Dissipative heating and hurricane intensity

被引：1
|
作者：
M. Bister
K. A. Emanuel
机构：
[1] Massachusetts Institute of Technology,Program in Atmospheres, Oceans, and Climate
来源：
Meteorology and Atmospheric Physics | 1998年 / 65卷
关键词：
Climate Change; Waste Water; Boundary Layer; Wind Speed; Water Management;
D O I：
暂无
中图分类号：
学科分类号：
摘要：
Dissipative heating has not been accounted for in either numerical simulations of hurricanes or in theories for the maximum intensity of hurricanes. We argue that the bulk of dissipative heating occurs in the atmospheric boundary layer near the radius of maximum winds and, using both theory and numerical simulation, show that dissipative heating increases maximum wind speeds in tropical cyclones by about 20%.
引用
收藏
页码：233 / 240
页数：7
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