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Winter of 1950-1951 in the Southeast


The Winter of 1950-1951 in the Southeast (December 1950–February 1951) was notably cold and disruptive in parts of the region, influenced by the lingering effects of the Great Appalachian Storm of November 1950 (late November, spilling into early winter context) and a major **ice storm/snow event in late January–early February 1951 (the "Great Ice Storm" or "Blizzard of 1951"). The season featured extreme cold waves (with record November lows extending into winter), heavy ice/sleet accumulations across the Mid-South and parts of the Southeast, and light to moderate snow in higher/northern areas. While not as snowfall-dominant as the 1989 Christmas coastal storm, the winter stands out for widespread icing (up to 2+ inches glaze), record cold (e.g., sub-zero in parts of the Deep South), and significant agricultural/infrastructure damage from the January–February ice storm, which affected areas from Louisiana to Kentucky/Ohio but spilled into northern Alabama, Georgia, and Tennessee. The Southeast saw below-normal temperatures overall (DJF anomaly negative in north Georgia records), with the January 1951 ice storm as the season's most impactful event.




Meteorological Setup

The winter followed the Great Appalachian Storm (November 22-30, 1950), a massive extratropical cyclone that brought blizzard conditions to the Appalachians, heavy rain/flooding east, and record cold southward. An Arctic front plunged deep into the Southeast, setting November lows that persisted into December (e.g., Atlanta 3°F, Birmingham 5°F, Pensacola 22°F—all November records). No major early-winter snow followed, but cold lingered.

The key winter event was the January 29–February 2, 1951 ice storm (the "Great Ice Storm of 1951" or "Blizzard of 1951"): A strong cold front interacted with Gulf moisture and a low tracking northeast from the Gulf/Southern Plains. Overrunning produced freezing rain/sleet/snow over a 100+ mile-wide band from Louisiana to Ohio/Kentucky, with heaviest icing in the Mid-South (Tennessee/Kentucky) but spillover into northern Alabama/Georgia. A strong high-pressure system pulled in polar air, creating ideal glaze conditions (warm air aloft over sub-freezing surface). No rapid coastal intensification; the storm was overrunning/ice-dominant. February moderated after the event.



Impacts


Precipitation and Distribution

Temperature Records

Impacts




Notes of Interest

This winter brought punishing cold and destructive ice to parts of the Southeast.