海洋和高原热状况对夏季风活动影响的初步分析
THE INFLUENCES OF SEA SURFACE TEMPERATURE AND THERMAL STATE OF THE TIBETAU PLATEAU ON THE SUMMER MONSOON ACTIVITY
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摘要: 我国是世界上著名的季风气候区.但过去相当多的研究是从气候概念来理解季风的.实际上,各年季风的起迄日期有早有晚,而强度也不同.正是由于这种差异,造成了我国各地的旱涝灾害.因此从个别年来研究季风,并探讨形成季风年际变化可能的原因是十分必要的.本文尝试通过1971年与1972年季风活动的对比分析,一方面了解环流特征季节变化的异同,另一方面希望能对这两年旱涝产生的原因有一个更明确的认识.Abstract: The summer monsoon activity is responsible for rainfall formation over china,especially in the eastern part.The anomalies of monsoon activity,change of intensity,early or later onset usually bring about drought or flood in one or another part of our country.Consequently,a detailed analysis of the monsoon actvity for individual year is worthwhile.This sort of study may be helpful for research of the formation causes and the improvement of the long range weather forecasting.
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高由禧、徐淑英,东亚季风进退与雨季的起迄,东亚季风的若干问题,科学出版社,1962 郭其蕴、司有元,我国汛期降水分布类型及其季节变化,地理集刊,13(1979). Asakura,T.,(朝正),Dynamic climatolvgy of atmospheric cirwlation over east Asia center in Japan,papers in meteorology and Geophysics.1968,1. Koteswaram,P.,The Asian summer monsoon and the general circulation over the tropies,Monsoon of the world,India M,D.,1960. Ramage,C.S.,Monsoon meteorology,Academic press,New York and London,1971. Rao.Y.P.,SW-Monsoon,New Delhi,1976. -
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