SEA LEVEL ANOMALIES IN THE LABRADOR SEA
The shallow circulation variability in the subpolar North Atlantic is analyzed using altimeter sea level anomalies from 1993 to 2004. Empirical orthogonal function analysis shows a long-term trend for the whole study area while a more localized analysis in the Labrador Sea shows patterns of interann...
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ftciteseerx:oai:CiteSeerX.psu:10.1.1.570.1998 2023-05-15T17:06:02+02:00 SEA LEVEL ANOMALIES IN THE LABRADOR SEA The Pennsylvania State University CiteSeerX Archives application/pdf http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.570.1998 http://earth.esa.int/workshops/venice06/participants/184/paper_184_funk.pdf en eng http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.570.1998 http://earth.esa.int/workshops/venice06/participants/184/paper_184_funk.pdf Metadata may be used without restrictions as long as the oai identifier remains attached to it. http://earth.esa.int/workshops/venice06/participants/184/paper_184_funk.pdf text ftciteseerx 2016-01-08T12:29:21Z The shallow circulation variability in the subpolar North Atlantic is analyzed using altimeter sea level anomalies from 1993 to 2004. Empirical orthogonal function analysis shows a long-term trend for the whole study area while a more localized analysis in the Labrador Sea shows patterns of interannual variability but no long-term trends. Largest variability is found in the western boundary current near 53°N in combination with a recirculation cell farther offshore. General agreement between velocity anomalies derived from altimetry and by moored instrumentation is found. An intensification of the recirculation cell may be associated with an increase of northward warm water transport. This variability pattern is supported by variations in microwave sea surface temperatures. 1. Text Labrador Sea North Atlantic Unknown |
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ftciteseerx |
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English |
description |
The shallow circulation variability in the subpolar North Atlantic is analyzed using altimeter sea level anomalies from 1993 to 2004. Empirical orthogonal function analysis shows a long-term trend for the whole study area while a more localized analysis in the Labrador Sea shows patterns of interannual variability but no long-term trends. Largest variability is found in the western boundary current near 53°N in combination with a recirculation cell farther offshore. General agreement between velocity anomalies derived from altimetry and by moored instrumentation is found. An intensification of the recirculation cell may be associated with an increase of northward warm water transport. This variability pattern is supported by variations in microwave sea surface temperatures. 1. |
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The Pennsylvania State University CiteSeerX Archives |
format |
Text |
title |
SEA LEVEL ANOMALIES IN THE LABRADOR SEA |
spellingShingle |
SEA LEVEL ANOMALIES IN THE LABRADOR SEA |
title_short |
SEA LEVEL ANOMALIES IN THE LABRADOR SEA |
title_full |
SEA LEVEL ANOMALIES IN THE LABRADOR SEA |
title_fullStr |
SEA LEVEL ANOMALIES IN THE LABRADOR SEA |
title_full_unstemmed |
SEA LEVEL ANOMALIES IN THE LABRADOR SEA |
title_sort |
sea level anomalies in the labrador sea |
url |
http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.570.1998 http://earth.esa.int/workshops/venice06/participants/184/paper_184_funk.pdf |
genre |
Labrador Sea North Atlantic |
genre_facet |
Labrador Sea North Atlantic |
op_source |
http://earth.esa.int/workshops/venice06/participants/184/paper_184_funk.pdf |
op_relation |
http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.570.1998 http://earth.esa.int/workshops/venice06/participants/184/paper_184_funk.pdf |
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Metadata may be used without restrictions as long as the oai identifier remains attached to it. |
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1766060929598881792 |