Anomalously fresh Chukchi Sea surface salinity in summer-autumn 2021
International audience The Chukchi Sea is a marginal sea in the Arctic with a mixed layer that is a few psu units saltier than ambient open Arctic water. Such higher salinity is maintained by salty and warm Pacific water inflow through the Bering Strait, implying that changes in inflow characteristi...
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ftinsu:oai:HAL:hal-04203959v1 2024-04-14T08:07:08+00:00 Anomalously fresh Chukchi Sea surface salinity in summer-autumn 2021 Grodsky, Semyon A. Reul, Nicolas Bentamy, Abderrahim Vandemark, Douglas Laboratoire d'Océanographie Physique et Spatiale (LOPS) Institut de Recherche pour le Développement (IRD)-Institut Français de Recherche pour l'Exploitation de la Mer (IFREMER)-Institut national des sciences de l'Univers (INSU - CNRS)-Université de Brest (UBO)-Centre National de la Recherche Scientifique (CNRS) 2023-02 https://hal.science/hal-04203959 https://doi.org/10.1080/2150704X.2022.2164231 en eng HAL CCSD Taylor and Francis info:eu-repo/semantics/altIdentifier/doi/10.1080/2150704X.2022.2164231 hal-04203959 https://hal.science/hal-04203959 doi:10.1080/2150704X.2022.2164231 ISSN: 2150-704X EISSN: 2150-7058 Remote Sensing Letters https://hal.science/hal-04203959 Remote Sensing Letters, 2023, 14 (2), pp.135-147. ⟨10.1080/2150704X.2022.2164231⟩ [SDU]Sciences of the Universe [physics] info:eu-repo/semantics/article Journal articles 2023 ftinsu https://doi.org/10.1080/2150704X.2022.2164231 2024-03-21T17:06:29Z International audience The Chukchi Sea is a marginal sea in the Arctic with a mixed layer that is a few psu units saltier than ambient open Arctic water. Such higher salinity is maintained by salty and warm Pacific water inflow through the Bering Strait, implying that changes in inflow characteristics should affect the thermohaline properties of the Chukchi Sea. Recently, two additional controlling factors have been highlighted – the strength of boundary currents along the Siberian coast, and meridional exchanges due to wind-driven transport. In this note, we illustrate that anomalous fresh Chukchi Sea surface salinity in summer-autumn 2021 may be related to the anomalous southward shift of the ice edge and its meltwater source. These anomalous ice conditions occur concurrently with anomalously low Beaufort High, anomalous westerly cyclonic winds over ice-covered and open water Chukchi Sea, and related southward Ekman transport of late season meltwater. The September 2021 ice expansion was the largest in 1981–2021 detrended ice records. Article in Journal/Newspaper Arctic Bering Strait Chukchi Chukchi Sea Institut national des sciences de l'Univers: HAL-INSU Arctic Bering Strait Chukchi Sea Pacific Remote Sensing Letters 14 2 135 147 |
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Open Polar |
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Institut national des sciences de l'Univers: HAL-INSU |
op_collection_id |
ftinsu |
language |
English |
topic |
[SDU]Sciences of the Universe [physics] |
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[SDU]Sciences of the Universe [physics] Grodsky, Semyon A. Reul, Nicolas Bentamy, Abderrahim Vandemark, Douglas Anomalously fresh Chukchi Sea surface salinity in summer-autumn 2021 |
topic_facet |
[SDU]Sciences of the Universe [physics] |
description |
International audience The Chukchi Sea is a marginal sea in the Arctic with a mixed layer that is a few psu units saltier than ambient open Arctic water. Such higher salinity is maintained by salty and warm Pacific water inflow through the Bering Strait, implying that changes in inflow characteristics should affect the thermohaline properties of the Chukchi Sea. Recently, two additional controlling factors have been highlighted – the strength of boundary currents along the Siberian coast, and meridional exchanges due to wind-driven transport. In this note, we illustrate that anomalous fresh Chukchi Sea surface salinity in summer-autumn 2021 may be related to the anomalous southward shift of the ice edge and its meltwater source. These anomalous ice conditions occur concurrently with anomalously low Beaufort High, anomalous westerly cyclonic winds over ice-covered and open water Chukchi Sea, and related southward Ekman transport of late season meltwater. The September 2021 ice expansion was the largest in 1981–2021 detrended ice records. |
author2 |
Laboratoire d'Océanographie Physique et Spatiale (LOPS) Institut de Recherche pour le Développement (IRD)-Institut Français de Recherche pour l'Exploitation de la Mer (IFREMER)-Institut national des sciences de l'Univers (INSU - CNRS)-Université de Brest (UBO)-Centre National de la Recherche Scientifique (CNRS) |
format |
Article in Journal/Newspaper |
author |
Grodsky, Semyon A. Reul, Nicolas Bentamy, Abderrahim Vandemark, Douglas |
author_facet |
Grodsky, Semyon A. Reul, Nicolas Bentamy, Abderrahim Vandemark, Douglas |
author_sort |
Grodsky, Semyon A. |
title |
Anomalously fresh Chukchi Sea surface salinity in summer-autumn 2021 |
title_short |
Anomalously fresh Chukchi Sea surface salinity in summer-autumn 2021 |
title_full |
Anomalously fresh Chukchi Sea surface salinity in summer-autumn 2021 |
title_fullStr |
Anomalously fresh Chukchi Sea surface salinity in summer-autumn 2021 |
title_full_unstemmed |
Anomalously fresh Chukchi Sea surface salinity in summer-autumn 2021 |
title_sort |
anomalously fresh chukchi sea surface salinity in summer-autumn 2021 |
publisher |
HAL CCSD |
publishDate |
2023 |
url |
https://hal.science/hal-04203959 https://doi.org/10.1080/2150704X.2022.2164231 |
geographic |
Arctic Bering Strait Chukchi Sea Pacific |
geographic_facet |
Arctic Bering Strait Chukchi Sea Pacific |
genre |
Arctic Bering Strait Chukchi Chukchi Sea |
genre_facet |
Arctic Bering Strait Chukchi Chukchi Sea |
op_source |
ISSN: 2150-704X EISSN: 2150-7058 Remote Sensing Letters https://hal.science/hal-04203959 Remote Sensing Letters, 2023, 14 (2), pp.135-147. ⟨10.1080/2150704X.2022.2164231⟩ |
op_relation |
info:eu-repo/semantics/altIdentifier/doi/10.1080/2150704X.2022.2164231 hal-04203959 https://hal.science/hal-04203959 doi:10.1080/2150704X.2022.2164231 |
op_doi |
https://doi.org/10.1080/2150704X.2022.2164231 |
container_title |
Remote Sensing Letters |
container_volume |
14 |
container_issue |
2 |
container_start_page |
135 |
op_container_end_page |
147 |
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1796304407211540480 |