Probabilistic Heavy Snow and Icing Discussion NWS Weather Prediction Center College Park MD 325 PM EST Wed Feb 19 2020 Valid 00Z Thu Feb 20 2020 - 00Z Sun Feb 23 2020 ...Central Plains and Rockies... Day 1... Low pressure developing in response to a departing jet streak in the Lee of the Rockies will spread snowfall into the High Plains of Colorado and Kansas, with low-level easterly flow supporting upslope enhancement into the Sangre De Cristos. Most of this snow should be light as the low-level surface feature drops quickly southward and the jet streak escapes eastward, bringing an end to the strong synoptic forcing. WPC probabilities for 4 inches are low in the SE Plains of CO. Into the terrain, however, the upslope enhancement will persist as the low drops southward, and WPC probabilities feature isolated high risk for 6 inches in the highest terrain. ...Great Lakes... Day 1... Strong cold advection behind a cold front will spread NW flow within the CAA across the Great Lakes tonight into Thursday. While the duration of this favorable CAA to produce LES will be limited, it will also be robust, with effective fetch from lake Superior and Huron aiding with the snowfall downwind of Lake Ontario. A period of heavy snowfall is likely SE of Lake Ontario, and WPC probabilities are high for 4 inches, and may locally exceed 8". ...Southern Appalachians and Mid Atlantic... Days 1-2... Guidance coming into much better agreement this afternoon in the evolution of a positively tilted upper trough and surface low affecting the Southern Appalachians and into NC/VA. Outside of the NAM, there is good consensus that mid-level WAA ahead of the upper trough will spread moisture northeast across the area atop a surface cold front which will sag into South Carolina and off the coast. At the same time, jet streak energy will merge and intensify to 170+kts as it exits near New England, leaving the diffluent RRQ atop the Carolinas, supporting ventilation to lower pressure and spawn cyclogenesis along the baroclinic zone offshore. The combination of all these features will produce widespread precipitation across the area, with cold air advection slowly transitioning p-type from rain to snow. The low-level thermal profile will be marginal, and antecedent conditions are unfavorable to snow accumulations, however, robust forcing, especially within an intensifying mid-level frontogenetic band pivoting across NC/VA will overcome these marginal conditions to produce a period of heavy snow. The most likely locations for heavy snowfall exceeding 4 inches will be in the terrain of NC/TN, with a secondary maximum possible in northeast NC where the longest duration of precipitation falling into the colder air will occur. Additionally, guidance indicates the potential for a band of snow to rotate eastward as the low pulls away Friday morning, which could also enhance snowfall locally. WPC probabilities for 4 inches are around 20% in the mountains, and 30-40% in northeast NC/far southeast VA. ...Southern Great Basin... Day 3... An upper low and associated surface wave will approach the Southern California coast Friday before moving onshore. Moisture will spread inland on southerly warm/moist advection ahead of this feature, but at the same time will drive snow levels to 6000 ft or higher. Moisture becomes significant as evidenced by PWAT anomalies reaching +2 to +3 standard deviations above the climo mean, but modest forcing and the high snow levels confine WPC probabilities for 6 inches to moderate/high in the Sierra and southern Wasatch ranges. For Days 1-3, the probability of significant icing (0.25-inch or greater) is less than 10 percent. Weiss