The thermodynamic balance of the Weddell Gyre

被引:24
作者
Garabato, Alberto C. Naveira [1 ]
Zika, Jan D. [1 ]
Jullion, Loic [2 ,3 ]
Brown, Peter J. [4 ]
Holland, Paul R. [5 ]
Meredith, Michael P. [5 ]
Bacon, Sheldon [4 ]
机构
[1] Univ Southampton, Natl Oceanog Ctr, Southampton, Hants, England
[2] Aix Marseille Univ, CNRS INSU, IRD, MIO, Marseille, France
[3] Univ Toulon & Var, CNRS INSU, IRD, MIO, La Garde, France
[4] Natl Oceanog Ctr, Southampton, Hants, England
[5] British Antarctic Survey, Cambridge CB3 0ET, England
基金
英国自然环境研究理事会;
关键词
Weddell Gyre; thermodynamics; SEA-ICE; SOUTHERN-OCEAN; DEEP; STRATIFICATION; CIRCULATION;
D O I
10.1002/2015GL066658
中图分类号
P [天文学、地球科学];
学科分类号
07 ;
摘要
The thermodynamic balance of the Weddell Gyre is assessed from an inverse estimate of the circulation across the gyre's rim. The gyre experiences a weak net buoyancy gain that arises from a leading-order cancelation between two opposing contributions, linked to two cells of water mass transformation and diapycnal overturning. The lower cell involves a cooling-driven densification of 8.42.0Sv of Circumpolar Deep Water and Antarctic Bottom Water near the gyre's southern and western margins. The upper cell entails a freshening-driven conversion of 4.92.0Sv of Circumpolar Deep Water into lighter upper ocean waters within the gyre interior. The distinct role of salinity between the two cells stems from opposing salinity changes induced by sea ice production, meteoric sources, and admixture of fresh upper ocean waters in the lower cell, which contrasts with coherent reductions in salinity associated with sea ice melting and meteoric sources in the upper cell.
引用
收藏
页码:317 / 325
页数:9
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