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We show that diapycnal mixing can drive a significant Antarctic Circumpolar Current (ACC) volume transport, even when the mixing is located remotely in northern-hemisphere ocean basins. In the case of remote forcing, the globally-averaged diapycnal m
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=dedup_wf_001::a232e0c5db310ef1db49651aeb4074f2
https://doi.org/10.1029/2011gl046849
https://doi.org/10.1029/2011gl046849
The strength of the Antarctic Circumpolar Current (ACC) is believed to depend on the westerly wind stress blowing over the Southern Ocean, although the exact relationship between winds and circumpolar transport is yet to be determined. Here we show,
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=dedup_wf_001::aff9e8ffbed91b513e08fa9bd952b115
https://ora.ox.ac.uk/objects/uuid:90a6af05-563e-4725-91f7-d09cf6004c6d
https://ora.ox.ac.uk/objects/uuid:90a6af05-563e-4725-91f7-d09cf6004c6d
Autor:
Boulton CA; Earth System Science, College of Life and Environmental Sciences, Laver Building (Level 7), University of Exeter, Exeter EX4 4QE, UK., Allison LC; Earth System Science, College of Life and Environmental Sciences, Laver Building (Level 7), University of Exeter, Exeter EX4 4QE, UK., Lenton TM; Earth System Science, College of Life and Environmental Sciences, Laver Building (Level 7), University of Exeter, Exeter EX4 4QE, UK.
Publikováno v:
Nature communications [Nat Commun] 2014 Dec 08; Vol. 5, pp. 5752. Date of Electronic Publication: 2014 Dec 08.