


Quantitative Precipitation Forecast
Issued by NWS
Issued by NWS
882 FOUS11 KWBC 150721 QPFHSD Probabilistic Heavy Snow and Icing Discussion NWS Weather Prediction Center College Park MD 321 AM EDT Wed Oct 15 2025 Valid 12Z Wed Oct 15 2025 - 12Z Sat Oct 18 2025 ...Central Great Basin & Northern Rockies... Days 1-2... A potent closed upper low, which impacted California and the Sierra to start the week is forecast to cross the central Great Basin today before lifting across the northern Rockies on Thursday. As it does so, it is also forecast to gradually weaken, but still provide ample broad scale upper ascent over the region. The greatest potential for moderate to locally heavy snow will likely be situated directly underneath the aforementioned upper low where the greatest lift and steepest lapse rates exist. The 00z HREF shows this potential for 1-2"/hr snowfall rates across the high terrain throughout north-central and northeast NV between 18Z-00Z today as snow levels drop as low as 7,000ft. For the northern Rockies, strong south-southwesterly upslope flow into the WY and UT mountain ranges will provide for more longevity of moderate high elevation snowfall ahead of the mid-upper low on Thursday. This includes the Tetons, Absarokas, Bighorns, Wind River Range, as well as the Wasatch and Uintas of UT. Snow levels will start out fairly high and around 9,000ft before dropping to around 7,000ft for areas underneath the mid-upper low as it pushes northeastward. Snow should taper off by Thursday night as the system quickly exits into the northern Plains and dry northwesterly flow becomes the dominant regime again for the time being. WPC probabilities for at least 8 inches of snow for this event are moderate-to-high (50-80%) across the Ruby Mts of northeast NV, as well as many of the ranges surrounding Yellowstone NP, the WY Bighorns, and the Uintas of UT. Most of these higher probabilities reside over regions higher than 9,000ft in elevation. The probability of significant freezing rain across CONUS is less than 10 percent. Snell $$