


Quantitative Precipitation Forecast
Issued by NWS
Issued by NWS
780 FOUS11 KWBC 251712 QPFHSD Probabilistic Heavy Snow and Icing Discussion NWS Weather Prediction Center College Park MD 112 PM EDT Fri Apr 25 2025 Valid 00Z Sat Apr 26 2025 - 00Z Tue Apr 29 2025 ...Sierra Nevada and Great Basin... Days 1-3... An impressive closed mid-level low (NAEFS 500mb height anomalies falling below the 1st percentile) will move onshore southern CA Saturday aftn before slowly filling while lifting northeast through the Great Basin on Sunday. Downstream of these robust height anomalies, significant synoptic lift will occur downstream through height falls, mid-level divergence, and overlapping upper diffluence as the LFQ of a strengthening subtropical jet streak digs through the trough axis and ejects meridionally. The overlap of this ascent into a region moistened by 700mb S/SW flow and an accompanying ribbon of IVT above the 90th percentile (from NAEFS) will result in widespread precipitation Saturday morning through Sunday afternoon. Snow levels during this time will be quite low in response to the anomalous upper low, falling to around 4500 ft, which is nearing the 10th percentile. This suggests that snow will accumulate across much of the CA and Great Basin terrain above this level through Sunday, but at least light accumulations or mixing with snow is possible much lower due to steep lapse rates and dynamic cooling. The heaviest accumulations, however, should remain across the Sierra, where D1 and D2 probabilities for 6+ inches exceed 70%, and 30%, respectively, and locally more than 12 inches is possible before precipitation wanes late D2. As this upper low continues to track northeast, the accompanying moisture and ascent will move across the Great Basin, bringing some light to moderate snow to the higher elevations of NV through Monday morning. WPC probabilities D3 reach as high as 50% for 6+ inches across the Ruby Mountains. ...Northern Rockies... Day 3... The closed low ejecting from the Great Basin will fill and open into a positively tilted trough Monday as it shifts east into the Rockies. Despite this evolution, deep layer ascent will remain impressive as periodic lobes of vorticity swing northeast downstream of the trough axis, and work together with mid-level divergence and upper diffluence in the LFQ of a jet streak arcing into the Northern Plains. Together, this will cause pressure falls over CO/WY leading to surface cyclogenesis, and this low will then track northeast into the Dakotas and Minnesota by the end of D3. While there is good model agreement in the general synoptic setup and evolution, low-clusters from the various ensembles still feature considerable spread in both timing and placement, additionally reflected by modest differences in the primary 500mb EOF on the D3 WPC clusters. The primary driver of these variances appears to be the speed at which this trough opens and ejects, with 2/3 of the ECENS suggesting a lower ejection, while 50% of the GFS members make up the faster end of the envelope, and by the end of D3 there are height differences among the cluster means of more than 80m across the Central High Plains. At this time, a solution somewhere between the camps as a consensus is probably best. While the exact placement of the low and its associated synoptic forcings will be critical, a cold front digging south through the Northern Rockies Sunday night into Monday will likely interact with an inverted surface trough, leading to enhanced ascent across parts of MT and WY D3. This is likely to occur regardless of the low evolution, but a slower system may produce more enhanced ascent and stronger accompanying deformation than a faster ejecting system. Either way, impressively combined upslope with fgen should result in heavy snow rates, with dynamic cooling response to the column occurring even outside of the higher terrain. Snow levels will be generally low anyway, (near the NBM 10th percentile after coordination with the local WFOs), suggesting that while the heaviest accumulation will remain above 5500 ft, significant accumulations are possible to 4500 ft, and lighter accumulations even lower than that. This is reflected by WPC probabilities that are high (>70%) D3 across the Big Horns, Absarokas, and other terrain around Yellowstone NP, but also much more widespread moderate probabilities for 2" expanding across much of the ID/MT/WY juncture. The probability of at least 0.10" of freezing rain across CONUS is less than 10%. Weiss $$