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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Other Authors: The Pennsylvania State University CiteSeerX Archives
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Online Access: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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spelling 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
institution Open Polar
collection Unknown
op_collection_id ftciteseerx
language 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.
author2 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
op_rights Metadata may be used without restrictions as long as the oai identifier remains attached to it.
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