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地形在东亚夏季风环流中的作用
引用本文:孙冬联,朱抱真.地形在东亚夏季风环流中的作用[J].热带气象学报,1991,0(3):268-274.
作者姓名:孙冬联  朱抱真
作者单位:1.国家气象局卫星气象中心
摘    要:本文应用大气所二室改建的二层球谱模式,引入OSU二层格点模式的物理过程,模拟了5月份东南亚和我国南海的夏季风环流。通过有无地形作用的对比试验,揭示出地形对东亚夏季风环流的建立以及季风区降水和大气热源的形成起了重要作用。 

收稿时间:1989/10/10 0:00:00
修稿时间:2/5/1991 12:00:00 AM

THE ROLE OF MOUNTAINOUS TOPOGRAPH IN SUMMER MONSOON OF EAST ASIA
Sun Donglian and Zhu Baozhen.THE ROLE OF MOUNTAINOUS TOPOGRAPH IN SUMMER MONSOON OF EAST ASIA[J].Journal of Tropical Meteorology,1991,0(3):268-274.
Authors:Sun Donglian and Zhu Baozhen
Institution:1.Satellite Metevorlogical Center, SMA2.Institute of Atmmospheric Physics, Academia Sinicica
Abstract:With introduced physical processes from OSU's 2-level grid model, an 2-level spherical spectral model developed by the institute is used to simulate the summer monsoon circulation in the Southeast Asia and the South China Sea in May. Experiments of comparison between the presence and absence of mountainous topographic effects suggest that the topograph plays an important role in the establishment of the summer monsoon circulation in East Asia and the formation of precipitation and atmospheric heat sources in the monsoon region.
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