Does the Wind Control the Import and Export of the South Atlantic?
A different way of examining the meridional flux of warm and intermediate water (su, 27.50) from the Southern Ocean into the South Atlantic is proposed. The method considers the Americas to be a ‘‘pseudo island’’ in the sense that the continent is entirely surrounded by water but has no circulation...
Other Authors: | |
---|---|
Format: | Text |
Language: | English |
Published: |
1999
|
Subjects: | |
Online Access: | http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.691.677 http://doronnof.net/files/76.pdf |
id |
ftciteseerx:oai:CiteSeerX.psu:10.1.1.691.677 |
---|---|
record_format |
openpolar |
spelling |
ftciteseerx:oai:CiteSeerX.psu:10.1.1.691.677 2023-05-15T14:29:15+02:00 Does the Wind Control the Import and Export of the South Atlantic? The Pennsylvania State University CiteSeerX Archives 1999 application/pdf http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.691.677 http://doronnof.net/files/76.pdf en eng http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.691.677 http://doronnof.net/files/76.pdf Metadata may be used without restrictions as long as the oai identifier remains attached to it. http://doronnof.net/files/76.pdf text 1999 ftciteseerx 2016-01-08T18:25:54Z A different way of examining the meridional flux of warm and intermediate water (su, 27.50) from the Southern Ocean into the South Atlantic is proposed. The method considers the Americas to be a ‘‘pseudo island’’ in the sense that the continent is entirely surrounded by water but has no circulation around it. It is shown that, although the northern connection between the Atlantic and the Pacific (via the Bering Strait) is weak, it imposes severe limitations on the sea level in the Atlantic basin: so much so that it allows one to compute the meridional transport without finding the detailed solution to the complete wind–thermohaline problem. The method employs an integration of the linearized momentum equations along a closed contour containing the Americas, Greenland, the Atlantic, and parts of the Arctic Ocean. First, an idealized rectangular model involving three layers, an active continuously stratified upper layer containing both thermocline (su, 26.80) and intermediate water (26.80, su, 27.80), an inert deep layer (27.80, su, 27.90), and a southward moving bottom layer (su. 27.90) is considered. In this idealized model, the Americas are represented by the pseudo island. Deep-water formation is allowed (in the northern part of the basin east of the Americas and south of the gap connecting the Atlantic–Arctic basin to the Pacific), but the cooling rate need not be specified. The basin is subject to both zonal winds and heat exchange with the Text Arctic Basin Arctic Arctic Ocean Atlantic Arctic Atlantic-Arctic Bering Strait Greenland Southern Ocean Unknown Arctic Southern Ocean Arctic Ocean Bering Strait Greenland Pacific |
institution |
Open Polar |
collection |
Unknown |
op_collection_id |
ftciteseerx |
language |
English |
description |
A different way of examining the meridional flux of warm and intermediate water (su, 27.50) from the Southern Ocean into the South Atlantic is proposed. The method considers the Americas to be a ‘‘pseudo island’’ in the sense that the continent is entirely surrounded by water but has no circulation around it. It is shown that, although the northern connection between the Atlantic and the Pacific (via the Bering Strait) is weak, it imposes severe limitations on the sea level in the Atlantic basin: so much so that it allows one to compute the meridional transport without finding the detailed solution to the complete wind–thermohaline problem. The method employs an integration of the linearized momentum equations along a closed contour containing the Americas, Greenland, the Atlantic, and parts of the Arctic Ocean. First, an idealized rectangular model involving three layers, an active continuously stratified upper layer containing both thermocline (su, 26.80) and intermediate water (26.80, su, 27.80), an inert deep layer (27.80, su, 27.90), and a southward moving bottom layer (su. 27.90) is considered. In this idealized model, the Americas are represented by the pseudo island. Deep-water formation is allowed (in the northern part of the basin east of the Americas and south of the gap connecting the Atlantic–Arctic basin to the Pacific), but the cooling rate need not be specified. The basin is subject to both zonal winds and heat exchange with the |
author2 |
The Pennsylvania State University CiteSeerX Archives |
format |
Text |
title |
Does the Wind Control the Import and Export of the South Atlantic? |
spellingShingle |
Does the Wind Control the Import and Export of the South Atlantic? |
title_short |
Does the Wind Control the Import and Export of the South Atlantic? |
title_full |
Does the Wind Control the Import and Export of the South Atlantic? |
title_fullStr |
Does the Wind Control the Import and Export of the South Atlantic? |
title_full_unstemmed |
Does the Wind Control the Import and Export of the South Atlantic? |
title_sort |
does the wind control the import and export of the south atlantic? |
publishDate |
1999 |
url |
http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.691.677 http://doronnof.net/files/76.pdf |
geographic |
Arctic Southern Ocean Arctic Ocean Bering Strait Greenland Pacific |
geographic_facet |
Arctic Southern Ocean Arctic Ocean Bering Strait Greenland Pacific |
genre |
Arctic Basin Arctic Arctic Ocean Atlantic Arctic Atlantic-Arctic Bering Strait Greenland Southern Ocean |
genre_facet |
Arctic Basin Arctic Arctic Ocean Atlantic Arctic Atlantic-Arctic Bering Strait Greenland Southern Ocean |
op_source |
http://doronnof.net/files/76.pdf |
op_relation |
http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.691.677 http://doronnof.net/files/76.pdf |
op_rights |
Metadata may be used without restrictions as long as the oai identifier remains attached to it. |
_version_ |
1766303313105518592 |