Mean properties of mesoscale eddies in the Kuroshio recirculation region

被引:0
作者
Libin Ma
Qiang Wang
机构
[1] Institute of Oceanology,Key Laboratory of Ocean Circulation and Waves
[2] Chinese Academy of Sciences,undefined
[3] University of Chinese Academy of Sciences,undefined
来源
Chinese Journal of Oceanology and Limnology | 2014年 / 32卷
关键词
mesoscale eddies; spatial distributions; temporal variations; potential factors;
D O I
暂无
中图分类号
学科分类号
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 ≥20 weeks) were examined. Comparison between short-span eddies (lifetime ≥4 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:21
相关论文
共 99 条
[1]  
Aoki S(1996)Eddy activities of the surface layer in the Western North Pacific detected by satellite altimeter and radiometer J. Oceanogr. 52 457-474
[2]  
Imawaki S(2008)The ECMWF ocean analysis system: ORA-S3 Mon. Weather Rev. 136 3 018-3 034
[3]  
Balmaseda M A(2009)Eddy activity in the four major upwelling systems from satellite altimetry (1992–2007) Prog. Oceanogr. 83 117-123
[4]  
Vidard A(2008)Mesoscale eddies off Peru in altimeter records: identification algorithms and eddy spatiotemporal patterns Prog. Oceanogr. 79 106-119
[5]  
Anderson D L T(1998)Geographic variability of the first-baroclinic Rossby radius of deformation J. Phys. Oceanogr. 28 433-460
[6]  
Chaigneau A(2007)Global observations of large oceanic eddies, Res. Lett. 34 L15606-216
[7]  
Eldin G(2011)Global observations of nonlinear mesoscale eddies Prog. Oceanogr. 91 167-879
[8]  
Dewitte B(2011)Mesoscale eddies in the South China Sea: Mean properties, spatiotemporal variability, and impact on thermohaline structure J. Geophys. Res. 116 C06018-511
[9]  
Chaigneau A(2005)The interaction of a baroclinic mean flow with long Rossby waves J. Phys. Oceanogr. 35 865-265
[10]  
Gizolme A(1999)The modification of long planetary waves by homogeneous potential vorticity layers J. Phys. Oceanogr. 29 500-19 498