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.
Citation:
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.
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.
Citation:
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.
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
2.
Center for Atmospheric and Oceanic Studies, Faculty of Science, Tohoku University, Sendai 980-8578, Japan
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.
DownLoad: