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December 2000 nor'easter

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Through Great Plains

Synoptic history

The storm developed as an Alberta clipper-type low pressure area that moved southeastward across the Great Plains and Midwest. Throughout North Dakota, Minnesota and Iowa, moderate snowfall accompanied the system. After weakening over the Ohio Valley, the storm redeveloped off the coast of North Carolina. In the days preceding the event, a cyclone over eastern Canada circulated cold air southward. Computer models indicated the potential for a major storm up to seven days in advance; however, initially, certain forecasts suggested that a separate storm over the southern U.S. would merge with the clipper. Instead, this feature moved out to sea.

As the secondary storm began to intensify offshore, precipitation rapidly expanded and tracked northward towards southern Virginia, eastern Maryland and Delaware, largely in the form of freezing rain, ice, and snow. From 0200 UTC on December 30 to 1200 UTC, the cyclone intensified by 13 mbar, and continued to deepen for several more hours. Snowfall reached southern New Jersey between 0600 and 0800 UTC, and New York City at around 1000 UTC. Thundersnow developed within heavy bands in some areas. The significant snow was characterized by a sharp western cutoff; for example, in Chester County, accumulations ranged from around 6 inches in the far eastern parts of the county to only an inch along its western border with Lancaster County.

While located off the New Jersey coast, the storm stopped strengthening and slowly moved northward. The center was situated near central Long Island at 2100 UTC. Across eastern Long Island and parts of eastern New England, snow mixed with and, in some cases, changed over to rain. The surface low had moved into eastern Connecticut by early on December 31. As it continued to head northeastward, a new center of low pressure developed near Boston and moved towards coastal Maine. The storm system had abated by January 1.

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