孙照渤,章基嘉,T.N.Palmer. 1990. 南海表面温度距平对我国夏季风和降水影响的数值试验[J]. 气象学报, 48(1):113-116, doi:10.11676/qxxb1990.014
南海表面温度距平对我国夏季风和降水影响的数值试验
A NUMERICAL EXPERIMENT OF SST OVER SOUTH CHINA SEA ON THE SUMMER MONSOON AND PRECIPITATION IN CHINA
投稿时间:1988-01-23  修订日期:1988-11-10
DOI:10.11676/qxxb1990.014
中文关键词:  
英文关键词:
基金项目:
作者单位
孙照渤 南京气象学院 
章基嘉 国家气象局 
T.N.Palmer 英国气象局 
摘要点击次数: 1917
全文下载次数: 2007
中文摘要:
      我国东部夏季降水不仅与副高脊线的向北推进有关,而且与对流层低层夏季季风向北推进有关[1]。Shukla[2],在研究印度季风降水量对阿拉伯海域海表温度响应时也指出,对季风环流模拟的真实性直接影响印度季风降水模拟的真实性。
英文摘要:
      Based on the observational analysis, a numerical experiment of the SST over South China Sea on the monsoon and precipitation in China is presented by using the 11-layer GCM of U. K. Met.Office. It is shown that the warm SST anomalies over South China Sea have attracting to Indian summer monsoon,and cold anomalies have repelling to the Indian monsoon. The relattions of summer monsoon and rainfall in China with the SST anomalies over south Chian Sea area are also discussed.
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