The South Atlantic in the Fine-Resolution Antarctic Model

The geographical area covered by the Fine-Resolution Antarctic Model (FRAM) includes that part of the South Atlantic south of 24°S. A description of the dynamics and thermodynamics of this region of the model is presented. Both the mean and eddy fields in the model are in good agreement with rea...

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Main Authors: D. P. Stevens, S. R. Thompson
Format: Article
Language:English
Published: Copernicus Publications 1994-08-01
Series:Annales Geophysicae
Online Access:https://www.ann-geophys.net/12/826/1994/angeo-12-826-1994.pdf
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author D. P. Stevens
S. R. Thompson
author_facet D. P. Stevens
S. R. Thompson
author_sort D. P. Stevens
collection DOAJ
description The geographical area covered by the Fine-Resolution Antarctic Model (FRAM) includes that part of the South Atlantic south of 24°S. A description of the dynamics and thermodynamics of this region of the model is presented. Both the mean and eddy fields in the model are in good agreement with reality, although the magnitude of the transients is somewhat reduced. The heat flux is northward and in broad agreement with many other estimates. Agulhas eddies are formed by the model and propagate westward into the Atlantic providing a mechanism for fluxing heat from the Indian Ocean. The confluence of the Brazil and Falkland currents produces a strong front and a large amount of mesoscale activity. In the less stratified regions to the south, topographic steering of the Antarctic circumpolar current is important.
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spelling doaj.art-e8a515abb74a49c9ac890891003b80942022-12-22T01:36:56ZengCopernicus PublicationsAnnales Geophysicae0992-76891432-05761994-08-011282683910.1007/s00585-994-0826-5The South Atlantic in the Fine-Resolution Antarctic ModelD. P. StevensS. R. ThompsonThe geographical area covered by the Fine-Resolution Antarctic Model (FRAM) includes that part of the South Atlantic south of 24°S. A description of the dynamics and thermodynamics of this region of the model is presented. Both the mean and eddy fields in the model are in good agreement with reality, although the magnitude of the transients is somewhat reduced. The heat flux is northward and in broad agreement with many other estimates. Agulhas eddies are formed by the model and propagate westward into the Atlantic providing a mechanism for fluxing heat from the Indian Ocean. The confluence of the Brazil and Falkland currents produces a strong front and a large amount of mesoscale activity. In the less stratified regions to the south, topographic steering of the Antarctic circumpolar current is important.https://www.ann-geophys.net/12/826/1994/angeo-12-826-1994.pdf
spellingShingle D. P. Stevens
S. R. Thompson
The South Atlantic in the Fine-Resolution Antarctic Model
Annales Geophysicae
title The South Atlantic in the Fine-Resolution Antarctic Model
title_full The South Atlantic in the Fine-Resolution Antarctic Model
title_fullStr The South Atlantic in the Fine-Resolution Antarctic Model
title_full_unstemmed The South Atlantic in the Fine-Resolution Antarctic Model
title_short The South Atlantic in the Fine-Resolution Antarctic Model
title_sort south atlantic in the fine resolution antarctic model
url https://www.ann-geophys.net/12/826/1994/angeo-12-826-1994.pdf
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