Mesoscale aspects of the Urban Heat Island around New York City

被引：1

作者：

S. D. Gedzelman

S. Austin

R. Cermak

N. Stefano

S. Partridge

S. Quesenberry

D. A. Robinson

机构：

[1] Department of Earth and Atmospheric Sciences,

[2] City College of New York,undefined

[3] New York,undefined

[4] NY,undefined

[5] USA,undefined

[6] Computer Sciences Department,undefined

[7] Physical,undefined

[8] Environmental,undefined

[9] and Computer Sciences Department,undefined

[10] Medgar Evers College,undefined

[11] Brooklyn,undefined

[12] NY,undefined

[13] USA,undefined

[14] Weather Access Inc.,undefined

[15] Highland Park,undefined

[16] NJ,undefined

[17] USA,undefined

[18] Sussex County Weather Network,undefined

[19] Wantage,undefined

[20] NJ,undefined

[21] USA,undefined

[22] Weather Access Inc.,undefined

[23] Chatham,undefined

[24] NJ,undefined

[25] USA,undefined

[26] South Jersey Resource Conservation and Development Council,undefined

[27] Hammontown,undefined

[28] NJ,undefined

[29] USA,undefined

[30] Department of Geography,undefined

[31] Rutgers University,undefined

[32] New Brunswick,undefined

[33] NJ,undefined

[34] USA,undefined

来源：

Theoretical and Applied Climatology | 2003年 / 75卷

关键词：

Wind Speed; Weather Station; York City; Cloud Cover; Early Summer;

D O I：

暂无

中图分类号：

学科分类号：

摘要：

¶A mesoscale analysis of the Urban Heat Island (UHI) of New York City (NYC) is performed using a mesoscale network of weather stations. In all seasons the UHI switches on rapidly in late afternoon and shuts down even more rapidly shortly after dawn. It averages about 4 °C in summer and autumn and 3 °C in winter and spring. It is largest on nights with clear skies, low relative humidity through much of the troposphere, and weak northwest winds, when it may exceed 8 °C. The synoptic meteorological situation associated with the largest UHI occurs roughly two to three nights after cold front passages.

引用

页码：29 / 42

页数：13

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