Properties of surface water masses in the Laptev and the East Siberian seas in summer 2018 from in situ and satellite data
Variability of surface water masses of the Laptev and the East Siberian seas in August–September 2018 is studied using in situ and satellite data. In situ data were collected during the ARKTIKA-2018 expedition and then complemented with satellite-derived sea surface temperature (SST), salinity (SSS)...
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Copernicus GmbH
2021
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Online Access: | https://archimer.ifremer.fr/doc/00678/79015/81413.pdf https://archimer.ifremer.fr/doc/00678/79015/81415.pdf https://doi.org/10.5194/os-17-221-2021 https://archimer.ifremer.fr/doc/00678/79015/ |
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ftarchimer:oai:archimer.ifremer.fr:79015 2023-05-15T15:24:29+02:00 Properties of surface water masses in the Laptev and the East Siberian seas in summer 2018 from in situ and satellite data Tarasenko, Anastasiia Supply, Alexandre Kusse-tiuz, Nikita Ivanov, Vladimir Makhotin, Mikhail Tournadre, Jean Chapron, Bertrand Boutin, Jacqueline Kolodziejczyk, Nicolas Reverdin, Gilles 2021-02 application/pdf https://archimer.ifremer.fr/doc/00678/79015/81413.pdf https://archimer.ifremer.fr/doc/00678/79015/81415.pdf https://doi.org/10.5194/os-17-221-2021 https://archimer.ifremer.fr/doc/00678/79015/ eng eng Copernicus GmbH https://archimer.ifremer.fr/doc/00678/79015/81413.pdf https://archimer.ifremer.fr/doc/00678/79015/81415.pdf doi:10.5194/os-17-221-2021 https://archimer.ifremer.fr/doc/00678/79015/ info:eu-repo/semantics/openAccess restricted use Ocean Science (1812-0784) (Copernicus GmbH), 2021-02 , Vol. 17 , N. 1 , P. 221-247 text Publication info:eu-repo/semantics/article 2021 ftarchimer https://doi.org/10.5194/os-17-221-2021 2021-09-23T20:36:55Z Variability of surface water masses of the Laptev and the East Siberian seas in August–September 2018 is studied using in situ and satellite data. In situ data were collected during the ARKTIKA-2018 expedition and then complemented with satellite-derived sea surface temperature (SST), salinity (SSS), sea surface height, wind speed, and sea ice concentration. The estimation of SSS fields is challenging in high-latitude regions, and the precision of soil moisture and ocean salinity (SMOS) SSS retrieval is improved by applying a threshold on SSS weekly error. For the first time in this region, the validity of DMI (Danish Meteorological Institute) SST and SMOS SSS products is thoroughly studied using ARKTIKA-2018 expedition continuous thermosalinograph measurements and conductivity–temperature–depth (CTD) casts. They are found to be adequate to describe large surface gradients in this region. Surface gradients and mixing of the river and the sea water in the ice-free and ice-covered areas are described with a special attention to the marginal ice zone at a synoptic scale. We suggest that the freshwater is pushed northward, close to the marginal ice zone (MIZ) and under the sea ice, which is confirmed by the oxygen isotope analysis. The SST-SSS diagram based on satellite estimates shows the possibility of investigating the surface water mass transformation at a synoptic scale and reveals the presence of river water on the shelf of the East Siberian Sea. The Ekman transport is calculated to better understand the pathway of surface water displacement on the shelf and beyond. Article in Journal/Newspaper arktika East Siberian Sea laptev Sea ice ice covered areas Archimer (Archive Institutionnelle de l'Ifremer - Institut français de recherche pour l'exploitation de la mer) East Siberian Sea ENVELOPE(166.000,166.000,74.000,74.000) Ocean Science 17 1 221 247 |
institution |
Open Polar |
collection |
Archimer (Archive Institutionnelle de l'Ifremer - Institut français de recherche pour l'exploitation de la mer) |
op_collection_id |
ftarchimer |
language |
English |
description |
