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Overview

During the midday hours of February 16th, a surface low pressure system began to develop over the Mid-Mississippi Valley region and shift east northeastward into the lower OH Valley region. The main surface low tracked east into the KY/VA border over the mid Appalachian Range by 00Z 2/17. During this time aloft, the upper air maps indicated a well-defined phasing of jet streaks from the Mid- Mississippi Valley into the Middle Atlantic region of the lower CONUS. The upper air winds aloft toped 190 knots in some areas of the jet max. This powerful, but quick hitting system in a progressive pattern showed the upper dynamics translating to the surface with a well-defined 700MB frontogenic band developing as it shifted a bit north. The onset of moderate to at times heavy snowfall began to develop over the central and southern portions of the forecast area. Snow began during the evening of the 16th and persisted through the rest of the evening and began to wind down by 4am across the area in the early morning hours of the 17th. The rates within the band averaged around 2 inches per hour. The band developed along a line from Coshocton, OH to Stillwater, OH, to Deersville, OH, to Wintersville, OH, to Weirton, WV, and finally to Imperial, PA. The band then continued into counties eastward into Westmoreland and the highlands as well. Still, the elevation impacts proved the most important with Davis, WV in Tucker County receiving around a foot. The shift and development of the banded area of this mid-latitude cyclone resulted in a county by county upgrade from the Winter Weather Advisory to a Winter Storm Warning at onset. Certainly a memorable event.

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Watch Warning and Advisory Map

Coshocton, Tuscarawas, Harrison, and Jefferson Counties in Ohio as well as Hancock and Brooke in West Virginia were upgraded to Winter Storm Warnings as the mesoscale band developed.

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