Probabilistic Heavy Snow and Icing Discussion NWS Weather Prediction Center College Park MD 320 PM EST Mon Jan 07 2019 Valid 00Z Tue Jan 08 2019 - 00Z Fri Jan 11 2019 ...Great Lakes across northern PA/upstate New York and New England... Days 1-3... The wave causing snow and mixed winter precip types across the upper Great Lakes moves east across Northern New York and northern New England through Tuesday. Low-mid level warm advection and convergence associated with a warm front lifting northeast will result in snow, sleet, and freezing rain as the warming results in a precip type transition. Moderate WPC probabilities exist for 4 inches of snow from the Adirondacks of NY eastward across the Green and White Mountains and terrain of western Maine. Farther southwest, moderate WPC probabilities for a tenth inch ice exist over the the Tug Hill Plateau, portions of the Adirondacks, and down in north-central PA. On Tuesday, a surface low is forecast to develop near Lake Ontario and move into northern New York and New England, with a triple point low developing near the southern Maine coast around Wed morning. Another round of snow driven by low-mid level warm advection and convergence crosses northern New York and northern New England, followed by the cessation of warm advection as the mid level circulation arrives. With the arrival of the circulation, cold air advection begins and allows the precip to stay as snow in northern Maine. The heavier snow is expected over Maine due to longer duration of snow. The event winds down as the low moves off the Maine coast later Wed. Post frontal lake effect snow is likely in a cold advection pattern starting Tues evening with low level convergence in the lee of lakes Superior and northern Lake Michigan. On Wed, continuing low level convergence and cross-lake flow supports additional accumulating snow in the UP of MI and northwest lower MI, and developing off Lakes Erie and Ontario. Relatively higher amounts are expected with longer duration snows in the western UP of MI. On Thu, moist northwest flow with bands of low level convergence favors snow showers in the lee of Lake Erie in northwest PA/adjacent southwest NY, off the southeast corner of Lake Ontario, and in windward terrain of the Tug Hill and Western Adirondacks/northern Green Mountains. Activity winds down off Lake Superior as a low level ridge builds in from the upper MS Valley, advecting drier air into the region and weakening near shore convergence. ...Northern California/Pacific Northwest/Northern Rockies... Days 1-3... A slow moving, deep area of low pressure drifting northeast across the Pacific will support deep southerly flow advecting warm and moist air into northern CA and the Pacific Northwest. As a result, snow levels will climb. Heavy snow is likely at higher elevations of the Shastas/Sisykiyous and OR/WA Cascades. The models are hitting windward terrain in the Shastas hard with potential for a couple of feet of snow at higher elevations over this period. Secondary maxima are expected over the northern WA Cascades, where a foot or two of snow is expected. Since the system is slow to move east, lower amounts are expected downstream in the northern Rockies, with several inches likely from the OR Blue Mountains to the ranges of ID and northwest MT. There is an increasing threat for freezing rain across portions of the the Cascades of Washington and Oregon and lee areas on Tuesday. Cold surface temperatures will be reinforced by easterly winds banking against the Cascades, which will support freezing rain as warm air advection aloft produces widespread precipitation. The current model suite is in good agreement for significant ice accretion in or east of the Cascades, and WPC probabilities show a possibility of a quarter inch of icing. Light icing may also occur in the Columbia River Gorge Tuesday into Wednesday. The uncertainty revolves around multiple precip types and duration of each type. The probability of a quarter inch of icing is less than 10 percent on day 3. Petersen