Probabilistic Heavy Snow and Icing Discussion NWS Weather Prediction Center College Park MD 355 PM EST Tue Mar 02 2021 Valid 00Z Wed Mar 03 2021 - 00Z Sat Mar 06 2021 ...Northern New York/Vermont... Day 1... A low will move across southern Ontario and then southern Quebec to just north of Vermont Wednesday before decaying as it moves towards Maine. The trailing front south of the low crosses northern NY and VT. The post-frontal flow becomes westerly, with moist upslope flow coming into both the Tug Hill and NY Adirondack Mountains, followed by the northern green Mountains of VT. Where ascent corresponds to the enhanced moisture in northern NY, several inches of snow are expected. The veering flow turns to the north tomorrow night, with drying aloft simultaneously occurring. As a result, snow shower coverage and intensity should quickly wane Wed night to Thu morning. WPC probabilities for 4 inches are as high as 60% in the northern Adirondacks. ...CO Rockies... Days 2-3... A low-mid level circulation moves from Southern California and across eastern UT and C. Enhanced low level convergence/ascent near the 700 mb circulation center crosses southern Utah, the Four Corners and the ranges of CO, leading to a period of snow across the mountains, with the higher QPF centered on the San Juan Mountains, where the strongest 700 mb convergence is forecast. Secondary snow accumulation maxima are forecast in other ranges of western to central CO, and Wasatch of southern Utah. WPC probabilities indicate a high likelihood for 4" in the San Juan Mountains, and moderate in the southern Wasatch, central Mogollon, and other CO ranges. The event winds down Thu as the 700 mb low moves east across the high plains, with ascent departing the mountains. ...Pacific Northwest... Day 3... A closed mid-level low is expected to linger off the coast of Washington and Oregon Thursday night and Friday. East of the low a Pacific jet streak and warm/moist mid-level SW flow extends from the coast of northern CA across western OR and WA. The slow eastward progression of the low will allow for slow movement of the bands of precipitation across western WA and OR. Heavy amounts of precipitation are possible in the mountains due to the combination of enhanced moisture in the low level jet and ascent from both the approaching front and also orographic lift in windward terrain. However, the southerly component of flow leading to warming, with snow levels likely to climb above 4000 ft, limiting significant snowfall to the Olympics and far northern Cascades, where 1 to 2 feet of snow is possible in the highest terrain. The probability of 8 inches is high in the WA Olympics. becoming moderate in the northern WA Cascades. For Days 1-3, the probability of significant icing (0.25 inch or greater) is less than 10 percent. Petersen