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Back-to-Back Pacific Storms to Impact the West Coast; Heavy Snow in the Central Appalachians

Back-to-back powerful Pacific storm systems to impact the Pacific Northwest and northern California through the end of this week with heavy rain, flooding, strong winds, and higher elevation mountain snow. A strong, long-duration atmospheric river will accompany the Pacific storms, bringing excessive rainfall and flash flooding to southwest Oregon and northwest California through the week. Read More >

Overview

One of the most significant late-season snowstorms in Upper Michigan history occurred May 9-10, 1990. Very warm temperatures on May 8 with highs in the 70s and even in the mid 80s in some spots gave way to rain on May 9 as an area of low pressure moved through Wisconsin. By the afternoon of the 9th, rain began changing over to slushy snow. Despite it being May, and despite the very warm temperatures a day before, snow began sticking by the evening and then rapidly accumulated overnight into the morning of May 10.

The higher elevations of the central Upper Peninsula and northern Wisconsin were hit the hardest, with the NWS office in Negaunee measuring an amazing 22.4 inches of snow from this storm! Road crews said this snow took twice as long as normal to clear because it was so wet and heavy, according to reports in the Marquette Mining Journal.

The snow didn't stick around long, however. By the next day, high temperatures were back in the 50s and 60s. Only a Trace of snow depth was reported at the NWS office in Negaunee on May 14, and by May 15 the snow was completely gone.

At the NWS office, the 14.2 inches of snow that fell after midnight on May 10 still holds the record for most snowfall on any singe day in the month of May since records began being kept in 1961. However there have been even later snowfalls in May - just none as heavy as this one. The latest snowfall of 1 inch or greater was on May 16, 1997.

Photo

Surface map showing the area of low pressure moving out of Wisconsin and over Lake Michigan

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