- Abstract:
-
Gill’s (1968) model of the Antarctic Circumpolar Current (ACC) is reinterpreted for a stratified, reduced-gravity ocean, where the barotropic streamfunction is replaced by the pycnocline depth, and the bottom drag coefficient by the Gent and McWilliams eddy diffusivity. The resultant model gives a simple description of the lateral structure of the ACC that is consistent with contemporary descriptions of ACC dynamics. The model is used to investigate and interpret the sensitivity of the ACC to...
Expand abstract - Publication status:
- Published
- Peer review status:
- Peer reviewed
- Version:
- Accepted manuscript
- Files:
-
-
(pdf, 3.7mb)
-
- Publisher copy:
- 10.1016/j.ocemod.2015.11.010
-
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- Publisher:
- Elsevier Publisher's website
- Journal:
- Ocean Modelling Journal website
- Volume:
- 97
- Pages:
- 37-51
- Publication date:
- 2015-11-28
- DOI:
- ISSN:
-
1463-5011
- URN:
-
uuid:c776c368-96f3-464c-8b45-b0ea7a235b16
- Source identifiers:
-
580056
- Local pid:
- pubs:580056
- Copyright holder:
- Elsevier
- Copyright date:
- 2015
- Notes:
- © 2015 Elsevier Ltd. All rights reserved. This is the accepted manuscript version of the article. The final version is available online from Elsevier at: [10.1016/j.ocemod.2015.11.010].
Journal article
Gill’s model of the Antarctic Circumpolar Current, revisited: The role of latitudinal variations in wind stress
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