Ocean eddy signature on SAR‐derived sea ice drift and vorticity

In the Arctic Ocean, the observation of mesoscale eddies is impeded by the presence of sea ice. To address this problem, we develop a new method of ocean eddy detection based on their signature in sea ice vorticity retrieved from Synthetic Aperture Radar (SAR) images. We examine the case of one eddy...

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Published in:Geophysical Research Letters
Main Authors: Cassianides, Angelina, Lique, Camille, Korosov, Anton
Format: Text
Language:English
Published: American Geophysical Union
Subjects:
geo
Online Access:https://doi.org/10.1029/2020GL092066
https://archimer.ifremer.fr/doc/00679/79137/81640.pdf
https://archimer.ifremer.fr/doc/00679/79137/
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spelling fttriple:oai:gotriple.eu:10670/1.rqo4ks 2023-05-15T14:29:17+02:00 Ocean eddy signature on SAR‐derived sea ice drift and vorticity Cassianides, Angelina Lique, Camille Korosov, Anton https://doi.org/10.1029/2020GL092066 https://archimer.ifremer.fr/doc/00679/79137/81640.pdf https://archimer.ifremer.fr/doc/00679/79137/ en eng American Geophysical Union doi:10.1029/2020GL092066 10670/1.rqo4ks https://archimer.ifremer.fr/doc/00679/79137/81640.pdf https://archimer.ifremer.fr/doc/00679/79137/ Archimer, archive institutionnelle de l'Ifremer Geophysical Research Letters (0094-8276) (American Geophysical Union), 2021-03 , Vol. 48 , N. 6 , P. e2020GL092066 (9p.) envir geo Text https://vocabularies.coar-repositories.org/resource_types/c_18cf/ fttriple https://doi.org/10.1029/2020GL092066 2023-01-22T17:43:55Z In the Arctic Ocean, the observation of mesoscale eddies is impeded by the presence of sea ice. To address this problem, we develop a new method of ocean eddy detection based on their signature in sea ice vorticity retrieved from Synthetic Aperture Radar (SAR) images. We examine the case of one eddy in October 2017 in the marginal ice zone of the Canadian Basin, which was sampled by mooring observations. Although the eddy could not be identified by visual inspection of the SAR images, its signature is revealed as a dipole anomaly in sea ice vorticity, which suggests that the eddy is a dipole composed of a cyclone and an anticyclone, with a horizontal scale of 80‐100 km and persisted over a week. The robustness of our method will allow us to detect more eddies as more SAR observations become available in the future. Plain Language Summary Mesoscale eddies are routinely observed by satellites in the ocean. Yet, in the ice‐covered Arctic Basin, the presence of sea ice makes it challenging to characterise the eddy field. Here, we present a detection method of surface ocean eddies based on their signature in the displacement of sea ice, using high spatial resolution satellite images. A dipole composed of a cyclonic and an anticyclonic eddy is identified over a week in mid‐October 2017 with a horizontal scale of 80‐100 km. Its presence is confirmed by high values of ocean speed in the surface layer during the same period. This work demonstrates that processing are required for identifying the signature of eddies in sea ice, which is not always obvious at first sight. Text Arctic Basin Arctic Arctic Ocean Sea ice Unknown Arctic Arctic Ocean Geophysical Research Letters 48 6
institution Open Polar
collection Unknown
op_collection_id fttriple
language English
topic envir
geo
spellingShingle envir
geo
Cassianides, Angelina
Lique, Camille
Korosov, Anton
Ocean eddy signature on SAR‐derived sea ice drift and vorticity
topic_facet envir
geo
description In the Arctic Ocean, the observation of mesoscale eddies is impeded by the presence of sea ice. To address this problem, we develop a new method of ocean eddy detection based on their signature in sea ice vorticity retrieved from Synthetic Aperture Radar (SAR) images. We examine the case of one eddy in October 2017 in the marginal ice zone of the Canadian Basin, which was sampled by mooring observations. Although the eddy could not be identified by visual inspection of the SAR images, its signature is revealed as a dipole anomaly in sea ice vorticity, which suggests that the eddy is a dipole composed of a cyclone and an anticyclone, with a horizontal scale of 80‐100 km and persisted over a week. The robustness of our method will allow us to detect more eddies as more SAR observations become available in the future. Plain Language Summary Mesoscale eddies are routinely observed by satellites in the ocean. Yet, in the ice‐covered Arctic Basin, the presence of sea ice makes it challenging to characterise the eddy field. Here, we present a detection method of surface ocean eddies based on their signature in the displacement of sea ice, using high spatial resolution satellite images. A dipole composed of a cyclonic and an anticyclonic eddy is identified over a week in mid‐October 2017 with a horizontal scale of 80‐100 km. Its presence is confirmed by high values of ocean speed in the surface layer during the same period. This work demonstrates that processing are required for identifying the signature of eddies in sea ice, which is not always obvious at first sight.
format Text
author Cassianides, Angelina
Lique, Camille
Korosov, Anton
author_facet Cassianides, Angelina
Lique, Camille
Korosov, Anton
author_sort Cassianides, Angelina
title Ocean eddy signature on SAR‐derived sea ice drift and vorticity
title_short Ocean eddy signature on SAR‐derived sea ice drift and vorticity
title_full Ocean eddy signature on SAR‐derived sea ice drift and vorticity
title_fullStr Ocean eddy signature on SAR‐derived sea ice drift and vorticity
title_full_unstemmed Ocean eddy signature on SAR‐derived sea ice drift and vorticity
title_sort ocean eddy signature on sar‐derived sea ice drift and vorticity
publisher American Geophysical Union
url https://doi.org/10.1029/2020GL092066
https://archimer.ifremer.fr/doc/00679/79137/81640.pdf
https://archimer.ifremer.fr/doc/00679/79137/
geographic Arctic
Arctic Ocean
geographic_facet Arctic
Arctic Ocean
genre Arctic Basin
Arctic
Arctic Ocean
Sea ice
genre_facet Arctic Basin
Arctic
Arctic Ocean
Sea ice
op_source Archimer, archive institutionnelle de l'Ifremer
Geophysical Research Letters (0094-8276) (American Geophysical Union), 2021-03 , Vol. 48 , N. 6 , P. e2020GL092066 (9p.)
op_relation doi:10.1029/2020GL092066
10670/1.rqo4ks
https://archimer.ifremer.fr/doc/00679/79137/81640.pdf
https://archimer.ifremer.fr/doc/00679/79137/
op_doi https://doi.org/10.1029/2020GL092066
container_title Geophysical Research Letters
container_volume 48
container_issue 6
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