An exchange window for the Injection of Antarctic Intermediate Water into the South Pacific
An exchange window for the Injection of Antarctic Intermediate Water into the South Pacific
Antarctic Intermediate Water (AAIW) occupies the intermediate horizon of most of the world oceans. Formed in the Southern Ocean, it is characterized by a relative salinity minimum. With a new, denser in situ National Oceanographic Data Center dataset, the authors have reanalyzed the export characteristics of AAIW from the Southern Ocean into the South Pacific Ocean. These new data show that part of the AAIW is exported from the subpolar frontal region by the large-scale circulation through an exchange window of 10° width situated east of 90°W in the southeast corner of the Pacific basin. This suggests the origin of this water to be in the Antarctic Circumpolar Current. A set of numerical modeling experiments has been used to reproduce these observed features and to demonstrate that the dynamics of the exchange window is controlled by the basin-scale meridional pressure gradient. The exchange of AAIW between the Southern and Pacific Oceans must therefore be understood in the context of the large basin-scale dynamical balance rather than simply local effects.
31-49
Iudicone, Daniele
e126ed06-8bab-4971-abf1-98a0d5f9dc7f
Rodgers, Keith B.
1078c51c-546c-486a-90fb-f33a5662338a
Schopp, Richard
cca6c24c-e18b-46d8-8763-7da6973d42a2
Madec, Gurvan
ffb28deb-4bbd-4a4c-914f-492f813e4864
January 2007
Iudicone, Daniele
e126ed06-8bab-4971-abf1-98a0d5f9dc7f
Rodgers, Keith B.
1078c51c-546c-486a-90fb-f33a5662338a
Schopp, Richard
cca6c24c-e18b-46d8-8763-7da6973d42a2
Madec, Gurvan
ffb28deb-4bbd-4a4c-914f-492f813e4864
Iudicone, Daniele, Rodgers, Keith B., Schopp, Richard and Madec, Gurvan
(2007)
An exchange window for the Injection of Antarctic Intermediate Water into the South Pacific.
Journal of Physical Oceanography, 37 (1), .
(doi:10.1175/JPO2985.1).
Abstract
Antarctic Intermediate Water (AAIW) occupies the intermediate horizon of most of the world oceans. Formed in the Southern Ocean, it is characterized by a relative salinity minimum. With a new, denser in situ National Oceanographic Data Center dataset, the authors have reanalyzed the export characteristics of AAIW from the Southern Ocean into the South Pacific Ocean. These new data show that part of the AAIW is exported from the subpolar frontal region by the large-scale circulation through an exchange window of 10° width situated east of 90°W in the southeast corner of the Pacific basin. This suggests the origin of this water to be in the Antarctic Circumpolar Current. A set of numerical modeling experiments has been used to reproduce these observed features and to demonstrate that the dynamics of the exchange window is controlled by the basin-scale meridional pressure gradient. The exchange of AAIW between the Southern and Pacific Oceans must therefore be understood in the context of the large basin-scale dynamical balance rather than simply local effects.
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Published date: January 2007
Identifiers
Local EPrints ID: 64343
URI: http://eprints.soton.ac.uk/id/eprint/64343
ISSN: 0022-3670
PURE UUID: fc5f6b36-efed-4f3e-a71f-c56104e2df16
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Date deposited: 10 Dec 2008
Last modified: 15 Mar 2024 11:48
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Contributors
Author:
Daniele Iudicone
Author:
Keith B. Rodgers
Author:
Richard Schopp
Author:
Gurvan Madec
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