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February 1952 nor'easter

Winter storm in New England, US

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Through Jet stream and Massachusetts

Development

The development of this extratropical cyclone was associated with a pronounced weakening of the usual zonal, or west-to-east, flow which dominates the Mid-Latitudes during the winter, with the jet stream dipping from the latitude of Boston to the latitude of Charleston, South Carolina. The initial low-pressure area originated in the Gulf of Mexico, with a downstream redevelopment offshore Cape Hatteras on February 16. The cyclone deepened rapidly, 25 millibars in 24 hours between February 17 and February 18, while moving just offshore Long Island and southern New England, and dropped heavy precipitation across the central and northern Mid-Atlantic states. The snowfall associated with the storm across eastern New York and southern New England produced the heaviest snows of the winter.

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