Studies of Eddies in the Marginal Ice Zone Along the East Greenland Current Using Spaceborne Synthetic Aperture Radar (SAR)

The characteristic ice edge eddies in the Marginal Ice Zone (MIZ) are studied based on satellite information from the Advanced Synthetic Aperture Radar (ASAR) instrument. The eddies frequency of existence during the day, month, and year, and their relationship to the wind field conditions are consid...

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Bibliographic Details
Main Author: Bondevik, Elin
Format: Master Thesis
Language:Norwegian Bokmål
Published: The University of Bergen 2011
Subjects:
Online Access:https://hdl.handle.net/1956/5113
id ftunivbergen:oai:bora.uib.no:1956/5113
record_format openpolar
spelling ftunivbergen:oai:bora.uib.no:1956/5113 2023-05-15T16:03:49+02:00 Studies of Eddies in the Marginal Ice Zone Along the East Greenland Current Using Spaceborne Synthetic Aperture Radar (SAR) Bondevik, Elin 2011-06-01 6354615 bytes application/pdf https://hdl.handle.net/1956/5113 nob nob The University of Bergen https://hdl.handle.net/1956/5113 Copyright the author. All rights reserved 756213 VDP::Mathematics and natural science: 400::Geosciences: 450::Oceanography: 452 VDP::Mathematics and natural science: 400::Physics: 430 Master thesis 2011 ftunivbergen 2023-03-14T17:43:03Z The characteristic ice edge eddies in the Marginal Ice Zone (MIZ) are studied based on satellite information from the Advanced Synthetic Aperture Radar (ASAR) instrument. The eddies frequency of existence during the day, month, and year, and their relationship to the wind field conditions are considered. On average, more than 1000 sea ice eddies were counted along the ice margin per year for 2008 and 2009. Eddies contribute to an enhanced melting by forcing contact between the sea ice and the warmer water off the ice edge. The amount of sea ice an eddy can carry is estimated to be 1413.7 km^2. This constitutes 0.7*10^6 by including the modified total of eddies during a year. The daily retreat of the ice edge is found to be 3.5 km d^-1 per 100 km of ice edge. This estimation is based on the bottom ablation, radius of the eddy, distance between two neighbouring eddies, thickness of ice and fraction of sea ice trapped in an eddy. The influence of the wind shows that relative low wind speed and wind directed from the north favours the existence of eddies. Master i Meteorologi og oseanografi MAMN-GEOF GEOF399 Master Thesis East Greenland east greenland current Greenland Sea ice University of Bergen: Bergen Open Research Archive (BORA-UiB) Asar ENVELOPE(134.033,134.033,68.667,68.667) Greenland
institution Open Polar
collection University of Bergen: Bergen Open Research Archive (BORA-UiB)
op_collection_id ftunivbergen
language Norwegian Bokmål
topic 756213
VDP::Mathematics and natural science: 400::Geosciences: 450::Oceanography: 452
VDP::Mathematics and natural science: 400::Physics: 430
spellingShingle 756213
VDP::Mathematics and natural science: 400::Geosciences: 450::Oceanography: 452
VDP::Mathematics and natural science: 400::Physics: 430
Bondevik, Elin
Studies of Eddies in the Marginal Ice Zone Along the East Greenland Current Using Spaceborne Synthetic Aperture Radar (SAR)
topic_facet 756213
VDP::Mathematics and natural science: 400::Geosciences: 450::Oceanography: 452
VDP::Mathematics and natural science: 400::Physics: 430
description The characteristic ice edge eddies in the Marginal Ice Zone (MIZ) are studied based on satellite information from the Advanced Synthetic Aperture Radar (ASAR) instrument. The eddies frequency of existence during the day, month, and year, and their relationship to the wind field conditions are considered. On average, more than 1000 sea ice eddies were counted along the ice margin per year for 2008 and 2009. Eddies contribute to an enhanced melting by forcing contact between the sea ice and the warmer water off the ice edge. The amount of sea ice an eddy can carry is estimated to be 1413.7 km^2. This constitutes 0.7*10^6 by including the modified total of eddies during a year. The daily retreat of the ice edge is found to be 3.5 km d^-1 per 100 km of ice edge. This estimation is based on the bottom ablation, radius of the eddy, distance between two neighbouring eddies, thickness of ice and fraction of sea ice trapped in an eddy. The influence of the wind shows that relative low wind speed and wind directed from the north favours the existence of eddies. Master i Meteorologi og oseanografi MAMN-GEOF GEOF399
format Master Thesis
author Bondevik, Elin
author_facet Bondevik, Elin
author_sort Bondevik, Elin
title Studies of Eddies in the Marginal Ice Zone Along the East Greenland Current Using Spaceborne Synthetic Aperture Radar (SAR)
title_short Studies of Eddies in the Marginal Ice Zone Along the East Greenland Current Using Spaceborne Synthetic Aperture Radar (SAR)
title_full Studies of Eddies in the Marginal Ice Zone Along the East Greenland Current Using Spaceborne Synthetic Aperture Radar (SAR)
title_fullStr Studies of Eddies in the Marginal Ice Zone Along the East Greenland Current Using Spaceborne Synthetic Aperture Radar (SAR)
title_full_unstemmed Studies of Eddies in the Marginal Ice Zone Along the East Greenland Current Using Spaceborne Synthetic Aperture Radar (SAR)
title_sort studies of eddies in the marginal ice zone along the east greenland current using spaceborne synthetic aperture radar (sar)
publisher The University of Bergen
publishDate 2011
url https://hdl.handle.net/1956/5113
long_lat ENVELOPE(134.033,134.033,68.667,68.667)
geographic Asar
Greenland
geographic_facet Asar
Greenland
genre East Greenland
east greenland current
Greenland
Sea ice
genre_facet East Greenland
east greenland current
Greenland
Sea ice
op_relation https://hdl.handle.net/1956/5113
op_rights Copyright the author. All rights reserved
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