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Geostrophic meridional transport in tropical Northwest Pacific based on Argo profiles
Zhang Zhichun1,2,3; Yuan Dongliang1,2; Chu, Peter C.4; Yuan, DL
2013-05-01
发表期刊CHINESE JOURNAL OF OCEANOLOGY AND LIMNOLOGY
ISSN0254-4059
卷号31期号:3页码:656-664
文章类型Article
摘要Absolute geostrophic currents in the North Pacific Ocean were calculated using P-vector method from newly gridded Argo profiling float data collected during 2004-2009. The meridional volume transport of geostrophic currents differed significantly from the classical Sverdrup balance, with differences of 10x10(6)-20x10(6)m(3)/s in the interior tropical Northwest Pacific Ocean. Analyses showed that errors of wind stress estimation could not explain all of the differences. The largest differences were found in the areas immediately north and south of the bifurcation latitude of the North Equatorial Current west of the dateline, and in the recirculation area of the Kuroshio and its extension, where nonlinear eddy activities were robust. Comparison of the geostrophic meridional transport and the wind-driven Sverdrup meridional transport in a high-resolution OFES simulation showed that nonlinear effects of the ocean circulation were the most likely reason for the differences. It is therefore suggested that the linear, steady wind-driven dynamics of the Sverdrup theory cannot completely explain the meridional transport of the interior circulation of the tropical Northwest Pacific Ocean.; Absolute geostrophic currents in the North Pacific Ocean were calculated using P-vector method from newly gridded Argo profiling float data collected during 2004-2009. The meridional volume transport of geostrophic currents differed significantly from the classical Sverdrup balance, with differences of 10x10(6)-20x10(6)m(3)/s in the interior tropical Northwest Pacific Ocean. Analyses showed that errors of wind stress estimation could not explain all of the differences. The largest differences were found in the areas immediately north and south of the bifurcation latitude of the North Equatorial Current west of the dateline, and in the recirculation area of the Kuroshio and its extension, where nonlinear eddy activities were robust. Comparison of the geostrophic meridional transport and the wind-driven Sverdrup meridional transport in a high-resolution OFES simulation showed that nonlinear effects of the ocean circulation were the most likely reason for the differences. It is therefore suggested that the linear, steady wind-driven dynamics of the Sverdrup theory cannot completely explain the meridional transport of the interior circulation of the tropical Northwest Pacific Ocean.
关键词Sverdrup Theory Absolute Geostrophic Current P-vector
学科领域Marine & Freshwater Biology ; Oceanography
DOI10.1007/s00343-013-2169-0
URL查看原文
收录类别SCI
语种英语
WOS研究方向Marine & Freshwater Biology ; Oceanography
WOS类目Limnology ; Oceanography
WOS记录号WOS:000318719700021
WOS关键词SVERDRUP BALANCE ; CIRCULATION ; ATLANTIC ; 24-DEGREES-N ; ACCOUNT ; SEA
WOS标题词Science & Technology ; Life Sciences & Biomedicine ; Physical Sciences
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被引频次:9[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/337002/16409
专题海洋环流与波动重点实验室
通讯作者Yuan, DL
作者单位1.Chinese Acad Sci, Inst Oceanol, Qingdao 266071, Peoples R China
2.Chinese Acad Sci, Key Lab Ocean Circulat & Waves, Qingdao 266071, Peoples R China
3.Chinese Acad Sci, Grad Univ, Beijing 100049, Peoples R China
4.USN, Naval Ocean Anal & Predict NOAP Lab, Dept Oceanog, Postgrad Sch, Monterey, CA USA
第一作者单位中国科学院海洋研究所;  海洋环流与波动重点实验室
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Zhang Zhichun,Yuan Dongliang,Chu, Peter C.,et al. Geostrophic meridional transport in tropical Northwest Pacific based on Argo profiles[J]. CHINESE JOURNAL OF OCEANOLOGY AND LIMNOLOGY,2013,31(3):656-664.
APA Zhang Zhichun,Yuan Dongliang,Chu, Peter C.,&Yuan, DL.(2013).Geostrophic meridional transport in tropical Northwest Pacific based on Argo profiles.CHINESE JOURNAL OF OCEANOLOGY AND LIMNOLOGY,31(3),656-664.
MLA Zhang Zhichun,et al."Geostrophic meridional transport in tropical Northwest Pacific based on Argo profiles".CHINESE JOURNAL OF OCEANOLOGY AND LIMNOLOGY 31.3(2013):656-664.
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