Probabilistic Heavy Snow and Icing Discussion NWS Weather Prediction Center College Park MD 315 PM EST Mon Feb 14 2022 Valid 00Z Tue Feb 15 2022 - 00Z Fri Feb 18 2022 ...Pacific Northwest through the Rockies... Days 1-3... A potent closed low dropping out of the Gulf of Alaska will move into the Pacific Northwest Tuesday morning /early D1/ and then maintain amplitude as it shifts southward along the Pacific Coast into the southern Great Basin Wednesday morning. This closed low will then open as it shifts eastward across the Four Corners and then into the Central Plains D3, but immediately in its wake a secondary shortwave will race out of Alberta to elongate the mid-level trough across the Central and Southern Rockies D2 into D3. This evolution will lead to an amplified, but positively tilted, mid and upper level trough, through which jet streaks will intensify to produce a coupled jet structure to intensify ascent across much of the Intermountain West. This combined with at least modest upslope enhancement behind a surface cold front, especially into the Central/Southern Rockies, should produce heavy snowfall, which will be only limited by modest available column moisture. On D1, widespread precipitation is likely from the OR Cascades southward through the Sierra and then through the Great Basin and into the Northern Rockies. With snow levels generally 5000-6000 ft during the period of most robust ascent aided by WAA, the heaviest snow should be confined above these levels, and WPC probabilities for 6+ inches are above 30% only in the Sierra and higher terrain of the Absaroka range. By D2, the evolution of the mid-level features will produce the most robust ascent across Wyoming, with heavy snowfall likely encompassing much of the state except the valleys below 4000 ft. WPC probabilities for more than 6 inches are above 40% in many of the ranges, with locally up to 12" possible in the Wind River range. By D3 /Wednesday night and Thursday/ the heaviest snow is expected to shift into the Central and Southern Rockies including the Front Range, Sangre De Cristos, and San Juans, where WPC probabilities feature a moderate risk for 6+ inches of snowfall, with local amounts to 10" likely. In the lower terrain, D3 probabilities for 2 inches reach 50% across the western High Plains of WY and CO, including the I-25 corridor and as far south as the White Mountains of AZ. ...Central Plains to Great Lakes... Day 3... A closed mid-level low ejecting out of the Four Corners will gradually open into a negatively tilted trough across the Central/Southern Plains Thursday before lifting northeast towards the Great Lakes. As this wave shifts eastward, it will shed a vorticity lobe back into the Desert Southwest, while a piece of northern stream energy drops out of Saskatchewan, and this latter shortwave may interact or phase with the leading piece of the closed low across the Upper Midwest Thursday night. The net result of this complex evolution is a longwave, positively tilted, trough draped from the Great Lakes through the Southwest, with a pronounced subtropical jet streak arcing across the Southern tier interacting with a departing jet streak into Canada. Both of these jets are likely to strengthen, with increased coupling leading to surface low development followed by at least modest deepening as the surface low moves from the High Plains of NM into the Mid-Mississippi Valley. This surface low is likely to move northeast along a surface cold front, and ahead of this front, warm and moist advection will become impressive noted by 850mb winds of 30-50 kts driving PWs to more than +2 standard deviations above the climo mean. This anomalous moisture acted upon by robust synoptic ascent should produce a swath of heavy precipitation, with rain, snow, sleet, and freezing rain all likely. While guidance continues to feature quite a bit of latitudinal spread, mostly in response to different intensities and positions of the upper jet streaks, the guidance in general has trended a bit stronger and further NW, towards the GFS/NAM camp. This implies a heavy swath of snowfall from far northern Oklahoma through eastern KS, northern MO, and then northeast into the Great Lakes. WPC probabilities for more than 4 inches of snow is above 50% across much of this area, including Kansas City, MO and Chicago, IL. Within this area of heavy snow, some accumulations of greater than 8 inches appear likely as mid-level fgen and deformation overlap within a deepening DGZ to suggest banded structures, and the WSE 90th% is over 12 inches within this swath. South of this heavy snow axis, a corridor of sleet and freezing rain is likely as the warm nose persists even as CAA behind the front drops surface temperatures below freezing. As with most mixed p-type events, there remains uncertainty into the depth of the cold nose and strength of the warm nose, so the demarcation between IP and ZR is uncertain. However, some models are predicting more sleet than freezing rain due to the intensity of the CAA, which would limit freezing rain accretions. Still, WPC probabilities for 0.1" of freezing rain are as high as 40% in a small area north of Saint Louis, MO, with a broad swath of more than 10% extending from southeast KS through the southern L.P of Michigan, including Detroit. Weiss