Probabilistic Heavy Snow and Icing Discussion NWS Weather Prediction Center College Park MD 125 PM EST Fri Feb 23 2024 Valid 00Z Sat Feb 24 2024 - 00Z Tue Feb 27 2024 ...The West... Days 1-3... Complex mid-level pattern days 1-2 will evolve into an amplifying trough across the West by Sunday, resulting in an increasingly active period of winter weather within the region. Split flow tonight will manifest as mid-level NW winds within a pinched gradient south of a trough over Alberta moving across the Pacific Northwest, with SW flow expanding across the Desert Southwest downstream of a closed low over the Pacific. A weak col will exist in between resulting in weak shear and minimal across across much of the West. This pattern will persist through Saturday night before amplification begins in response to a potent shortwave and accompanying vorticity maxima diving along the British Columbia coast and moving onshore WA/OR Monday. This will result in a deepening longwave trough across much of the West, with downstream divergence and height falls producing robust synoptic ascent to support expanding precipitation. As this lift intensifies and expands, it will interact with increasing moisture across the region. Two waves of modest IVT are progged to surge into the West according to CW3E probabilities, reaching above 250 kg/ms in the northern tier (above +1 sigma according to NAEFS) and approaching 500 kg/ms late in the period in the Great Basin and Desert Southwest. This enhanced moisture will be acted upon by the deep layer ascent to produce expanding precipitation from NW to SE, aided by a potent surface cold front which will dig across the Pacific Northwest, reaching the Great Basin by Monday evening. This cold front will not only produce additional lift through low-level convergence, but will also cause a rapid drop in snow levels from generally 3500-5000 ft late D2, to below 500 ft in the WA/ID/MT, and around 2000 ft just behind the front. The combination of lowering snow levels with robust synoptic lift (aided by periodic upslope flow) and persistent moisture advection will result in heavy snow spreading across much of the terrain of the west by D3, with snow possibly filling into the lowlands and valleys as well. WPC probabilities for more than 6 inches of snow D1 and D2 are above 70%, but confined to the higher terrain of the WA Cascades and Northern Rockies. By D3 the footprint of high (>70%) probabilities for more than 6 inches expands along the OR Cascades, into much of the ID terrain including the Salmon River and Sawtooth Ranges, and into parts of NW WY near the Grand Tetons. Local snowfall during the 3 days will likely exceed 4 feet in the highest terrain, and difficult to dangerous travel is likely at many of the mountain passes by Monday. Finally, there is some potential as well for snow squalls along the cold front as it drops rapidly southeast D3. Along this front, the environment appears favorable for convective snow showers and possible snow squalls as reflected by elevated low-level RH aligned with impressive 0-2km fgen and SBCAPE exceeding 100 J/kg resulting in a high SnSq parameter. It is a bit too early to discern where the greatest threat for snow squalls exists, but the threat for snow squalls with briefly intense snowfall rates and gusty winds leading to difficult travel is increasing for parts of the Northwest, Great Basin, and Central Rockies. ...Ohio Valley... A compact but potent shortwave will dig out of the Great Lakes tonight into Saturday, resulting in a fast moving surface low moving across the Ohio Valley. The antecedent thermal structure is marginal for heavy snow, but impressive ascent combined with cold advection behind this wave will result in a changeover from rain to heavy snow for parts of IN/OH/WV. Snowfall rates may reach 1"/hr at times, which should overcome the warm ground to result in rapid accumulation, but the fast movement and limited spatial extent of this ascent will limit snowfall totals. WPC probabilities have increased, and now feature a 10-20% chance for more than 4 inches of snow in a few areas. The probability of ice accumulations of 0.10 inch or more is less than 10 percent. Weiss