IOCAS-IR  > 海洋环流与波动重点实验室
Fronts, baroclinic transport, and mesoscale variability of the Antarctic Circumpolar Current in the southeast Indian Ocean
Duan Yongliang1,2,3; Hou Yijun1,2; Liu Hongwei1,2,3; Hu Po1,2; Hou, YJ (reprint author), Chinese Acad Sci, Inst Oceanol, Qingdao 266071, Peoples R China.
2012-11-01
发表期刊ACTA OCEANOLOGICA SINICA
ISSN0253-505X
卷号31期号:6页码:1-11
文章类型Article
摘要Fronts, baroclinic transport, and mesoscale variability of the Antarctic Circumpolar Current (ACC) along 115A degrees E are examined on the basis of CTD data from two hydrographic cruises occupied in 1995 as a part of the World Ocean Circulation Experiment (WOCE cruise I9S) and in 2004 as a part of CLIVAR/CO2 repeat hydrography program. The integrated baroclinic transport across I9S section is (97.2x10(6)+/- 2.2x10(6)) m(3)/s relative to the deepest common level (DCL). The net transport at the north end of I9S, determined by the south Australian circulation system, is about 16.5x10(6) m(3)/s westward. Relying on a consistent set of water mass criteria and transport maxima, the ACC baroclinic transport, (117x10(6)+/- 6.7x10(6)) m(3)/s to the east, is carried along three fronts: the Subantarctic Front (SAF) at a mean latitude of 44A degrees-49A degrees S carries (50.6x10(6)+/- 13.4x10(6)) m(3)/s; the Polar Front (PF), with the northern branch (PF-N) at 50.5A degrees S and the southern branch (PFS) at 58A degrees S, carries (51.3x10(6)+/- 8.7x10(6)) m(3)/s; finally, the southern ACC front (SACCF) and the southern boundary of the ACC (SB) consist of three cores between 59A degrees S and 65A degrees S that combined carry (15.2x10(6)+/- 1.8x10(6)) m(3)/s. Mesoscale eddy features are identifiable in the CTD sections and tracked in concurrent maps of altimetric sea level anomalies (SLA) between 44A degrees-48A degrees S and 53A degrees-57A degrees S. Because of the remarkable mesoscale eddy features within the SAF observed in both the tracks of the cruises, the eastward transport of the SAF occurs at two latitude bands separating by 1A degrees. Both the CTD and the altimetric data suggest that the mesoscale variability is concentrated around the Antarctic Polar Frontal Zone (APFZ) and causes the ACC fronts to merge, diverge, and to fluctuate in intensity and position along their paths.
关键词Antarctic Circumpolar Current Fronts Transport Eddies
学科领域Oceanography
DOI10.1007/s13131-012-0248-2
URL查看原文
收录类别SCI
语种英语
WOS记录号WOS:000312494000001
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被引频次:3[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/337002/12150
专题海洋环流与波动重点实验室
通讯作者Hou, YJ (reprint author), Chinese Acad Sci, Inst Oceanol, Qingdao 266071, Peoples R China.
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.Univ Chinese Acad Sci, Beijing 100049, Peoples R China
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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Duan Yongliang,Hou Yijun,Liu Hongwei,et al. Fronts, baroclinic transport, and mesoscale variability of the Antarctic Circumpolar Current in the southeast Indian Ocean[J]. ACTA OCEANOLOGICA SINICA,2012,31(6):1-11.
APA Duan Yongliang,Hou Yijun,Liu Hongwei,Hu Po,&Hou, YJ .(2012).Fronts, baroclinic transport, and mesoscale variability of the Antarctic Circumpolar Current in the southeast Indian Ocean.ACTA OCEANOLOGICA SINICA,31(6),1-11.
MLA Duan Yongliang,et al."Fronts, baroclinic transport, and mesoscale variability of the Antarctic Circumpolar Current in the southeast Indian Ocean".ACTA OCEANOLOGICA SINICA 31.6(2012):1-11.
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