of the OR Cascades and near Mt. Shasta. During D3, a warm front just offshore will lift northward, and the accompanying precipitation will follow on enhanced WAA lifting across OR/ID/WA. The intensity of this precipitation should generally be lighter in the snow areas than on D2, but additional accumulations exceeding 6 inches are possible (30-50%), highest in the WA Cascades. ...Central Appalachians... Day 1... Weakening surface low pressure moving across the OH VLY will spread downstream moisture northward into the Central Appalachians and Mid-Atlantic States. This moisture will surge northward on intensifying 295K isentropic ascent, lifting atop a retreating but still expansive high pressure centered over New England and its resultant wedge east of the Appalachians. As the high retreats and the surface low weakens while moving eastward, low-level flow will veer to become primarily S/SE, not ideal for locking in any low- level cold air. This suggests that while precipitation will begin wintry (snow/sleet/freezing rain) in most areas from the highest elevations of SC northward, it will quickly turn to rain outside of the higher terrain. Even in the Mid-Atlantic and Northeast as far southeast as the I-95 corridor, precipitation may start as a brief period of sleet or snow before turning to rain. This will limit wintry accumulation in many areas. However, in the higher terrain of WV, through the MD Panhandle, and into the Laurel Highlands, a prolonged period of freezing rain is likely, which will accrete to moderate to substantial ice amounts through Sunday night. Some modest conditional instability reflected by theta-e lapse rates around 0C/km will support at times briefly heavy rain rates, somewhat limiting the accretion potential (especially without any dry-bulbing affects), but prolonged duration of freezing rain has still bumped WPC probabilities to moderate (30-50%) for 0.25" centered near the MD Panhandle, with high probabilities (>70%) for at least 0.01" stretched from NC northward along the Appalachians into Upstate NY. ...Northern Plains... Days 1-2... A wave of low pressure moving from MT through MN Sunday into Monday will deepen in response to a mid-level shortwave closing off overhead, collocated with the LFQ of a modest but poleward arcing jet streak. As this low slowly intensifies, the downstream plume of rich theta-e air spreading northward from the Gulf of Mexico will begin to wrap cyclonically around the low, potentially supporting modest TROWAL development pivoting into far northern ND and northern MN Sunday night. The leading WAA ahead of this developing low will likely result in some modest freezing rain across far western ND and eastern MT early D1 due to lack of saturation within the DGZ, but WPC probabilities on D1 are above 70% for at least some icing, with a narrow channel of 10-30% near the ND/MT border for 0.1 inches. More impressive is likely to be the snowfall on the northern edge of this system as it progresses east, with snow becoming more intense Monday from eastern ND through northern MN. Here, elevated instability beneath the TROWAL combined with modest deformation could result in banded snow structures, offsetting otherwise modest omega present within the column. There is still some uncertainty into how much snow may result as precipitation expands and intensifies Monday, but WPC probabilities have increased and are 50-70% from northern ND across into northern MN for 2+ inches, and the WSE plumes do suggest at least a low-end potential for 4-5 inches in some areas. Regardless of the intensity and amounts of snow, hazardous travel is likely as fluffy SLR snow combines with gusty winds to cause snow covered roads with restricted visibility, but WSSI-P for moderate impacts remains quite low for this area suggesting primarily minor impacts. Weiss $$ --- SBBSecho 3.20-Linux * Origin: capitolcityonline.net * Telnet/SSH:2022/HTTP (618:250/1) |
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