D!3BEBCE % BE Fast Northward Energy Transfer in the Atlantic due to Agulhas Rings
The adiabatic transit time of wave energy radiated by an Agulhas ring released in the South Atlantic Ocean to the North Atlantic Ocean is investigated in a two-layer ocean model. Of particular interest is the arrival time of baroclinic energy in the northern part of the Atlantic, because it is relat...
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ftciteseerx:oai:CiteSeerX.psu:10.1.1.658.1722 2023-05-15T17:33:51+02:00 D!3BEBCE % BE Fast Northward Energy Transfer in the Atlantic due to Agulhas Rings Erik Van Sebille Peter Jan Van Leeuwen The Pennsylvania State University CiteSeerX Archives 2006 application/pdf http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.658.1722 http://centaur.reading.ac.uk/24131/1/Vansebille-2007.pdf en eng http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.658.1722 http://centaur.reading.ac.uk/24131/1/Vansebille-2007.pdf Metadata may be used without restrictions as long as the oai identifier remains attached to it. http://centaur.reading.ac.uk/24131/1/Vansebille-2007.pdf text 2006 ftciteseerx 2016-01-08T16:42:44Z The adiabatic transit time of wave energy radiated by an Agulhas ring released in the South Atlantic Ocean to the North Atlantic Ocean is investigated in a two-layer ocean model. Of particular interest is the arrival time of baroclinic energy in the northern part of the Atlantic, because it is related to variations in the meridional overturning circulation. The influence of the Mid-Atlantic Ridge is also studied, because it allows for the conversion from barotropic to baroclinic wave energy and the generation of topographic waves. Barotropic energy from the ring is present in the northern part of the model basin within 10 days. From that time, the barotropic energy keeps rising to attain a maximum 500 days after initiation. This is independent of the presence or absence of a ridge in the model basin. Without a ridge in the model, the travel time of the baroclinic signal is 1300 days. This time is similar to the transit time of the ring from the eastern to the western coast of the model basin. In the presence of the ridge, the baroclinic signal arrives in the northern part of the model basin after approximately 10 days, which is the same time scale as that of Text North Atlantic South Atlantic Ocean Unknown Mid-Atlantic Ridge |
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Open Polar |
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Unknown |
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ftciteseerx |
language |
English |
description |
The adiabatic transit time of wave energy radiated by an Agulhas ring released in the South Atlantic Ocean to the North Atlantic Ocean is investigated in a two-layer ocean model. Of particular interest is the arrival time of baroclinic energy in the northern part of the Atlantic, because it is related to variations in the meridional overturning circulation. The influence of the Mid-Atlantic Ridge is also studied, because it allows for the conversion from barotropic to baroclinic wave energy and the generation of topographic waves. Barotropic energy from the ring is present in the northern part of the model basin within 10 days. From that time, the barotropic energy keeps rising to attain a maximum 500 days after initiation. This is independent of the presence or absence of a ridge in the model basin. Without a ridge in the model, the travel time of the baroclinic signal is 1300 days. This time is similar to the transit time of the ring from the eastern to the western coast of the model basin. In the presence of the ridge, the baroclinic signal arrives in the northern part of the model basin after approximately 10 days, which is the same time scale as that of |
author2 |
The Pennsylvania State University CiteSeerX Archives |
format |
Text |
author |
Erik Van Sebille Peter Jan Van Leeuwen |
spellingShingle |
Erik Van Sebille Peter Jan Van Leeuwen D!3BEBCE % BE Fast Northward Energy Transfer in the Atlantic due to Agulhas Rings |
author_facet |
Erik Van Sebille Peter Jan Van Leeuwen |
author_sort |
Erik Van |
title |
D!3BEBCE % BE Fast Northward Energy Transfer in the Atlantic due to Agulhas Rings |
title_short |
D!3BEBCE % BE Fast Northward Energy Transfer in the Atlantic due to Agulhas Rings |
title_full |
D!3BEBCE % BE Fast Northward Energy Transfer in the Atlantic due to Agulhas Rings |
title_fullStr |
D!3BEBCE % BE Fast Northward Energy Transfer in the Atlantic due to Agulhas Rings |
title_full_unstemmed |
D!3BEBCE % BE Fast Northward Energy Transfer in the Atlantic due to Agulhas Rings |
title_sort |
d!3bebce % be fast northward energy transfer in the atlantic due to agulhas rings |
publishDate |
2006 |
url |
http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.658.1722 http://centaur.reading.ac.uk/24131/1/Vansebille-2007.pdf |
geographic |
Mid-Atlantic Ridge |
geographic_facet |
Mid-Atlantic Ridge |
genre |
North Atlantic South Atlantic Ocean |
genre_facet |
North Atlantic South Atlantic Ocean |
op_source |
http://centaur.reading.ac.uk/24131/1/Vansebille-2007.pdf |
op_relation |
http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.658.1722 http://centaur.reading.ac.uk/24131/1/Vansebille-2007.pdf |
op_rights |
Metadata may be used without restrictions as long as the oai identifier remains attached to it. |
_version_ |
1766132484446093312 |