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Lagrangian eddy kinetic energy of ocean mesoscale eddies and its application to the Northwestern Pacific
Ding, Mengrong1,2,3; Lin, Pengfei1,3; Liu, Hailong1,3; Hu, Aixue2; Liu, Chuanyu4,5,6
2020-07-30
发表期刊SCIENTIFIC REPORTS
ISSN2045-2322
卷号10期号:1页码:11
通讯作者Lin, Pengfei([email protected]) ; Liu, Hailong([email protected])
摘要Coherent oceanic mesoscale eddies with unique dynamical structures have great impacts on ocean transports and global climate. Eddy kinetic energy (EKE), derived from time-dependent circulation, is commonly used to study mesoscale eddies. However, there are three deficiencies of EKE when focusing on the analysis of coherent mesoscale eddies. Here, we propose a comprehensive concept-Lagrangian EKE (LEKE) as an additional metric which is a combination of gridded EKE calculated in Eulerian framework and tracked coherent mesoscale eddies in Lagrangian framework. Evidences suggest that LEKE can make up these deficiencies as an effective supplement. In this study, regional application over Northwestern Pacific Ocean is taken as an example. It clearly demonstrates that LEKE reveals more accurate and detailed characteristics of both cyclonic and anticyclonic eddies than EKE when coherent mesoscale eddies are the specific focus, such as the variation rates of kinetic energy during the eddy propagation, spatial-temporal differences of kinetic energy between cyclonic and anticyclonic eddies. Overall, using LEKE to analyze coherent mesoscale eddies gives the rise to understand the spatial-temporal contrasts between eddies with different polarities, and provides a new perspective to recognize the crucial role played by coherent mesoscale eddies in the ocean.
DOI10.1038/s41598-020-69503-z
收录类别SCI
语种英语
资助项目Strategic Priority Research Program of Chinese Academy of Sciences[XDB42010404]; National Natural Science Foundation of China[41976026]; National Natural Science Foundation of China[41776030]; National Natural Science Foundation of China[41931183]; National Natural Science Foundation of China[41931182]; National Natural Science Foundation of China[41576026]; National Key R&D Program for Developing Basic Sciences[2016YFC1401401]; National Key R&D Program for Developing Basic Sciences[2016YFC1401601]; Regional and Global Model Analysis (RGMA) component of the Earth and Environmental System Modeling Program of the U.S. Department of Energy's Office of Biological & Environmental Research (BER) via National Science Foundation[IA 1844590]; National Science Foundation of the US; NSFC[41976012]; NSFC[Y72143101B]; Talents program of Chinese Academy of Sciences[Y82122101L]; Aoshan Talents Program by the QNML[2017ASTCPES03]; University of Chinese Academy of Sciences (UCAS)
WOS研究方向Science & Technology - Other Topics
WOS类目Multidisciplinary Sciences
WOS记录号WOS:000559797100009
出版者NATURE PUBLISHING GROUP
引用统计
被引频次:8[WOS]   [WOS记录]     [WOS相关记录]
文献类型期刊论文
条目标识符http://ir.qdio.ac.cn/handle/337002/168175
专题海洋环流与波动重点实验室
通讯作者Lin, Pengfei; Liu, Hailong
作者单位1.Chinese Acad Sci, Inst Atmospher Phys, State Key Lab Numer Modeling Atmospher Sci & Geop, Beijing, Peoples R China
2.Natl Ctr Atmospher Res, Climate & Global Dynam Lab, POB 3000, Boulder, CO 80307 USA
3.Univ Chinese Acad Sci, Coll Earth & Planetary Sci, Beijing, Peoples R China
4.Chinese Acad Sci, Inst Oceanol, Key Lab Ocean Circulat & Waves, Qingdao, Peoples R China
5.Qingdao Pilot Natl Lab Marine Sci & Technol, Lab Ocean Dynam & Climate, Qingdao, Peoples R China
6.Chinese Acad Sci, Ctr Ocean Mega Sci, Qingdao, Peoples R China
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GB/T 7714
Ding, Mengrong,Lin, Pengfei,Liu, Hailong,et al. Lagrangian eddy kinetic energy of ocean mesoscale eddies and its application to the Northwestern Pacific[J]. SCIENTIFIC REPORTS,2020,10(1):11.
APA Ding, Mengrong,Lin, Pengfei,Liu, Hailong,Hu, Aixue,&Liu, Chuanyu.(2020).Lagrangian eddy kinetic energy of ocean mesoscale eddies and its application to the Northwestern Pacific.SCIENTIFIC REPORTS,10(1),11.
MLA Ding, Mengrong,et al."Lagrangian eddy kinetic energy of ocean mesoscale eddies and its application to the Northwestern Pacific".SCIENTIFIC REPORTS 10.1(2020):11.
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