Application of continuation methods in physical oceanography
A specific example will be considered in which continuation methods are used to study fundamental problems in physical oceanography.The separation be- havior of the Gulf Stream in the North Atlantic is a long standing problem in dynamical oceanography,with state-of-the-art ocean models still having...
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ftunivutrecht:oai:dspace.library.uu.nl:1874/2205 2023-07-23T04:20:29+02:00 Application of continuation methods in physical oceanography Katsman, C.A. Dijkstra, H.A. Schmeits, M.J. 1999-01-21 application/pdf https://dspace.library.uu.nl/handle/1874/2205 en eng https://dspace.library.uu.nl/handle/1874/2205 info:eu-repo/semantics/OpenAccess Aardwetenschappen Article 1999 ftunivutrecht 2023-07-01T22:43:25Z A specific example will be considered in which continuation methods are used to study fundamental problems in physical oceanography.The separation be- havior of the Gulf Stream in the North Atlantic is a long standing problem in dynamical oceanography,with state-of-the-art ocean models still having trouble to simulate to correct mean path.Bifurcation analysis in simplified models,as used here,points to one of difficulties involved:there may be two separation paths at the same forcing conditions.By studying the stability of steady North Atlantic ocean circulation patterns,also transitions to time-dependence are found which are linked to specific low frequency variability in the Gulf Stream region. Article in Journal/Newspaper North Atlantic Utrecht University Repository |
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Open Polar |
collection |
Utrecht University Repository |
op_collection_id |
ftunivutrecht |
language |
English |
topic |
Aardwetenschappen |
spellingShingle |
Aardwetenschappen Katsman, C.A. Dijkstra, H.A. Schmeits, M.J. Application of continuation methods in physical oceanography |
topic_facet |
Aardwetenschappen |
description |
A specific example will be considered in which continuation methods are used to study fundamental problems in physical oceanography.The separation be- havior of the Gulf Stream in the North Atlantic is a long standing problem in dynamical oceanography,with state-of-the-art ocean models still having trouble to simulate to correct mean path.Bifurcation analysis in simplified models,as used here,points to one of difficulties involved:there may be two separation paths at the same forcing conditions.By studying the stability of steady North Atlantic ocean circulation patterns,also transitions to time-dependence are found which are linked to specific low frequency variability in the Gulf Stream region. |
format |
Article in Journal/Newspaper |
author |
Katsman, C.A. Dijkstra, H.A. Schmeits, M.J. |
author_facet |
Katsman, C.A. Dijkstra, H.A. Schmeits, M.J. |
author_sort |
Katsman, C.A. |
title |
Application of continuation methods in physical oceanography |
title_short |
Application of continuation methods in physical oceanography |
title_full |
Application of continuation methods in physical oceanography |
title_fullStr |
Application of continuation methods in physical oceanography |
title_full_unstemmed |
Application of continuation methods in physical oceanography |
title_sort |
application of continuation methods in physical oceanography |
publishDate |
1999 |
url |
https://dspace.library.uu.nl/handle/1874/2205 |
genre |
North Atlantic |
genre_facet |
North Atlantic |
op_relation |
https://dspace.library.uu.nl/handle/1874/2205 |
op_rights |
info:eu-repo/semantics/OpenAccess |
_version_ |
1772184881932009472 |