How Does Antarctic Bottom Water Cross the Southern Ocean?

被引:52
作者
Solodoch, A. [1 ]
Stewart, A. L. [1 ]
Hogg, A. McC. [2 ,3 ]
Morrison, A. K. [2 ,4 ]
Kiss, A. E. [2 ,3 ]
Thompson, A. F. [5 ]
Purkey, S. G. [6 ]
Cimoli, L. [6 ]
机构
[1] Univ Calif Los Angeles, Dept Atmospher & Ocean Sci, Los Angeles, CA 90095 USA
[2] Australian Natl Univ, Res Sch Earth Sci, Canberra, ACT, Australia
[3] ARC Ctr Excellence Climate Extremes, Douglas, Qld, Australia
[4] Australian Ctr Excellence Antarctic Sci, Parkville, Vic, Australia
[5] CALTECH, Environm Sci & Engn, Pasadena, CA 91125 USA
[6] Scripps Inst Oceanog, UCSD, San Diego, CA USA
基金
澳大利亚研究理事会; 美国国家科学基金会; 美国国家航空航天局;
关键词
meridional overturning circulation; Antarctic Bottom Water; ocean circulation; Southern Ocean; Deep Western Boundary Currents; ocean stirring; GLOBAL OVERTURNING CIRCULATION; WEDDELL GYRE; SEA-ICE; CIRCUMPOLAR CURRENT; DEEP; TRANSPORT; VENTILATION; PACIFIC; DENSITY; EXPORT;
D O I
10.1029/2021GL097211
中图分类号
P [天文学、地球科学];
学科分类号
07 ;
摘要
Antarctic Bottom Water (AABW), which fills the global ocean abyss, is derived from dense water that forms in several distinct Antarctic shelf regions. Previous modeling studies have reached conflicting conclusions regarding export pathways of AABW across the Southern Ocean and the degree to which AABW originating from distinct source regions are blended during their export. This study addresses these questions using passive tracer deployments in a 61-year global high-resolution (0.1 degrees) ocean/sea-ice simulation. Two distinct export "conduits" are identified: Weddell Sea- and Prydz Bay-sourced AABW are blended together and exported mainly to the Atlantic and Indian Oceans, while Ross Sea- and Adelie Land-sourced AABW are exported mainly to the Pacific Ocean. Northward transport of each tracer occurs almost exclusively (>90%) within a single conduit. These findings imply that regional changes in AABW production may impact the three-dimensional structure of the global overturning circulation.
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页数:11
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