| 海洋和高原热状况对夏季风活动影响的初步分析 |
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| 引用本文： | 郭其蕴,王继琴.海洋和高原热状况对夏季风活动影响的初步分析[J].海洋学报,1980,2(2):41-54. |
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| 作者姓名： | 郭其蕴 王继琴 |
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| 作者单位： | 1.中国科学院大气物理研究所 |
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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.
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| 收稿时间： | 6/1/1979 12:00:00 AM |
THE INFLUENCES OF SEA SURFACE TEMPERATURE AND THERMAL STATE OF THE TIBETAU PLATEAU ON THE SUMMER MONSOON ACTIVITY |
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| Guo Qiyun and Wang Jiqin.THE INFLUENCES OF SEA SURFACE TEMPERATURE AND THERMAL STATE OF THE TIBETAU PLATEAU ON THE SUMMER MONSOON ACTIVITY[J].Acta Oceanologica Sinica (in Chinese),1980,2(2):41-54. |
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| Authors: | Guo Qiyun and Wang Jiqin |
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| Institution: | 1.Institute of Atmospheric Physics, Academia Sinica2.Institute of Geography, Academia Sinica |
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| 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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