Assimilation of sea surface salinities from SMOS in an Arctic coupled ocean and sea ice reanalysis

In the Arctic, the sea surface salinity (SSS) plays a key role in processes related to water mixing and sea ice. However, the lack of salinity observations causes large uncertainties in Arctic Ocean forecasts and reanalysis. Recently the Soil Moisture and Ocean Salinity (SMOS) satellite mission was...

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Published in:Ocean Science
Main Authors: J. Xie, R. P. Raj, L. Bertino, J. Martínez, C. Gabarró, R. Catany
Format: Article in Journal/Newspaper
Language:English
Published: Copernicus Publications 2023
Subjects:
Online Access:https://doi.org/10.5194/os-19-269-2023
https://doaj.org/article/693eaa213dae4a94abde5afd6dfa9ddc
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author J. Xie
R. P. Raj
L. Bertino
J. Martínez
C. Gabarró
R. Catany
author_facet J. Xie
R. P. Raj
L. Bertino
J. Martínez
C. Gabarró
R. Catany
author_sort J. Xie
collection Directory of Open Access Journals: DOAJ Articles
container_issue 2
container_start_page 269
container_title Ocean Science
container_volume 19
description In the Arctic, the sea surface salinity (SSS) plays a key role in processes related to water mixing and sea ice. However, the lack of salinity observations causes large uncertainties in Arctic Ocean forecasts and reanalysis. Recently the Soil Moisture and Ocean Salinity (SMOS) satellite mission was used by the Barcelona Expert Centre to develop an Arctic SSS product. In this study, we evaluate the impact of assimilating this data in a coupled ocean–ice data assimilation system. Using the deterministic ensemble Kalman filter from July to December 2016, two assimilation runs respectively assimilated two successive versions of the SMOS SSS product on top of a pre-existing reanalysis run. The runs were validated against independent in situ salinity profiles in the Arctic. The results show that the biases and the root-mean-squared differences (RMSD) of SSS are reduced by 10 % to 50 % depending on the area and highlight the importance of assimilating satellite salinity data. The time series of freshwater content (FWC) further shows that its seasonal cycle can be adjusted by assimilation of the SSS products, which is encouraging of the assimilation of SSS in a long-time reanalysis to better reproduce the Arctic water cycle.
format Article in Journal/Newspaper
genre Arctic
Arctic Ocean
Sea ice
genre_facet Arctic
Arctic Ocean
Sea ice
geographic Arctic
Arctic Ocean
geographic_facet Arctic
Arctic Ocean
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spelling ftdoajarticles:oai:doaj.org/article:693eaa213dae4a94abde5afd6dfa9ddc 2025-01-16T20:06:29+00:00 Assimilation of sea surface salinities from SMOS in an Arctic coupled ocean and sea ice reanalysis J. Xie R. P. Raj L. Bertino J. Martínez C. Gabarró R. Catany 2023-03-01T00:00:00Z https://doi.org/10.5194/os-19-269-2023 https://doaj.org/article/693eaa213dae4a94abde5afd6dfa9ddc EN eng Copernicus Publications https://os.copernicus.org/articles/19/269/2023/os-19-269-2023.pdf https://doaj.org/toc/1812-0784 https://doaj.org/toc/1812-0792 doi:10.5194/os-19-269-2023 1812-0784 1812-0792 https://doaj.org/article/693eaa213dae4a94abde5afd6dfa9ddc Ocean Science, Vol 19, Pp 269-287 (2023) Geography. Anthropology. Recreation G Environmental sciences GE1-350 article 2023 ftdoajarticles https://doi.org/10.5194/os-19-269-2023 2023-03-12T01:32:09Z In the Arctic, the sea surface salinity (SSS) plays a key role in processes related to water mixing and sea ice. However, the lack of salinity observations causes large uncertainties in Arctic Ocean forecasts and reanalysis. Recently the Soil Moisture and Ocean Salinity (SMOS) satellite mission was used by the Barcelona Expert Centre to develop an Arctic SSS product. In this study, we evaluate the impact of assimilating this data in a coupled ocean–ice data assimilation system. Using the deterministic ensemble Kalman filter from July to December 2016, two assimilation runs respectively assimilated two successive versions of the SMOS SSS product on top of a pre-existing reanalysis run. The runs were validated against independent in situ salinity profiles in the Arctic. The results show that the biases and the root-mean-squared differences (RMSD) of SSS are reduced by 10 % to 50 % depending on the area and highlight the importance of assimilating satellite salinity data. The time series of freshwater content (FWC) further shows that its seasonal cycle can be adjusted by assimilation of the SSS products, which is encouraging of the assimilation of SSS in a long-time reanalysis to better reproduce the Arctic water cycle. Article in Journal/Newspaper Arctic Arctic Ocean Sea ice Directory of Open Access Journals: DOAJ Articles Arctic Arctic Ocean Ocean Science 19 2 269 287
spellingShingle Geography. Anthropology. Recreation
G
Environmental sciences
GE1-350
J. Xie
R. P. Raj
L. Bertino
J. Martínez
C. Gabarró
R. Catany
Assimilation of sea surface salinities from SMOS in an Arctic coupled ocean and sea ice reanalysis
title Assimilation of sea surface salinities from SMOS in an Arctic coupled ocean and sea ice reanalysis
title_full Assimilation of sea surface salinities from SMOS in an Arctic coupled ocean and sea ice reanalysis
title_fullStr Assimilation of sea surface salinities from SMOS in an Arctic coupled ocean and sea ice reanalysis
title_full_unstemmed Assimilation of sea surface salinities from SMOS in an Arctic coupled ocean and sea ice reanalysis
title_short Assimilation of sea surface salinities from SMOS in an Arctic coupled ocean and sea ice reanalysis
title_sort assimilation of sea surface salinities from smos in an arctic coupled ocean and sea ice reanalysis
topic Geography. Anthropology. Recreation
G
Environmental sciences
GE1-350
topic_facet Geography. Anthropology. Recreation
G
Environmental sciences
GE1-350
url https://doi.org/10.5194/os-19-269-2023
https://doaj.org/article/693eaa213dae4a94abde5afd6dfa9ddc