鸟笼
发表于 2025-3-27 00:32:44
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
Fecal-Impaction
发表于 2025-3-27 03:22:36
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Canopy
发表于 2025-3-27 06:45:08
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.
离开可分裂
发表于 2025-3-27 12:18:50
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
过于平凡
发表于 2025-3-27 13:56:52
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远地点
发表于 2025-3-27 20:44:10
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magenta
发表于 2025-3-28 00:01:39
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
oxidize
发表于 2025-3-28 04:30:20
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.
松果
发表于 2025-3-28 08:46:15
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.