Detection of subsurface processes with ERS 1+2 altimeters

The over ow of bottom water through the Denmark Strait and the Faroe Bank Channel uctuates in both temperature and currents. From in situ data it is derived that the uctuations due to steric eects can result in sea surface variability of several centimeters. ERS 1+2 satellite altimeter observations...

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Bibliographic Details
Main Authors: Jacob L. Hyer, Ole B. Andersen, Per Knudsen, Kort Og Matrikelstyrelsen
Other Authors: The Pennsylvania State University CiteSeerX Archives
Format: Text
Language:English
Subjects:
Faroe Bank
Denmark Strait
Online Access:http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.460.270
http://earth.esa.int/pub/ESA_DOC/gothenburg/105hoeye.pdf
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record_format openpolar
spelling ftciteseerx:oai:CiteSeerX.psu:10.1.1.460.270 2023-05-15T16:00:37+02:00 Detection of subsurface processes with ERS 1+2 altimeters Jacob L. Hyer Ole B. Andersen Per Knudsen Kort Og Matrikelstyrelsen The Pennsylvania State University CiteSeerX Archives application/pdf http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.460.270 http://earth.esa.int/pub/ESA_DOC/gothenburg/105hoeye.pdf en eng http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.460.270 http://earth.esa.int/pub/ESA_DOC/gothenburg/105hoeye.pdf Metadata may be used without restrictions as long as the oai identifier remains attached to it. http://earth.esa.int/pub/ESA_DOC/gothenburg/105hoeye.pdf text ftciteseerx 2016-01-08T06:31:58Z The over ow of bottom water through the Denmark Strait and the Faroe Bank Channel uctuates in both temperature and currents. From in situ data it is derived that the uctuations due to steric eects can result in sea surface variability of several centimeters. ERS 1+2 satellite altimeter observations conrm the results from in situ observations and detect enhanced sea surface height variability in regions immediately downstream of the sills. Subsurface processes such as over ows can thus be detected by ERS 1+2 data. Text Denmark Strait Unknown Faroe Bank ENVELOPE(-8.667,-8.667,60.917,60.917)
institution Open Polar
collection Unknown
op_collection_id ftciteseerx
language English
description The over ow of bottom water through the Denmark Strait and the Faroe Bank Channel uctuates in both temperature and currents. From in situ data it is derived that the uctuations due to steric eects can result in sea surface variability of several centimeters. ERS 1+2 satellite altimeter observations conrm the results from in situ observations and detect enhanced sea surface height variability in regions immediately downstream of the sills. Subsurface processes such as over ows can thus be detected by ERS 1+2 data.
author2 The Pennsylvania State University CiteSeerX Archives
format Text
author Jacob L. Hyer
Ole B. Andersen
Per Knudsen
Kort Og Matrikelstyrelsen
spellingShingle Jacob L. Hyer
Ole B. Andersen
Per Knudsen
Kort Og Matrikelstyrelsen
Detection of subsurface processes with ERS 1+2 altimeters
author_facet Jacob L. Hyer
Ole B. Andersen
Per Knudsen
Kort Og Matrikelstyrelsen
author_sort Jacob L. Hyer
title Detection of subsurface processes with ERS 1+2 altimeters
title_short Detection of subsurface processes with ERS 1+2 altimeters
title_full Detection of subsurface processes with ERS 1+2 altimeters
title_fullStr Detection of subsurface processes with ERS 1+2 altimeters
title_full_unstemmed Detection of subsurface processes with ERS 1+2 altimeters
title_sort detection of subsurface processes with ers 1+2 altimeters
url http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.460.270
http://earth.esa.int/pub/ESA_DOC/gothenburg/105hoeye.pdf
long_lat ENVELOPE(-8.667,-8.667,60.917,60.917)
geographic Faroe Bank
geographic_facet Faroe Bank
genre Denmark Strait
genre_facet Denmark Strait
op_source http://earth.esa.int/pub/ESA_DOC/gothenburg/105hoeye.pdf
op_relation http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.460.270
http://earth.esa.int/pub/ESA_DOC/gothenburg/105hoeye.pdf
op_rights Metadata may be used without restrictions as long as the oai identifier remains attached to it.
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