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1999年夏季中国降水南多北少成因初探
Preliminary Studies on the Cause of Southern Flood and Northern Drought during the Summer of 1999 in China
【摘要】 对1999年中国夏季降水特征及其成因的分析表明,1999年夏季中国长江中下游地区降水偏多有其重要的气候背景,主要受到降水年代际振荡湿期的影响,而 La Nina事件的冬季增强是造成 1999年中国夏季雨带位置偏南,北方少雨干旱的重要物理因素。
【Abstract】 The distribution of precipitation and its cause during the summer of 1999 have been inves- tigated. The results show that it is the decadal-to-interdecadal oscillations of precipitation in the mid- dle and low reaches of the Yangtze River, which is in the wet phase from the recent decadal, that is considered as the most important climate background of the relative richer rainfall during the summer of 1999. Furthermore, the intensifying of La Nina event in the former winter is accounted for the south- ward excursion of main rain belt and drought in the north of China.
【关键词】 La Nia;
年代际振荡;
季风;
旱涝;
模型;
【Key words】 La Nia, decadal-to-interdecadal oscillation; monsoon, flood and drought, model.;
【Key words】 La Nia, decadal-to-interdecadal oscillation; monsoon, flood and drought, model.;
【基金】 国家“九五”重中之重科技攻关项目“我国短期气候预测系统的研究”96-908-04-01专题资助
- 【文献出处】 气候与环境研究 ,Climatic and Environmental Research , 编辑部邮箱 ,2001年03期
- 【分类号】P461.3
- 【被引频次】17
- 【下载频次】125