Variability of surface water masses of the Laptev and the East Siberian seas in August–September 2018 is studied using in situ and satellite data. In situ data were collected during the ARKTIKA-2018 expedition and then complemented with satellite-derived sea surface temperature (SST), salinity (SSS), sea surface height, wind speed, and sea ice concentration. The estimation of SSS fields is challenging in high-latitude regions, and the precision of soil moisture and ocean salinity (SMOS) SSS retrieval is improved by applying a threshold on SSS weekly error. For the first time in this region, the validity of DMI (Danish Meteorological Institute) SST and SMOS SSS products is thoroughly studied using ARKTIKA-2018 expedition continuous thermosalinograph measurements and conductivity–temperature–depth (CTD) casts. They are found to be adequate to describe large surface gradients in this region. Surface gradients and mixing of the river and the sea water in the ice-free and ice-covered areas are described with a special attention to the marginal ice zone at a synoptic scale. We suggest that the freshwater is pushed northward, close to the marginal ice zone (MIZ) and under the sea ice, which is confirmed by the oxygen isotope analysis. The SST-SSS diagram based on satellite estimates shows the possibility of investigating the surface water mass transformation at a synoptic scale and reveals the presence of river water on the shelf of the East Siberian Sea. The Ekman transport is calculated to better understand the pathway of surface water displacement on the shelf and beyond. |
format |
Article in Journal/Newspaper |
author |
Tarasenko, Anastasiia Supply, Alexandre Kusse-tiuz, Nikita Ivanov, Vladimir Makhotin, Mikhail Tournadre, Jean Chapron, Bertrand Boutin, Jacqueline Kolodziejczyk, Nicolas Reverdin, Gilles |
spellingShingle |
Tarasenko, Anastasiia Supply, Alexandre Kusse-tiuz, Nikita Ivanov, Vladimir Makhotin, Mikhail Tournadre, Jean Chapron, Bertrand Boutin, Jacqueline Kolodziejczyk, Nicolas Reverdin, Gilles Properties of surface water masses in the Laptev and the East Siberian seas in summer 2018 from in situ and satellite data |
author_facet |
Tarasenko, Anastasiia Supply, Alexandre Kusse-tiuz, Nikita Ivanov, Vladimir Makhotin, Mikhail Tournadre, Jean Chapron, Bertrand Boutin, Jacqueline Kolodziejczyk, Nicolas Reverdin, Gilles |
author_sort |
Tarasenko, Anastasiia |
title |
Properties of surface water masses in the Laptev and the East Siberian seas in summer 2018 from in situ and satellite data |
title_short |
Properties of surface water masses in the Laptev and the East Siberian seas in summer 2018 from in situ and satellite data |
title_full |
Properties of surface water masses in the Laptev and the East Siberian seas in summer 2018 from in situ and satellite data |
title_fullStr |
Properties of surface water masses in the Laptev and the East Siberian seas in summer 2018 from in situ and satellite data |
title_full_unstemmed |
Properties of surface water masses in the Laptev and the East Siberian seas in summer 2018 from in situ and satellite data |
title_sort |
properties of surface water masses in the laptev and the east siberian seas in summer 2018 from in situ and satellite data |
publisher |
Copernicus GmbH |
publishDate |
2021 |
url |
https://archimer.ifremer.fr/doc/00678/79015/81413.pdf https://archimer.ifremer.fr/doc/00678/79015/81415.pdf https://doi.org/10.5194/os-17-221-2021 https://archimer.ifremer.fr/doc/00678/79015/ |
long_lat |
ENVELOPE(166.000,166.000,74.000,74.000) |
geographic |
East Siberian Sea |
geographic_facet |
East Siberian Sea |
genre |
arktika East Siberian Sea laptev Sea ice ice covered areas |
genre_facet |
arktika East Siberian Sea laptev Sea ice ice covered areas |
op_source |
Ocean Science (1812-0784) (Copernicus GmbH), 2021-02 , Vol. 17 , N. 1 , P. 221-247 |
op_relation |
https://archimer.ifremer.fr/doc/00678/79015/81413.pdf https://archimer.ifremer.fr/doc/00678/79015/81415.pdf doi:10.5194/os-17-221-2021 https://archimer.ifremer.fr/doc/00678/79015/ |
op_rights |
info:eu-repo/semantics/openAccess restricted use |
op_doi |
https://doi.org/10.5194/os-17-221-2021 |
container_title |
Ocean Science |
container_volume |
17 |
container_issue |
1 |
container_start_page |
221 |
op_container_end_page |
247 |
_version_ |
1766355136852000768 |