Titlebook: Snowstorms Along the Northeastern Coast of the United States: 1955 to 1985; Paul J. Kocin,Louis W. Uccellini Book 1990 American Meteorolog

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Climatological Overview of the Period from 1955 to 1985, 15 cm in the southeastern corner of Virginia to greater than 250 cm across sections of central and northern New England, New York, and West Virginia. The increase in snowfall at higher latitudes is skewed from southwest to northeast by the Atlantic Ocean’s moderating influence on temperatures near

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Description of Upper-Level Features Associated with the Snowstorms,NMC charts. They are designed to provide an overview of the geopotential height, wind, and temperature fields that are indicative of the upper-level dynamical and thermodynamical processes associated with the storms.

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Summary of the Physical and Dynamical Processes that Influence Northeast Snowstorms,extensive distribution of heavy snowfall (>25 cm) across one of the most heavily populated and industrialized regions of the world, including the metropolitan areas of New York, Washington, Boston, Philadelphia, and Baltimore. Analyses of the surface and upperlevel fields of pressure, geopotential h

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Book 1990y populated coastal region of the Middle Atlantic states and southern New England over the last four decades. Heavy snowfall and high winds associated with storms often referred to as "nor‘easters" can maroon millions of people at home or in transit, severely disrupt human services and commerce, and

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Historical Overview: A Brief Review of Major Snowstorms of the Eighteenth, Nineteenth, and Twentiet300 years of such information provides important historical and climatological insight into the limits of severity these storms are capable of attaining. A sampling of the region’s legendary storms is briefly described below.

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Descriptions of 20 Major Snowstorms,al patterns that characterize major snow events, to determine what case-to-case variability might make generalizations difficult to apply, and to describe the dynamical and physical processes associated with these patterns. A description of upper-level meteorological fields will be presented in the next chapter.