Probabilistic Heavy Snow and Icing Discussion NWS Weather Prediction Center College Park MD 455 PM EDT Fri Apr 28 2023 Valid 00Z Sat Apr 29 2023 - 00Z Tue May 02 2023 ...Western Great Lakes... Days 1-3... The Great Lakes region (in actuality, much of North America) will be impacted by an increasingly amplified jet stream pattern. NAEFS at 18Z Saturday shows a 97.5 climatological percentile ridge forming over western Canada which then carves out an impressive 500mb low over the Great Lakes on Sunday. Between 12Z Sunday - 12Z Monday, NAEFS shows 850-500mb heights that are outside the lowest observed heights in thew CFSR climatological record for late April-early May. This highly anomalous upper low over the Great Lakes will remain stalled over the region through Monday evening due to the developing high-latitude blocking pattern taking shape over Greenland and northern Quebec. This prolonged period of abnormally cooler temperatures and moisture revolving around the upper low is a recipe for a multi-day snow event in portions of the western Michigan U.P. and far northern Wisconsin. From a synoptic-to-mesoscale evolution, the heaviest snowfall starts Saturday night and into Sunday when the strongest upper level divergence ensues as the upper mean 700-300mb trough takes on a negative tilt. The GFS shows a zone of excellent 700-300mb layer averaged Q-vector convergence directly over the western U.P. of Michigan and northern WI that persists for the better part of 24-30 hours. As the 700mb low forms north of Green Bay Saturday night, the warm conveyor belt at 850-700mb will also introduce a ribbon of moisture flux overhead that persists into Sunday. By Sunday night, a pivoting shortwave trough on the northwest flank of the upper low will provide another source of positive vorticity advection into the Michigan U.P. and northern Wisconsin, further prolonging the heavy snow potential. The key in accumulations will come down to thermals, vertical velocities in the DGZ, and timing of heaviest snowfall rates. SLRs will be lower than climatology for the most part, making for a heavy/wet snow. Taking GFS cross-sections of the western Great Lakes Sunday morning and afternoon, the strongest VVs were focused at the low levels where there is added topographical/lake enhancement, but there was strong 700-500mb frontogenesis as well, showing the strong Q-vector convergence aloft is likely to be a key contributor to heavier snowfall rates than just mesoscale lake effect/low level convergence mesoscale effects. The latest experimental PWSSI does show 40-50% probabilities of Moderate Impacts along the MI/WI border near Ironwood. The footprint of Minor Impacts ranging between 40-60% ranges from northern WI to southeast of the Michigan U.P.'s Porcupine Mountains. Confidence is increasing these areas picking up >12" of snowfall over the course of the next 2-3 days. WPC probabilities for 72-hour snowfall totals >12" were an impressive 70% near and east of Ironwood. It is worth noting that probabilities for >18" were up to 50% between this evening and Monday evening. Localized impacts will be largely driven by the combination of Snow Amount and Snow Load, which given the time of year and heavy/wet type of snow expected, could lead to localized Major impacts where snowfall totals surpass 12". The probability of significant icing greater than 0.25" is less than 10 percent. Mullinax