Changing the Atmosphere
The difference of the mean SL between the Low (12/92-11/93) and the High (3/96-2/98) is shown to the. The SL of the subpolar gyre rose from the High to the Low period by ~5cm. At the same time the SL along the mean paths of Gulf Stream, Azores Current, and North Atlantic Current fell by up to 15cm....
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ftciteseerx:oai:CiteSeerX.psu:10.1.1.581.2952 2023-05-15T17:25:17+02:00 Changing the Atmosphere Laury Miller Bob Cheney The Pennsylvania State University CiteSeerX Archives 2001 application/pdf http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.581.2952 http://www.aviso.oceanobs.com/fileadmin/documents/OSTST/1999/esselborn.pdf en eng MIT Press http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.581.2952 http://www.aviso.oceanobs.com/fileadmin/documents/OSTST/1999/esselborn.pdf Metadata may be used without restrictions as long as the oai identifier remains attached to it. http://www.aviso.oceanobs.com/fileadmin/documents/OSTST/1999/esselborn.pdf text 2001 ftciteseerx 2016-01-08T13:02:08Z The difference of the mean SL between the Low (12/92-11/93) and the High (3/96-2/98) is shown to the. The SL of the subpolar gyre rose from the High to the Low period by ~5cm. At the same time the SL along the mean paths of Gulf Stream, Azores Current, and North Atlantic Current fell by up to 15cm. period Dynamic heights and SL deviations at section A1E ( ) agree very well, which suggests that SL changes are mainly baroclinically induced. At section A2 the correlation is less pronounced- an indication that barotropic SL changes might be important in the northeastern subtropical gyre. left right University of Hamburg Text north atlantic current North Atlantic Unknown |
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Open Polar |
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Unknown |
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ftciteseerx |
language |
English |
description |
The difference of the mean SL between the Low (12/92-11/93) and the High (3/96-2/98) is shown to the. The SL of the subpolar gyre rose from the High to the Low period by ~5cm. At the same time the SL along the mean paths of Gulf Stream, Azores Current, and North Atlantic Current fell by up to 15cm. period Dynamic heights and SL deviations at section A1E ( ) agree very well, which suggests that SL changes are mainly baroclinically induced. At section A2 the correlation is less pronounced- an indication that barotropic SL changes might be important in the northeastern subtropical gyre. left right University of Hamburg |
author2 |
The Pennsylvania State University CiteSeerX Archives |
format |
Text |
author |
Laury Miller Bob Cheney |
spellingShingle |
Laury Miller Bob Cheney Changing the Atmosphere |
author_facet |
Laury Miller Bob Cheney |
author_sort |
Laury Miller |
title |
Changing the Atmosphere |
title_short |
Changing the Atmosphere |
title_full |
Changing the Atmosphere |
title_fullStr |
Changing the Atmosphere |
title_full_unstemmed |
Changing the Atmosphere |
title_sort |
changing the atmosphere |
publisher |
MIT Press |
publishDate |
2001 |
url |
http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.581.2952 http://www.aviso.oceanobs.com/fileadmin/documents/OSTST/1999/esselborn.pdf |
genre |
north atlantic current North Atlantic |
genre_facet |
north atlantic current North Atlantic |
op_source |
http://www.aviso.oceanobs.com/fileadmin/documents/OSTST/1999/esselborn.pdf |
op_relation |
http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.581.2952 http://www.aviso.oceanobs.com/fileadmin/documents/OSTST/1999/esselborn.pdf |
op_rights |
Metadata may be used without restrictions as long as the oai identifier remains attached to it. |
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1766116664036818944 |