Short-Time Ice Drift and Deformation Measurements Using Multi-Mission Synethetic Aperture Radar

Norway is in a good position regarding frequent access to synthetic aperture radar data. A Norwegian– Canadian agreement provides large quotas of RADARSAT-2 images used operationally by e.g. the Norwegian Ice Service. More recently, Norway’s participation in the Copernicus program also allows rapid...

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Main Authors: Kræmer, Thomas, Brekke, Camilla
Format: Article in Journal/Newspaper
Language:English
Published: 2015
Subjects:
Online Access:https://hdl.handle.net/10037/8443
id ftunivtroemsoe:oai:munin.uit.no:10037/8443
record_format openpolar
spelling ftunivtroemsoe:oai:munin.uit.no:10037/8443 2023-05-15T14:23:51+02:00 Short-Time Ice Drift and Deformation Measurements Using Multi-Mission Synethetic Aperture Radar Kræmer, Thomas Brekke, Camilla 2015-06 https://hdl.handle.net/10037/8443 eng eng Norges forskningsråd: 195143 Proceedings of the 23rd International Conference on Port and Ocean Engineering under Arctic Conditions June 14-18, 2015 Trondheim, Norway FRIDAID 1243238 2077-7841 https://hdl.handle.net/10037/8443 URN:NBN:no-uit_munin_8022 openAccess VDP::Matematikk og Naturvitenskap: 400::Fysikk: 430 VDP::Mathematics and natural science: 400::Physics: 430 Journal article Tidsskriftartikkel 2015 ftunivtroemsoe 2021-06-25T17:54:34Z Norway is in a good position regarding frequent access to synthetic aperture radar data. A Norwegian– Canadian agreement provides large quotas of RADARSAT-2 images used operationally by e.g. the Norwegian Ice Service. More recently, Norway’s participation in the Copernicus program also allows rapid access to SENTINEL-1A data. By combining these data sources we can get satellite time series with very low time separation which allows us to study ice drift, deformation and ice growth processes with a time resolution of minutes and hours rather than days. This allows us to measure the drift of fast moving ice which is usually not observable due to insufficient time sampling. We study ice drift derived using varying time separations ranging from minutes to one day and show the effect on estimated ice speeds. The derived drift is used to construct deformation maps showing areas of converging and diverging ice. We show that very high time resolution is sometimes necessary for measuring fast moving ice. We focus on a particular example that illustrates how low time sampling implies missing significant changes in deformation within one day Article in Journal/Newspaper Arctic University of Tromsø: Munin Open Research Archive Norway
institution Open Polar
collection University of Tromsø: Munin Open Research Archive
op_collection_id ftunivtroemsoe
language English
topic VDP::Matematikk og Naturvitenskap: 400::Fysikk: 430
VDP::Mathematics and natural science: 400::Physics: 430
spellingShingle VDP::Matematikk og Naturvitenskap: 400::Fysikk: 430
VDP::Mathematics and natural science: 400::Physics: 430
Kræmer, Thomas
Brekke, Camilla
Short-Time Ice Drift and Deformation Measurements Using Multi-Mission Synethetic Aperture Radar
topic_facet VDP::Matematikk og Naturvitenskap: 400::Fysikk: 430
VDP::Mathematics and natural science: 400::Physics: 430
description Norway is in a good position regarding frequent access to synthetic aperture radar data. A Norwegian– Canadian agreement provides large quotas of RADARSAT-2 images used operationally by e.g. the Norwegian Ice Service. More recently, Norway’s participation in the Copernicus program also allows rapid access to SENTINEL-1A data. By combining these data sources we can get satellite time series with very low time separation which allows us to study ice drift, deformation and ice growth processes with a time resolution of minutes and hours rather than days. This allows us to measure the drift of fast moving ice which is usually not observable due to insufficient time sampling. We study ice drift derived using varying time separations ranging from minutes to one day and show the effect on estimated ice speeds. The derived drift is used to construct deformation maps showing areas of converging and diverging ice. We show that very high time resolution is sometimes necessary for measuring fast moving ice. We focus on a particular example that illustrates how low time sampling implies missing significant changes in deformation within one day
format Article in Journal/Newspaper
author Kræmer, Thomas
Brekke, Camilla
author_facet Kræmer, Thomas
Brekke, Camilla
author_sort Kræmer, Thomas
title Short-Time Ice Drift and Deformation Measurements Using Multi-Mission Synethetic Aperture Radar
title_short Short-Time Ice Drift and Deformation Measurements Using Multi-Mission Synethetic Aperture Radar
title_full Short-Time Ice Drift and Deformation Measurements Using Multi-Mission Synethetic Aperture Radar
title_fullStr Short-Time Ice Drift and Deformation Measurements Using Multi-Mission Synethetic Aperture Radar
title_full_unstemmed Short-Time Ice Drift and Deformation Measurements Using Multi-Mission Synethetic Aperture Radar
title_sort short-time ice drift and deformation measurements using multi-mission synethetic aperture radar
publishDate 2015
url https://hdl.handle.net/10037/8443
geographic Norway
geographic_facet Norway
genre Arctic
genre_facet Arctic
op_relation Norges forskningsråd: 195143
Proceedings of the 23rd International Conference on Port and Ocean Engineering under Arctic Conditions June 14-18, 2015 Trondheim, Norway
FRIDAID 1243238
2077-7841
https://hdl.handle.net/10037/8443
URN:NBN:no-uit_munin_8022
op_rights openAccess
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