中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
A three-dimensional modeling study on eddy-mean flow interaction between a Gaussian-type anticyclonic eddy and Kuroshio

文献类型:期刊论文

作者Xie, Qiang(Chinese Acad Sci, Inst Deep Sea Sci & Engn, Sanya 572000, Peoples R China); Xie, Qiang2,3; Chen, Gengxin4; Liu, Qinyan4; Wang, Dongxiao(Chinese Acad Sci, South China Sea Inst Oceanol, State Key Lab Trop Oceanog, 164 West Xingang Rd, Guangzhou 510301, Guangdong, Peoples R China); Wang, Dongxiao4; Geng, Wu1,4
刊名JOURNAL OF OCEANOGRAPHY
出版日期2018-02-01
卷号74期号:1页码:23-37
关键词Energy Analysis Kuroshio Luzon Strait Eddy Eddy Kinetic Energy Eddy-mean Flow Interaction
DOI10.1007/s10872-017-0435-z
产权排序第1完成单位 ; 第2完成单位 ; 第3完成单位 ; 第4完成单位
文献子类Article
英文摘要The Princeton ocean model is employed to study the energy balance of a fast-moving anticyclonic eddy (AE) during eddy-mean flow interaction. The AE is initialized with an axisymmetric Gaussian-type temperature profile and is placed to the east of the Philippine Islands. An energy analysis suggests that the advection term, pressure work and friction term play dominant roles in the initial eddy decay. During the strong interaction stage, barotropic instability (BTI) becomes the main force for the eddy kinetic energy (EKE) production, with the largest positive BTI in the interaction zone, which means that the eddy always obtains kinetic energy from the Kuroshio during this stage. Most of the EKE dissipation, the large conversion from the eddy available potential energy to the EKE and that from the mean kinetic energy to the EKE all occur at the upper layer during the strong interaction stage. When the AE interacts with the mean flow on the eastern side of the Kuroshio, whether the AE gains kinetic energy from the Kuroshio or loses kinetic energy to the Kuroshio is mainly determined by its shape in the interaction zone.
URL标识查看原文
WOS关键词PACIFIC SUBTROPICAL COUNTERCURRENT ; SOUTH CHINA SEA ; NORTH PACIFIC ; LUZON STRAIT ; MESOSCALE EDDIES ; WESTERN BOUNDARY ; INTERANNUAL VARIABILITY ; OCEAN EDDIES ; TAIWAN ; EVOLUTION
语种英语
WOS记录号WOS:000419913900003
源URL[http://ir.idsse.ac.cn/handle/183446/5918]  
专题深海科学研究部_海洋环流观测与数值模拟研究室
通讯作者Xie, Qiang(Chinese Acad Sci, Inst Deep Sea Sci & Engn, Sanya 572000, Peoples R China); Xie, Qiang; Wang, Dongxiao(Chinese Acad Sci, South China Sea Inst Oceanol, State Key Lab Trop Oceanog, 164 West Xingang Rd, Guangzhou 510301, Guangdong, Peoples R China); Wang, Dongxiao
作者单位1.Univ Chinese Acad Sci, Beijing 100049, Peoples R China
2.Chinese Acad Sci, Inst Deep Sea Sci & Engn, Sanya 572000, Peoples R China
3.Qingdao Natl Lab Marine Sci & Technol, Lab Reg Oceanog & Numer Modeling, Qingdao 266071, Peoples R China
4.Chinese Acad Sci, South China Sea Inst Oceanol, State Key Lab Trop Oceanog, 164 West Xingang Rd, Guangzhou 510301, Guangdong, Peoples R China
推荐引用方式
GB/T 7714
Xie, Qiang,Xie, Qiang,Chen, Gengxin,et al. A three-dimensional modeling study on eddy-mean flow interaction between a Gaussian-type anticyclonic eddy and Kuroshio[J]. JOURNAL OF OCEANOGRAPHY,2018,74(1):23-37.
APA Xie, Qiang.,Xie, Qiang.,Chen, Gengxin.,Liu, Qinyan.,Wang, Dongxiao.,...&Geng, Wu.(2018).A three-dimensional modeling study on eddy-mean flow interaction between a Gaussian-type anticyclonic eddy and Kuroshio.JOURNAL OF OCEANOGRAPHY,74(1),23-37.
MLA Xie, Qiang,et al."A three-dimensional modeling study on eddy-mean flow interaction between a Gaussian-type anticyclonic eddy and Kuroshio".JOURNAL OF OCEANOGRAPHY 74.1(2018):23-37.

入库方式: OAI收割

来源:深海科学与工程研究所

浏览0
下载0
收藏0
其他版本

除非特别说明,本系统中所有内容都受版权保护,并保留所有权利。