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Evolution and propagation of a mesoscale eddy in the northern South China Sea during winter 被引量:4

Evolution and propagation of a mesoscale eddy in the northern South China Sea during winter
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摘要 In situ observations, satellite data, and the output from an eddy-resolving ocean circulation model were used to study the generations and propagations of an anticyclonic eddy in the northern South China Sea (NSCS) during the winter of 2009-2010. In the NSCS, the anticyclonic eddy firstly appeared to the west of the Luzon Strait, migrated generally along the continental slope and dissipated around the Xisha Archipela- go. The evolution of the warm eddy contains three phases: development, maturation, and decay. The eddy mainly stayed near 119.7°E in December and then gradually moved to 118.7°E until January 15, when its intensity, as indicated by the thermocline temperature and salinity anomalies, increased significantly, re- flecting the growth of the eddy. The eddy reached its peak on January 15 and persisted until February 23. During this period, the eddy propagated westward to 116.4°E. After, the warm eddy weakened significantly and dissipated finally near the Xisha Archipelago. In situ observations, satellite data, and the output from an eddy-resolving ocean circulation model were used to study the generations and propagations of an anticyclonic eddy in the northern South China Sea (NSCS) during the winter of 2009-2010. In the NSCS, the anticyclonic eddy firstly appeared to the west of the Luzon Strait, migrated generally along the continental slope and dissipated around the Xisha Archipela- go. The evolution of the warm eddy contains three phases: development, maturation, and decay. The eddy mainly stayed near 119.7°E in December and then gradually moved to 118.7°E until January 15, when its intensity, as indicated by the thermocline temperature and salinity anomalies, increased significantly, re- flecting the growth of the eddy. The eddy reached its peak on January 15 and persisted until February 23. During this period, the eddy propagated westward to 116.4°E. After, the warm eddy weakened significantly and dissipated finally near the Xisha Archipelago.
出处 《Acta Oceanologica Sinica》 SCIE CAS CSCD 2013年第7期1-7,共7页 海洋学报(英文版)
基金 The National Basic Research Program of China under contract No.011 CB403503 the Project "908" of China under contract No. 908-01-BC10 the National Natural Science Foundation of China under contract Nos 41176028 and 41176024 Guangdong Province Natural Science Foundation of China under contract No.S2011010001001 the Knowledge Innovation Program of the Chinese Academy of Sciences of China under contract No.SQ200809
关键词 northern South China Sea anticyclonic eddy PROPAGATION northern South China Sea, anticyclonic eddy, propagation
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