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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Main Authors: Laury Miller, Bob Cheney
Other Authors: The Pennsylvania State University CiteSeerX Archives
Format: Text
Language:English
Published: MIT Press 2001
Subjects:
Online Access:http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.581.2952
http://www.aviso.oceanobs.com/fileadmin/documents/OSTST/1999/esselborn.pdf
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spelling 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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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
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North Atlantic
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North Atlantic
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