Probabilistic Heavy Snow and Icing Discussion NWS Weather Prediction Center College Park MD 431 AM EST Sun Dec 01 2019 Valid 12Z Sun Dec 01 2019 - 12Z Wed Dec 04 2019 ...California to Great Basin and Rocky Mountains... Days 1-3... ...More heavy snow for the California Sierra Nevada Range... An upper low centered west of Oregon will retrograde SW to a position off the northern California coast Sunday. A prolonged and robust Pacific jet will advect copious moisture into California, noted by PWAT anomalies of more than 2 standard deviations above the mean in the GFS both Sunday and Monday. The models and means show a split jet structure with difluent flow aloft resulting in well defined and persistent upper divergence maxima coming onshore and continuing inland into the CA Sierra Nevada mountains. With a secondary max in the northern branch crossing eastern OR into central ID, light to moderate snow are expected in those areas on day 1. On Monday, Day 2, the upper jet starts to gradually ween and move southeast with time, so the strength of the upper divergence maxima weakens over time. This results in lower amounts than day 1 in the CA Sierra and signal the major event will wind down on Monday. Further inland with the upper trough crossing the Pacific northwest towards the northern Rockies, the jet maxima departs ID and comes into Wyoming, where upper divergence maxima supports a period of snow, with several inches in the Tetons and Yellowstone National park. This ends as the upper trough passes the latter half of day 2. On Day 3, the continuation of the Pacific jet coming onshore into southern CA and into the southern CA Sierra Nevada leads to persistent snow, with accumulations up to a foot possible. Over the 3 days, total accumulations may exceed 5 feet in parts of the Sierra, with widespread 6-10" in the terrain of the Great Basin and into Wyoming. There is also the potential for some light freezing rain in the vicinity of the Columbia River Valley in northwest OR and southwest WA. ...Upper Great Lakes... Day 1... The ongoing major winter storm will gradually move eastward, with coupled upper divergence/lower convergence and lake enhancements supporting heavy snow on the north side of this low across northern WI through northern lower MI and the southern UP of MI. Sunday evening. The heaviest snowfall is likely where some lake enhancement is expected on the W side of Lake Michigan. A second maxima is downstream of Lake Huron in northeast lower MI, where the longest duration of deformation occurs. The event tapers later tonight as the deformation bands moves east out of MI as the upper low departs. Further south, a transition of p-types is likely, with a band of mixed sleet and freezing rain across central MI that gradually changes to snow as falling heights lower temperatures aloft. Surface temps are expected to be only at or slightly below freezing, so ice accretion efficiency may be low. Loss of the mid level inversion should end the freezing rain threat tonight. ...Lower Lakes/Mid Atlantic/Northeast... ...Prolonged Snow Event in interior Eastern New York and New England... Days 1-3.. The models indicate strong low-mid level warm advection and moisture advection underneath a well defined upper divergence maxima progressing across western NY and PA downstream across the rest of NY?PA today and southern and central New England thereafter. Where it is cold enough for mostly snow, a band of heavier amounts is expected from Rochester and Syracuse NY down the Mohawk Valley to the Capital District and then the Berkshires and Worcester Hills. Further south a mixture of sleet/freezing rain and rain will occur across southern NY and northern PA into southern New England. As this band of WAA associated with a warm front lifts northeast from PA into Southern New England, moderate to heavy precipitation is likely. Local enhancements to freezing rain are likely in the lee of the Allegheny Mountains of PA until the warming ends the event. Amounts of 0.25" of accretion are expected. Further northeast, more sleet is likely across northern PA to northern NJ and southeast NY and interior CT. Most areas of northeast PA and NJ are likely to start as a quick hit of snow with 1-2" possible. Tonight, a surface low will begin to develop off the NJ coast as energy from the low across the Great Lakes transfers eastward. This low will move slowly east northeast into Monday. Confluent flow north of the developing cyclone produces mid level frontogenesis and a low level jet maxima of 40-50 kt easterly flow across central New England. This should result in heavy snow in the Catskills, Berkshires, southern Green Mountains, and Monadnocks. Precip should change back to snow across the Delaware River Valley, lower Hudson Valley, and Litchfield hills of northwest CT. From the Catskills, into the Berkshires, the Worcester Hills, and Monadnocks of NH, event totals snow could be around 18 inches with locally higher amounts. Closer to the MA coast, amounts will likely be less due to warm air intrusion turning p-type over to IP/ZR for a time, and may be even lower as a dry slot wraps in on Monday, potentially cutting off snowfall for a period of time. On Tuesday, the models show the system turning north and cross the Gulf of Maine, with QPF and snow differences resulting from the cyclone timing and intensity differences. The cluster of models closer to the coast like the NAM, ECMWF, and UKMET are preferred. But each has a different axis and orientation of QPF and resultant snow, so uncertainty is greater than normal and confidence lacking. Late Tuesday, the upper low moves into the Canadian maritime and the lift decreases and the event ends. The probability of 0.25 inches of freezing rain is less than 10 percent days 2 and 3. Petersen