Variability of surface velocity in the Kuroshio Current and adjacent waters derived from Argos drifter buoys and satellite altimeter data
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Variability of surface velocity in the Kuroshio Current and adjacent waters derived from Argos drifter buoys and satellite altimeter data
Variability of surface velocity in the Kuroshio Current and adjacent waters derived from Argos drifter buoys and satellite altimeter data
海洋湖沼学报(英文)2009年27卷第2期 页码:208-217
Affiliations:
Physical Oceanography Laboratory Ocean University of China
Author bio:
Funds:
Supported by the National Basic Research Program of China (973 Program, Nos. 2007CB411804, 2005CB422303), the NSFC (No. 40706006), the Key Project of International Science and Technology Cooperation Program of China (No. 2006DFB21250) and the “111 Project” (B07036), the Program for New Century Excellent Talents in University (NECT-07-0781)
Variability of surface velocity in the Kuroshio Current and adjacent waters derived from Argos drifter buoys and satellite altimeter data[J]. 海洋湖沼学报(英文), 2009,27(2):208-217.
Ma, C., Wu, D. & Lin, X. Variability of surface velocity in the Kuroshio Current and adjacent waters derived from Argos drifter buoys and satellite altimeter data., Chin. J. Ocean. Limnol. 27, 208–217 (2009). https://doi.org/10.1007/s00343-009-9260-6
Variability of surface velocity in the Kuroshio Current and adjacent waters derived from Argos drifter buoys and satellite altimeter data[J]. 海洋湖沼学报(英文), 2009,27(2):208-217. DOI: 10.1007/s00343-009-9260-6.
Ma, C., Wu, D. & Lin, X. Variability of surface velocity in the Kuroshio Current and adjacent waters derived from Argos drifter buoys and satellite altimeter data., Chin. J. Ocean. Limnol. 27, 208–217 (2009). https://doi.org/10.1007/s00343-009-9260-6DOI:
Variability of surface velocity in the Kuroshio Current and adjacent waters derived from Argos drifter buoys and satellite altimeter data
摘要
Abstract
By combining Argos drifter buoys and TOPEX/POSEIDON altimeter data
the time series of sea-surface velocity fields in the Kuroshio Current (KC) and adjacent regions are established. And the variability of the KC from the Luzon Strait to the Tokara Strait is studied based on the velocity fields. The results show that the dominant variability period varies in different segments of the KC: The primary period near the Luzon Strait and to the east of Taiwan Island is the intra-seasonal time scale; the KC on the continental shelf of the ECS is the steadiest segment without obvious periodicity
while the Tokara Strait shows the period of seasonal variability. The diverse periods are caused by the Rossby waves propagating from the interior ocean
with adjustments in topography of island chain and local wind stress.
关键词
Keywords
references
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相关作者
Xudong ZHANG
Xiaofeng LI
Xin YUAN
Qingye WANG
Jie MA
Shijian HU
Dunxin HU
Xiangpeng WANG
相关机构
Key Laboratory of Ocean Observation and Forecasting, Key Laboratory of Ocean Circulation and Waves, Institute of Oceanology, Chinese Academy of Sciences
Center for Ocean Mega-Science, Chinese Academy of Sciences
Laoshan Laboratory
Key Laboratory of Ocean Circulation and Waves, Institute of Oceanology, Chinese Academy of Sciences