| Wang Qi,Liu Qinyu,Hu Ruijin,Xie Qiang.A possible role of the South China Sea in ENSO cycle[J].Acta Oceanologica Sinica,2002,(2):217-226 |
| A possible role of the South China Sea in ENSO cycle |
| A possible role of the South China Sea in ENSO cycle |
| 投稿时间：2001-10-07 修订日期：2002-01-20 |
| DOI： |
| 中文关键词: The South China Sea possible role ENSO cycle |
| 英文关键词:The South China Sea possible role ENSO cycle |
| 基金项目:Wang Qi is the advanced visiting scholar of the Chinese Academy of Sciences supported by Grant No. KZCX2-205.;This work was also supported by the National Key Program for Developing Basic Science Research on the Formation Mechanism and Prediction Theory of Severe Climate Disasters in China under contract No.G1998040900 and the National Natural Science Foundation of China under contract No.40106002. |
| 作者 | 单位 | | Wang Qi | Physical Oceanography Laboratory, Ocean University of Qingdao, Qingdao 266003, China | | Liu Qinyu | Physical Oceanography Laboratory, Ocean University of Qingdao, Qingdao 266003, China | | Hu Ruijin | Physical Oceanography Laboratory, Ocean University of Qingdao, Qingdao 266003, China | | Xie Qiang | South China Sea Institute of Oceanology, Chinese Academy of Sciences, Guangzhou 510301, China |
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| 中文摘要: |
| A data-based hypothesis on the role of the South China Sea (SCS) in ENSO cycle is proposed:during El Niño,there are westerly wind anomaly over the western equatorial Pacific and positive SST anomaly in the eastern equatorial Pacific.Meanwhile anomalous convection moves to the central Pacific with anomalous sinking over Indonesian Archipelago.The latter can cause southerly wind anomaly over the north of South China Sea (NSCS) and makes the NSCS warmer.The warm NSCS can attract the anomalous convection to it in some degree.This attraction is in favor for producing easterly wind anomaly over the western equatorial Pacific,so it helps to form a cycle. |
| 英文摘要: |
| A data-based hypothesis on the role of the South China Sea (SCS) in ENSO cycle is proposed:during El Niño,there are westerly wind anomaly over the western equatorial Pacific and positive SST anomaly in the eastern equatorial Pacific.Meanwhile anomalous convection moves to the central Pacific with anomalous sinking over Indonesian Archipelago.The latter can cause southerly wind anomaly over the north of South China Sea (NSCS) and makes the NSCS warmer.The warm NSCS can attract the anomalous convection to it in some degree.This attraction is in favor for producing easterly wind anomaly over the western equatorial Pacific,so it helps to form a cycle. |
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