Modification of the deep salinity-maximum in the Southern Ocean by circulation in the Antarctic Circumpolar Current and the Weddell Gyre
Author:
Funder
Natural Environment Research Council (GB)
Publisher
Springer Science and Business Media LLC
Subject
Oceanography
Link
http://link.springer.com/article/10.1007/s10236-017-1054-3/fulltext.html
Reference61 articles.
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2. Bindoff NL, Rosenberg MA, Warner MJ (2000) On the circulation and water masses over the Antarctic continental slope and rise between 80 and 150°E. Deep-Sea Res II Top Stud Oceanogr 47:2299–2326
3. Callahan JE (1972) The structure and circulation of deep water in the Antarctic. Deep Sea Research and Oceanographic Abstracts 19:563–575. doi: 10.1016/0011-7471(72)90040-x
4. Cisewski B, Strass VH, Prandke H (2005) Upper-ocean vertical mixing in the Antarctic Polar Front Zone. Deep-Sea Res II Top Stud Oceanogr 52:1087–1108. doi: 10.1016/j.dsr2.2005.01.010
5. Cisewski B, Strass VH, Losch M, Prandke H (2008) Mixed layer analysis of a mesoscale eddy in the Antarctic Polar Front Zone. Journal of Geophysical Research-Oceans 113:19. doi: 10.1029/2007jc004372
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