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From | To | Subject | Date/Time | |||
Mike Powell | All | HVYSNOW: Probabilistic He |
November 17, 2024 12:23 PM * |
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FOUS11 KWBC 170812 QPFHSD Probabilistic Heavy Snow and Icing Discussion NWS Weather Prediction Center College Park MD 312 AM EST Sun Nov 17 2024 Valid 12Z Sun Nov 17 2024 - 12Z Wed Nov 20 2024 ...Western U.S.... Days 1-3... A developing active pattern is in its early stages as the first in a series of Pacific storm systems revolves beneath the base of a longwave trough that will become quasi-stationary in the Gulf of Alaska to start the period. Then, as a strong ridge builds over the Aleutians mid-week, the longwave trough will dive south into the northeast Pacific and direct a steady barrage of rich Pacific moisture at the region into the second half of the week. Tonight, the warm front associated with the initial surge in Pacific moisture is working across the interior Northwest. Meanwhile, a cold front will push across western WA/OR Sunday morning that will cause snow levels to plummet to as low as 2,000ft in the WA Cascades and 2,500ft in the OR Cascades by this afternoon. By Sunday evening, some locations on the windward side of the Cascades could see snow levels as low as 1,000ft. It is also worth noting that there are likely to be some instances of freezing rain today with low-moderate probabilities for >0.01" of freezing rain in parts of eastern OR and the northern ID Panhandle. The falling snow levels will occur well inland across the Northern Rockies Sunday night and into Monday. NAEFS shows 500-700mb temps and heights that are below the 10th percentile throughout the Northwest on Monday. This unusually cold air-mass is in place at the same time as persistent onshore flow, courtesy of the longwave trough to the north, strikes mountain ranges such as the Cascades at an orthogonal angle to maximize the snowfall potential through Monday. Following a brief lull Monday night, a rapidly strengthening storm system (both the GFS and ECMWF have the low sub 950mb by Tuesday afternoon!) will direct a stronger atmospheric river at the Pacific Northwest with not only exceptional moisture advection (>750 kg/m/s IVT on NAEFS would be above the 97.5 climatological percentile Tuesday afternoon), but intense winds along the mountainous terrain. Robust warm air-advection late Tuesday and into Tuesday night will lead to snow levels rising to above 3,000ft in the WA Cascades and Olympics, around 4,000ft in the OR Cascades, and 6,000ft in the northern California ranges by Wednesday morning. The concern would be for the potential for a heavier/wet snow type to rapidly accumulate, while powerful wind gusts potential lead to tree damage and power outages Tuesday night and into Wednesday. All told, there is no shortage of snow in the forecast for the Pacific Northwest and Northern Rockies. Snow is likely to be measured in feet along not just the Cascades above 3,000ft, but the Olympics, the Salmon/Shasta/Siskiyou of northern California, and well inland through the Blue, Sawtooth, Boise, Bitterroot, Tetons, and Lewis Mountain Ranges. The latest WSSI shows Moderate to Major Impacts in the Cascades and Bitterroots with impacts including not just dangerous travel conditions (including notable Cascade passes), but the weight of the snow and strong winds by Tuesday night could result in tree damage and power outages in some areas. ...Northern Plains... Day 3... Confidence is increasing in a powerful late November cyclone to track from the Southern Plains on Monday and race north into the Midwest Monday night. Both NAEFS and ECMWF SATs support a highly anomalous area of low pressure Monday night, but the ECMWF is farther west and closer to the Missouri River than the NAEFS, which is located farther east over central Iowa. By Tuesday morning, the NAEFS (a GFS/CMC ensemble based tool) shows the storm about to cross the Mississippi River in southeast MN while the ECMWF is over southwest MN. The primary reason for this is the ECMWF shows a slightly slower and stronger 500mb solution than the GFS, albeit they are not overly different in the storm evolution. Where they differ is that the ECMWF (RGEM as well) phases sooner with an upper level disturbance over the northern High Plains and is pulled farther west than the GFS. By 21Z Tuesday, both the ECMWF and RGEM show a closed 500mb low near Bismarck, while the GFS is more elongated and does not close off fully until a few hours later near the ND/Canada border. These details are critical in determining where the deformation zone (or heaviest snow bands) set up; over the Dakotas or more over south-central Canada. For the moment, WPC PWPF shows moderate-high probabilities (50-70%) for >4" of snowfall over north-central ND. It is worth noting that the WPC PWPF does show low chances (10-30%) for snowfall >8", and near the North Dakota/Canada border, a small 10% chance area for >12" of snowfall. Residents in the Dakotas should monitor the forecast closely over the next 24-48 hours. While exact amounts are unclear, the exceptionally strong storm system over Minnesota coupled with high pressure building in over the Northern Rockies will make for a very windy setup over the Northern Plains. Snow is still expected to fall across much of central and western North Dakota and wind gusts of 30-40 mph would result in whiteout conditions for areas that, in some cases, would experience their first round of accumulating snowfall this season. The Probabilistic WSSI (WSSI-P) shows moderate-high chances (50-70%) for Minor Impacts across much of central North Dakota with the highest probabilities focused in north-central North Dakota. The WSSI-P shows Snow Amount and Blowing Snow to be the primary impacts in these areas. In summary, while exact amounts remain low confidence at this range, the combination of some accumulating snow and hazardous visibility reductions due to blowing snow are still likely to cause some treacherous travel conditions in these areas late Tuesday and into Wednesday morning. The probability of significant ice across the CONUS is less than 10 percent. Mullinax $$ --- SBBSecho 3.20-Linux * Origin: capitolcityonline.net * Telnet/SSH:2022/HTTP (618:250/1) |
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