| HU Jianyu,KAWAMURA Hiroshi.Detection of cyclonic eddy generated by looping tropical cyclone in the northern South China Sea: a case study[J].Acta Oceanologica Sinica,2004,(2):213-224 |
| Detection of cyclonic eddy generated by looping tropical cyclone in the northern South China Sea: a case study |
| Detection of cyclonic eddy generated by looping tropical cyclone in the northern South China Sea: a case study |
| 投稿时间：2003-10-11 修订日期：2004-03-20 |
| DOI： |
| 中文关键词: cyclonic eddy looping tropical cyclone northern South China Sea TOPEX/POSEIDON altimeter data |
| 英文关键词:cyclonic eddy looping tropical cyclone northern South China Sea TOPEX/POSEIDON altimeter data |
| 基金项目: |
| 作者 | 单位 | E-mail | | HU Jianyu | Key Laboratory of Marine Environmental Science of Ministry of Education
Institute of Subtropical Oceanography, Xiamen University, Xiamen 361005, China
Center for Atmospheric and Oceanic Studies, Faculty of Science, Tohoku University, Sendai 980-8578, Japan | hujy@xmu.edu.cn | | KAWAMURA Hiroshi | Center for Atmospheric and Oceanic Studies, Faculty of Science, Tohoku University, Sendai 980-8578, Japan | |
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| 中文摘要: |
| A case study on the cyclonic eddy generated by the tropical cyclone looping over the northern South China Sea (NSCS) is presented, using TOPEX/POSEIDON altimeter data and AVHRR sea surface temperature (SST) data. Three cases relating to the tropical cyclone events (Typhoon Kai-Tak in July 2000, Tropical Storm Russ in June 1994 and Tropical Storm Maria in August-September 2000) over the NSCS have been analyzed. For each looping tropical cyclone case, the cyclonic eddy with an obvious sea level depression appears in the sea area where the tropical cyclone takes a loop form, and lasts for about 2 weeks with a slight variation in location. The cold core with the SST difference greater than 2℃against its surrounding areas is also observed by the satellite-derived SST data. |
| 英文摘要: |
| A case study on the cyclonic eddy generated by the tropical cyclone looping over the northern South China Sea (NSCS) is presented, using TOPEX/POSEIDON altimeter data and AVHRR sea surface temperature (SST) data. Three cases relating to the tropical cyclone events (Typhoon Kai-Tak in July 2000, Tropical Storm Russ in June 1994 and Tropical Storm Maria in August-September 2000) over the NSCS have been analyzed. For each looping tropical cyclone case, the cyclonic eddy with an obvious sea level depression appears in the sea area where the tropical cyclone takes a loop form, and lasts for about 2 weeks with a slight variation in location. The cold core with the SST difference greater than 2℃against its surrounding areas is also observed by the satellite-derived SST data. |
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