On the vertical structure of damped steady circulation in the tropics
On the vertical structure of damped steady circulation in the tropics
复制标题
热带地区阻尼稳定环流的垂直结构
DOI：
--
复制
发表时间：
1982
期刊：
影响因子：
--
通讯作者：
D. Stevens
中科院分区：
文献类型：
--
作者：
J. Geisler;D. Stevens
本文分析了在定常孤立非绝热加热强迫下耗散热带大气定常运动的垂直结构。得到了适合于该问题的垂直模态，并将强迫投影到这些模态上。利用Gill（1980）给出的水平结构的解析表达式，对这些模态求和，得到加热区以东区域响应的振幅和垂直结构。
This paper presents an analysis of the vertical structure of steady motion in a dissipative tropical atmosphere forced by steady isolated diabatic heating. Vertical modes appropriate to the problem are obtained, and the forcing is projected onto these modes. With the use of an analytic expression obtained by Gill (1980) for the horizontal structure, these modes are summed to obtain the amplitude and the vertical structure of the response in the region to the east of the heating.