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南海海温变异与长江中下游六月降水的联系 被引量:3

RELATIONSHIP BETWEEN THE VARIATION OF THE SEASURFACE TEMPERATURE OVER THE SOUTH CHINA SEA AND THE RAINFALLS OVER THE MIDDLE AND LOWER REACHES OF THE YANGTZE RIVER IN JUNE
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摘要 本文利用1951—1984年长江中下游6月降水资料以及195t年——1977年南海海面温度资料,分析了长江中下游6月降水与副热带系统以及西风带活动的关系,並采用典型相关分析法,研究了南海海温与南海高压以及长江中下游地区6月降水的联系,取得了较好的结果。 In this paper, the data of the rainfalls over the middle and lower reaches of the Yangtze River in June during 1951-1984 and of the sea-surface temperatureCSST)over the South China sea during 1951-1977 are used to analyse the relationship betweeh the rainfall in June over the middle and lower neaches of the Yangtze River and subtropic systems and the activity of the westerly belt., The canonical correlation analysis method is also applied to investigate the relationship between the SST of the South China Sea, the South China sea High and the rainfall in June over the middle and lower reaches of the Yangtze River and the better restlts are obtaineda
出处 《气象科学》 CSCD 北大核心 1990年第2期174-181,共8页 Journal of the Meteorological Sciences
基金 国家攻关项目760704的资助
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参考文献2

  • 1罗绍华,金祖辉,陈烈庭.印度洋和南海海温与长江中下游夏季降水的相关分析[J]大气科学,1985(03).
  • 2陈其恭,陆菊中,徐桂玉,毛秀凤.用500毫巴环流特征予报长江中下游六月份的旱涝[J]南京大学学报(自然科学版),1978(03).

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