Large-scale sea ice motion from Sentinel-1 and the RADARSAT Constellation Mission

As Arctic sea ice extent continues to decline, remote sensing observations are becoming even more vital for the monitoring and understanding of sea ice. Recently, the sea ice community has entered a new era of synthetic aperture radar (SAR) satellites operating at C-band with the launch of Sentinel-...

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Main Authors: Howell, Stephen E. L., Brady, Mike, Komarov, Alexander S.
Format: Text
Language:English
Published: 2021
Subjects:
Online Access:https://doi.org/10.5194/tc-2021-223
https://tc.copernicus.org/preprints/tc-2021-223/
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spelling ftcopernicus:oai:publications.copernicus.org:tcd96396 2023-05-15T14:46:10+02:00 Large-scale sea ice motion from Sentinel-1 and the RADARSAT Constellation Mission Howell, Stephen E. L. Brady, Mike Komarov, Alexander S. 2021-07-22 application/pdf https://doi.org/10.5194/tc-2021-223 https://tc.copernicus.org/preprints/tc-2021-223/ eng eng doi:10.5194/tc-2021-223 https://tc.copernicus.org/preprints/tc-2021-223/ eISSN: 1994-0424 Text 2021 ftcopernicus https://doi.org/10.5194/tc-2021-223 2021-07-26T16:22:27Z As Arctic sea ice extent continues to decline, remote sensing observations are becoming even more vital for the monitoring and understanding of sea ice. Recently, the sea ice community has entered a new era of synthetic aperture radar (SAR) satellites operating at C-band with the launch of Sentinel-1A in 2014, Sentinel-1B in 2016 and the RADARSAT Constellation Mission (RCM) in 2019. These missions represent 5 spaceborne SAR sensors, that together routinely cover the pan-Arctic sea ice domain. Here, we utilized over 60,000 SAR images from Sentinel-1AB (S1) and RCM to generate large-scale sea ice motion (SIM) estimates over the pan-Arctic domain from March to December, 2020. On average, 4.5 million SIM vectors from S1 and RCM were automatically detected per week for 2020 and when combined (S1+RCM) they facilitated the generation of 7-day, 25 km SIM products across the pan-Arctic domain. S1+RCM SIM provided more coverage in Hudson Bay, Davis Strait, Beaufort Sea, Bering Sea, and over the North Pole compared to SIM from S1 alone. S1+RCM SIM was able to be resolved within the narrow channels and inlets across the pan-Arctic alleviating the main limitation of coarser resolution sensors. S1+RCM SIM provided larger ice speeds with a mean difference (MD) of 1.3 km/day compared to the National Snow and Ice Data Center (NSIDC) SIM product and a MD of 0.76 km/day compared to Ocean and Sea Ice-Satellite Application Facility (OSI-SAF) SIM product. S1+RCM was also able to better resolve SIM in the marginal ice zone compared to the NSIDC and OSA-SAF SIM products. Overall, our results demonstrate that combining SIM from multiple spaceborne SAR satellites allows for large-scale SIM to be routinely generated across the pan-Arctic domain. Text Arctic Beaufort Sea Bering Sea Davis Strait Hudson Bay National Snow and Ice Data Center North Pole Sea ice Copernicus Publications: E-Journals Arctic Bering Sea Hudson Hudson Bay North Pole
institution Open Polar
collection Copernicus Publications: E-Journals
op_collection_id ftcopernicus
language English
description As Arctic sea ice extent continues to decline, remote sensing observations are becoming even more vital for the monitoring and understanding of sea ice. Recently, the sea ice community has entered a new era of synthetic aperture radar (SAR) satellites operating at C-band with the launch of Sentinel-1A in 2014, Sentinel-1B in 2016 and the RADARSAT Constellation Mission (RCM) in 2019. These missions represent 5 spaceborne SAR sensors, that together routinely cover the pan-Arctic sea ice domain. Here, we utilized over 60,000 SAR images from Sentinel-1AB (S1) and RCM to generate large-scale sea ice motion (SIM) estimates over the pan-Arctic domain from March to December, 2020. On average, 4.5 million SIM vectors from S1 and RCM were automatically detected per week for 2020 and when combined (S1+RCM) they facilitated the generation of 7-day, 25 km SIM products across the pan-Arctic domain. S1+RCM SIM provided more coverage in Hudson Bay, Davis Strait, Beaufort Sea, Bering Sea, and over the North Pole compared to SIM from S1 alone. S1+RCM SIM was able to be resolved within the narrow channels and inlets across the pan-Arctic alleviating the main limitation of coarser resolution sensors. S1+RCM SIM provided larger ice speeds with a mean difference (MD) of 1.3 km/day compared to the National Snow and Ice Data Center (NSIDC) SIM product and a MD of 0.76 km/day compared to Ocean and Sea Ice-Satellite Application Facility (OSI-SAF) SIM product. S1+RCM was also able to better resolve SIM in the marginal ice zone compared to the NSIDC and OSA-SAF SIM products. Overall, our results demonstrate that combining SIM from multiple spaceborne SAR satellites allows for large-scale SIM to be routinely generated across the pan-Arctic domain.
format Text
author Howell, Stephen E. L.
Brady, Mike
Komarov, Alexander S.
spellingShingle Howell, Stephen E. L.
Brady, Mike
Komarov, Alexander S.
Large-scale sea ice motion from Sentinel-1 and the RADARSAT Constellation Mission
author_facet Howell, Stephen E. L.
Brady, Mike
Komarov, Alexander S.
author_sort Howell, Stephen E. L.
title Large-scale sea ice motion from Sentinel-1 and the RADARSAT Constellation Mission
title_short Large-scale sea ice motion from Sentinel-1 and the RADARSAT Constellation Mission
title_full Large-scale sea ice motion from Sentinel-1 and the RADARSAT Constellation Mission
title_fullStr Large-scale sea ice motion from Sentinel-1 and the RADARSAT Constellation Mission
title_full_unstemmed Large-scale sea ice motion from Sentinel-1 and the RADARSAT Constellation Mission
title_sort large-scale sea ice motion from sentinel-1 and the radarsat constellation mission
publishDate 2021
url https://doi.org/10.5194/tc-2021-223
https://tc.copernicus.org/preprints/tc-2021-223/
geographic Arctic
Bering Sea
Hudson
Hudson Bay
North Pole
geographic_facet Arctic
Bering Sea
Hudson
Hudson Bay
North Pole
genre Arctic
Beaufort Sea
Bering Sea
Davis Strait
Hudson Bay
National Snow and Ice Data Center
North Pole
Sea ice
genre_facet Arctic
Beaufort Sea
Bering Sea
Davis Strait
Hudson Bay
National Snow and Ice Data Center
North Pole
Sea ice
op_source eISSN: 1994-0424
op_relation doi:10.5194/tc-2021-223
https://tc.copernicus.org/preprints/tc-2021-223/
op_doi https://doi.org/10.5194/tc-2021-223
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