Probabilistic Heavy Snow and Icing Discussion NWS Weather Prediction Center College Park MD 447 AM EDT Sun Mar 21 2021 Valid 12Z Sun Mar 21 2021 - 12Z Wed Mar 24 2021 ...Central to Southern Rockies/Southwest into Central High Plains... Days 1-3... On Day 1, snow remains likely across the CO foothills and front range as a mid-upper level trough slowly approaches, with the forward flank upper jet maxima crossing eastern CO into KS. A combination of a well defined and persistent 700 mb convergence maxima helps lift the available moisture, in conjunction with upper divergence maxima and orographics in windward areas to produce moderate to heavy snow. Lee cyclogenesis occurs Sunday night, and this low is likely to lift northeast into the Central Plains by Tuesday morning. As the surface low develops over far NE NM and lifts northeast, low-level flow will turn E/NE, producing upslope enhancement into the Front Range and Palmer Divide, especially Monday morning. The heaviest snow D1-2 is likely in the Front Range and Palmer Divide, extending south into the Sangre DeCristo Mountains of southeast CO. Locally a foot of snow is possible. The thermal profiles east of the terrain are marginal for snowfall, but the likelihood for a deformation axis to enhance ascent to dynamically cool the column should produce a few inches of snow along the I-25 urban corridor and into the high plains of NE CO. On Day 3, Tuesday, the next upper trough crosses NV/AZ on the way to CO/NM. The amplifying trough leads to increasing upper level divergence maxima developing in southern CO and NM. A wave and then circulation develops in southern CO, drifting south into northern NM. Well defined boundary layer convergence occurs along the path of the circulation, peaking Tue night-early Wed morning in southeast CO to northeast NM. The GFS and ECMWF have increased QPF this cycle and potential snow amounts in response to mid level frontogenesis, favorable difluence aloft with embedded 3030 mb divergence maxima, plus east northeast flow coming into the Sangre deCristo Mountains that provide an orographic component to lift. The prolonged ascent leads to locally heavy snow in southeast CO/northeast NM focused along the Sangre DeCristo mountains.The ECMWF/GFS/NAM/UKMET/Canadian global show potential or a foot of snow, and a moderate risk for 8 inches of snow in these areas. Secondary maxima are expected in the southern UT mountains south into the Mogollon Rim of AZ and White Mountains of NM as the trailing cold front and 700 mb trough move south across these areas, with frontal convergence providing lift in the terrain. Forecast amounts are not as high since the sfc-700 mb convergence strength is not as strong as over northeast NM. ...Pacific Northwest through the Northern Rockies... Days 1-3... Well defined and persistent warm/moisture advection occurs across WA into the northern Rockies today into Monday. Peak ascent in the 850-700 mb layer and high layer relative humidity over 90 percent lead to conditions favorable for heavy snow in the WA Olympics and Cascades. The lift is accented by a 300 mb jet max max streaming onshore and across WA state today and tonight. Difluent flow aloft crosses the northern Rockies as well, combining with 700 mb ascent to lead to persistent snow in the ranges of northern ID to northwest MT Sun night to early Mon . Heavy snow remains likely in the terrain of the Olympics and WA/OR Cascades, with 2 day totals locally as high as 2 feet in the northern WA Cascades. WPC probabilities are high for 8 inches. Secondary snowfall maxima are expected in the OR Blue Mountains, and into the Northern Rockies with Day 1 plus Day 2 amounts locally a foot. The jet streak and associated forcing weaken and drop southeast, leading to renewed light snow accumulations in the Absarokas, Tetons, and Big Horns. On Day 3 the remaining snow is expected to be focused on the Wind River Range of WY and Gillette Arch, continuing down to the Laramie Mountains. The approach of a 700 mb ridge towards the Pacific northwest leads to a dry period there. For Days 1-3, the probability of significant icing (0.25 inch or more) is less than 10 percent. Petersen