Mean properties of mesoscale eddies in the Kuroshio recirculation region

被引:9
作者
Ma Libin [1 ,2 ]
Wang Qiang [1 ]
机构
[1] Chinese Acad Sci, Inst Oceanol, Key Lab Ocean Circulat & Waves, Qingdao 266071, Peoples R China
[2] Univ Chinese Acad Sci, Beijing 100049, Peoples R China
基金
中国国家自然科学基金;
关键词
mesoscale eddies; spatial distributions; temporal variations; potential factors; PACIFIC SUBTROPICAL COUNTERCURRENT; NORTH PACIFIC; EDDY; TOPEX/POSEIDON; VARIABILITY; TRANSPORT; SOUTH; HEAT;
D O I
10.1007/s00343-014-3029-2
中图分类号
Q [生物科学];
学科分类号
07 ; 0710 ; 09 ;
摘要
Using a 19-year altimetric dataset, the mean properties and spatiotemporal variations of eddies in the Kuroshio recirculation region are examined. A total of 2 001 cyclonic tracks and 1 847 anticyclonic tracks were identified using a geometry-based eddy detection method. The mean radius was 57 km for cyclonic eddies and was 61 km for anticyclonic eddies, respectively, and the mean lifetime was about 10 weeks for both type eddies. There were asymmetric spatial distributions for eddy generation and eddy termination, which were domain-dependent. Mean eddy generation rates were 2.0 per week for cyclonic eddies and were 1.9 per week for anticyclonic eddies. Both type eddies tended to deform during their lifetime and had different propagation characteristics, which mainly propagated westward and southwestward with velocities 4.0-9.9 cm/s, in the Kuroshio recirculation region. Further discussion illustrates that the eddy westward speed maybe influenced by the combined effect of vertical shear of horizontal currents and nonlinearity of eddy. To better understand the evolution of eddy tracks, a total of 134 long-lived tracks (lifetime a parts per thousand yen20 weeks) were examined. Comparison between short-span eddies (lifetime a parts per thousand yen4 weeks and < 20 weeks) and long-lived eddies is also conducted and the result shows that the short-span and long-lived eddies have similar time evolution. Finally, eddy seasonal variations and interannual changes are discussed. Correlation analysis shows that eddy activity is sensitive to the wind stress curl and meridional gradient of sea surface temperature on interannual timescales. Besides, the strength and orientation of background flows also have impacts on the eddy genesis.
引用
收藏
页码:681 / 702
页数:22
相关论文
共 45 条
[1]  
Aoki S, 1996, J OCEANOGR, V52, P457, DOI DOI 10.1007/BF02239049
[2]  
AVISO, 2008, SSALTO DUCAS US HDB
[3]   The ECMWF ocean analysis system: ORA-S3 [J].
Balmaseda, Magdalena A. ;
Vidard, Arthur ;
Anderson, David L. T. .
MONTHLY WEATHER REVIEW, 2008, 136 (08) :3018-3034
[4]   Eddy activity in the four major upwrelling systems from satellite altimetry (1992-2007) [J].
Chaigneau, Alexis ;
Eldin, Gerard ;
Dewitte, Boris .
PROGRESS IN OCEANOGRAPHY, 2009, 83 (1-4) :117-123
[5]   Mesoscale eddies off Peru in altimeter records: Identification algorithms and eddy spatio-temporal patterns [J].
Chaigneau, Alexis ;
Gizolme, Arnaud ;
Grados, Carmen .
PROGRESS IN OCEANOGRAPHY, 2008, 79 (2-4) :106-119
[6]  
Chelton DB, 1998, J PHYS OCEANOGR, V28, P433, DOI 10.1175/1520-0485(1998)028<0433:GVOTFB>2.0.CO
[7]  
2
[8]   Global observations of large oceanic eddies [J].
Chelton, Dudley B. ;
Schlax, Michael G. ;
Samelson, Roger M. ;
de Szoeke, Roland A. .
GEOPHYSICAL RESEARCH LETTERS, 2007, 34 (15)
[9]   Global observations of nonlinear mesoscale eddies [J].
Chelton, Dudley B. ;
Schlax, Michael G. ;
Samelson, Roger M. .
PROGRESS IN OCEANOGRAPHY, 2011, 91 (02) :167-216
[10]   Mesoscale eddies in the South China Sea: Mean properties, spatiotemporal variability, and impact on thermohaline structure [J].
Chen, Gengxin ;
Hou, Yijun ;
Chu, Xiaoqing .
JOURNAL OF GEOPHYSICAL RESEARCH-OCEANS, 2011, 116