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From | To | Subject | Date/Time | |||
Mike Powell | All | HVYSNOW: Probabilistic He |
November 22, 2024 9:25 AM * |
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FOUS11 KWBC 220831 QPFHSD Probabilistic Heavy Snow and Icing Discussion NWS Weather Prediction Center College Park MD 331 AM EST Fri Nov 22 2024 Valid 12Z Fri Nov 22 2024 - 12Z Mon Nov 25 2024 ...Pacific Coast through the Interior Northwest and Great Basin... Days 1-3... Persistent closed low centered off the Pacific Northwest coast will remain energized by vorticity maxima swinging through the associated trough this period. This will result in amplification of the gyre, noted by an expansive region of 500-700mb height anomalies reaching below -1 sigma, and approaching -3 sigma in the core of the trough. Beneath this trough, deepening surface low pressure will approach the WA coast today, but likely get pulled back to the west on Saturday before landfall in response to secondary shortwave energy digging to its south. This will result in persistent onshore and divergent mid-level flow, accompanying upper level jet energy to spread moisture onshore as a continuation of the ongoing atmospheric river (AR) across northern CA through early Saturday. While IVT values exceeding 500 kg/m/s wane and pivot southward by the end of D1, this will still result in plentiful moisture and widespread moderate to at times heavy precipitation pushing onshore the Pacific Coast into the interior Northwest. Snow levels within this AR will be quite high, generally 6000-8000 ft, except east of the WA Cascades on D1 where they will remain entrenched around 4000 ft before rising. This indicates that most of the heavy snow will be above pass levels, except in the higher Cascade Passes D1, and the Sierra Passes D1-D2. WPC probabilities D1 are high for more than 6 inches of snow in the northern WA Cascades, the Salmon River Range, and portions of the Northern Rockies near Glacier NP. On D2, snowfall is more robust and expansive, with a greater than 90% chance of 6 inches again in the Northern Rockies and Salmon River/Sawtooth Ranges. More impressively, the Sierra will be favorably located to be impinged upon by moisture by the end of D1, leading to pronounced upslope snow. WPC probabilities are above 80% for 12+ inches through Saturday, with 2 feet possible above 8000 ft. By D2 onward, snow levels crash again as a cold front pushes onshore, but this is accompanied by reduced moisture advection as the column begins to dry out. Some moderate snow will persist through onshore flow, especially in the Sierra where an additional 6-12 inches is possible, but otherwise WPC probabilities for more than 6 inches are between 30-50% and focused across the Wasatch, Uintas, and ranges of NW WY. ...Appalachians and Northeast... Days 1-2... Impressive upper low over the Northeast will feature a complex evolution through the weekend resulting in a couple surface lows and varying areas of heavy snow. The Central Appalachians, especially from the Laurel Highlands southward across WV and as far south as the Great Smokey Mtns of TN/NC, will benefit from prolonged upslope flow on the western periphery of the upper low resulting in waves of heavy snowfall through Saturday. WPC's snowband probability tracker depicts an extended period of 1-2"/hr snowfall rates during the D1 period across the Allegheny Mtns. WPC probabilities in this area are high (>70%) on D1 for more than 8 inches of snow. Event total snowfall could peak around 2 feet in central WV. The ongoing potent and compact surface low churning near Long Island is forecast to loop westward and eventually toward the south today over eastern PA as it remains embedded within the large 500mb gyre overhead. As this occurs, an impressive plume of low- level moisture will continue to wrap northwest into the system, driving rich theta-e advection into a TROWAL to support some elevated instability and enhance available moisture for heavy precipitation early on D1. Increasing deformation is noted on current radar trends on the W/SW side of the system as it becomes exceptionally wrapped. This setup will support intense mesoscale ascent and bands of heavy precipitation rotating W/SW as the low retrogrades. Although the column will be marginally supportive of accumulating snow outside of higher elevations (above about 1500 ft), the intense lift should dynamically cool the column and allow efficient snowfall accumulation at times even in lower terrain. SLRs for this event will likely be below climo due to near freezing temps and warm soils/compaction, but still, rates of 1-2"/hr will promote heavy accumulations, especially in the Poconos and Catskills and surrounding areas early this morning. Most of the ongoing snowfall is expected to occur before or right around the start of the D1 period (12z Fri), so WPC probabilities don't reflect the ongoing event. Nonetheless, the greatest snowfall amounts are expected in northeast PA and neighboring areas of New York and northern NJ, with 2-day snowfall potentially reaching above 12" in a few highly elevated spots. This will likely result in dangerous travel and impacts to infrastructure including scattered power outages. In the lower elevations of the Mid-Atlantic, some snow bands could pivot as far SE as the I-95 corridor, so while accumulations in the major urban areas from Washington, D.C. to New York City are expected to be minimal, if any, these cities could see their first "falling" snow of the season Friday morning/aftn. Along the Adirondacks, Green, and White Mountains, the upper low will draw moist easterly flow northward and into these ranges Friday night through Saturday while another surface low develops east of Maine and pivots northwest. Snow levels should be high enough that only the highest terrain will receive significant snow, but WPC probabilities have increased and now feature a 30-50% chance on D2 of more than 4 inches, primarily in the White Mountains of NH and the peaks of northern ME. ...Northern Rockies through the Northern Plains... Days 1-2... A shortwave ejecting through the base of an anomalous trough off the Pacific Coast will swing eastward into the Northwest Saturday and then begin to amplify into a potent but fast moving impulse across the Northern Rockies and into the Northern Plains Sunday. This deepening system will drive downstream ascent through height falls, PVA, and divergence. At the same time, a zonally oriented jet streak will pivot south of the region, placing its favorable LFQ atop the far northern High Plains, interacting with increasing baroclinicity as a front wavers near the international border. The overlap of synoptic lift with the enhanced mesoscale ascent through fgen will result in weak cyclogenesis, leading to an expanding area of precipitation falling as snow. The column will be plenty cold for wintry precipitation thanks to high pressure from Canada extending southward, and as the WAA along the warm front lifts north, it will result in an exceptionally deep DGZ to support fluffy aggregate dendrites which should accumulate efficiently. The biggest question remains whether or not this favorable environment and most impactful snowfall will span south over the U.S.-Canada border. The heaviest snowfall is likely in the terrain near the Northern Rockies where upslope flow will enhance ascent, and WPC probabilities support a high risk (>70%) for at least 8 inches near Glacier NP on D2. However, heavy snowfall is also possible farther east across northern MT along the international border D1-D2 where the most robust synoptic ascent will materialize. A leading surge of modest upper diffluence and WAA may lead to a burst of snow today across northwest and northern MT. WPC probabilities for at least 2" on D1 are high throughout northern MT. For the main activity related to the approaching shortwave on D2, the guidance has continued to trend a bit farther north from central MT eastward to ND, with current WPC probabilities suggest around a 30% chance for more than 4 inches right along the international border as far east as north- central MT on D2, with higher probabilities for heavy snowfall located in southern Alberta and Saskatchewan. The probability of significant ice across the CONUS is less than 10 percent. Snell ...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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