中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
Energetics of Eddy-Mean Flow Interactions along the Western Boundary Currents in the North Pacific

文献类型:期刊论文

作者Yan, Xiaomei1,2,3,4; Kang, Dujuan4; Curchitser, Enrique N.4; Pang, Chongguang1,2,3
刊名JOURNAL OF PHYSICAL OCEANOGRAPHY
出版日期2019-03-01
卷号49期号:3页码:789-810
关键词Boundary currents Eddies Mesoscale processes Ocean circulation Ocean dynamics
ISSN号0022-3670
DOI10.1175/JPO-D-18-0201.1
通讯作者Yan, Xiaomei(yanxiaomei@qdio.ac.cn)
英文摘要The energetics of eddy-mean flow interactions along two western boundary currents of the North Pacific, the Kuroshio and Ryukyu Currents, are systematically investigated using 22 years of numerical data from the Ocean General Circulation Model for the Earth Simulator (OFES). For the time-mean and time-varying flow fields, all the energy components and conversions exhibit inhomogeneous spatial distributions. In the two currents, complex cross-stream and along-stream variations are seen in the eddy-mean flow energy conversions. East of Taiwan, the kinetic energy is mainly transferred from the mean flow to the eddy field through barotropic instability, whereas the baroclinic energy conversions form a meridional dipole structure caused by the topographic constraint. In the northern area, particularly, the eddy field drains 2.25 x 10(8) W of kinetic energy and releases 2.82 x 10(8) W of available potential energy when interacting with the mean flow, indicating that mesoscale eddies impinging on the Kuroshio decay with baroclinic inverse energy cascades. In the Ryukyu Current, inverse energy conversions from the eddy field to the mean flow also dominate the power transfer in the subsurface layer. The eddy field transfers 0.16 x 10(8) W of kinetic energy and 1.89 x 10(8) W of available potential energy to the mean flow, suggesting that meososcale eddies play an important role in maintaining the velocity and hydrographic structure of the current. In other areas, both barotropic and baroclinic instabilities contribute to the generation of eddy kinetic energy with the latter one providing more than 3 times as much power as the former one.
资助项目National Natural Science Foundation of China[41606016] ; National Natural Science Foundation of China[41776021] ; National Natural Science Foundation of China[41576060] ; AoShan Science and Technology Innovation Program[2016AKSJ12] ; National Key R&D Program of China[2016YFC0301203] ; NSFC Shandong Joint Fund for Marine Science Research Centers[U1406401]
WOS研究方向Oceanography
语种英语
WOS记录号WOS:000460532000001
出版者AMER METEOROLOGICAL SOC
源URL[http://ir.qdio.ac.cn/handle/337002/155307]  
专题海洋研究所_海洋环流与波动重点实验室
通讯作者Yan, Xiaomei
作者单位1.Chinese Acad Sci, CAS Key Lab Ocean Circulat & Waves, Inst Oceanol, Qingdao, Peoples R China
2.Pilot Natl Lab Marine Sci & Technol Qingdao, Qingdao, Peoples R China
3.Chinese Acad Sci, Ctr Ocean Mega Sci, Qingdao, Peoples R China
4.Rutgers State Univ, Dept Environm Sci, New Brunswick, NJ 08901 USA
推荐引用方式
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Yan, Xiaomei,Kang, Dujuan,Curchitser, Enrique N.,et al. Energetics of Eddy-Mean Flow Interactions along the Western Boundary Currents in the North Pacific[J]. JOURNAL OF PHYSICAL OCEANOGRAPHY,2019,49(3):789-810.
APA Yan, Xiaomei,Kang, Dujuan,Curchitser, Enrique N.,&Pang, Chongguang.(2019).Energetics of Eddy-Mean Flow Interactions along the Western Boundary Currents in the North Pacific.JOURNAL OF PHYSICAL OCEANOGRAPHY,49(3),789-810.
MLA Yan, Xiaomei,et al."Energetics of Eddy-Mean Flow Interactions along the Western Boundary Currents in the North Pacific".JOURNAL OF PHYSICAL OCEANOGRAPHY 49.3(2019):789-810.

入库方式: OAI收割

来源:海洋研究所

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