| Ding Liangmo. 1991. The influence of the surface heat fluxes of the Kuroshio key-area on meiyu rainfall in the Changjiang River region. Acta Oceanologica Sinica, (1):73－82 |
| The influence of the surface heat fluxes of the Kuroshio key-area on meiyu rainfall in the Changjiang River region |
| The influence of the surface heat fluxes of the Kuroshio key-area on meiyu rainfall in the Changjiang River region |
| Received:April 15, 1990 Revised:June 28, 1990 |
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| Abstract: |
| On the basis,of the surface heat fluxes of the Kuroshio key-area (26°-30°N,125°-30°E)in March andApril,the climatologicai influence of the Kuroshio heat fluxes on meiyu rainfall in the Changjiang River (Yangtse River) region are studied.The results are concluded as follows;the surface heat fluxes of the Kuroshio key-area have certain influence on meiyu rainfall in the Changjiang River region during June and July.The correctness rates for the five stations in the Changjing River region (i.e.Wuhan,Jiujiang,Anqing,Nanjing and Shanghai)are in the range of 9/20-13/20.The surface heat fluxes influence mainly on the homogeneous rainfall pattern,the correctness rates come to 7/10-8/10 for the lower valley of the Changjiang River.The estimation expression of the meiyu rainfall for Shanghai consisting of the surface heat flux and the sea surface temperature anomaly of the Kuroshio key area agrees well with the actual meiyu rainfall condition. |
| 中文摘要: |
| On the basis,of the surface heat fluxes of the Kuroshio key-area (26°-30°N,125°-30°E)in March andApril,the climatologicai influence of the Kuroshio heat fluxes on meiyu rainfall in the Changjiang River (Yangtse River) region are studied.The results are concluded as follows;the surface heat fluxes of the Kuroshio key-area have certain influence on meiyu rainfall in the Changjiang River region during June and July.The correctness rates for the five stations in the Changjing River region (i.e.Wuhan,Jiujiang,Anqing,Nanjing and Shanghai)are in the range of 9/20-13/20.The surface heat fluxes influence mainly on the homogeneous rainfall pattern,the correctness rates come to 7/10-8/10 for the lower valley of the Changjiang River.The estimation expression of the meiyu rainfall for Shanghai consisting of the surface heat flux and the sea surface temperature anomaly of the Kuroshio key area agrees well with the actual meiyu rainfall condition. |
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