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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Main Authors: Xie, Jiping, Raj, Roshin P., Bertino, Laurent, Martínez, Justino, Gabarró, Carolina, Catany, Rafael
Format: Article in Journal/Newspaper
Language:English
Published: Copernicus Publications 2022
Subjects:
Online Access:https://doi.org/10.5194/egusphere-2022-660
https://noa.gwlb.de/receive/cop_mods_00061926
https://egusphere.copernicus.org/preprints/egusphere-2022-660/egusphere-2022-660.pdf
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author Xie, Jiping
Raj, Roshin P.
Bertino, Laurent
Martínez, Justino
Gabarró, Carolina
Catany, Rafael
author_facet Xie, Jiping
Raj, Roshin P.
Bertino, Laurent
Martínez, Justino
Gabarró, Carolina
Catany, Rafael
author_sort Xie, Jiping
collection Niedersächsisches Online-Archiv NOA
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 propose 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 Ensemble Kalman filter from July to December 2016, two assimilation runs 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 areas and put the latest product to its advantage. The time series of Freshwater Content (FWC) further show that its seasonal cycle can be adjusted by assimilation of the SSS products, which is encouraging for its use in a long-time reanalysis to monitor 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 ftnonlinearchiv:oai:noa.gwlb.de:cop_mods_00061926 2025-01-16T20:05:25+00:00 Assimilation of sea surface salinities from SMOS in an Arctic coupled ocean and sea ice reanalysis Xie, Jiping Raj, Roshin P. Bertino, Laurent Martínez, Justino Gabarró, Carolina Catany, Rafael 2022-07 electronic https://doi.org/10.5194/egusphere-2022-660 https://noa.gwlb.de/receive/cop_mods_00061926 https://egusphere.copernicus.org/preprints/egusphere-2022-660/egusphere-2022-660.pdf eng eng Copernicus Publications https://doi.org/10.5194/egusphere-2022-660 https://noa.gwlb.de/receive/cop_mods_00061926 https://egusphere.copernicus.org/preprints/egusphere-2022-660/egusphere-2022-660.pdf https://creativecommons.org/licenses/by/4.0/ uneingeschränkt info:eu-repo/semantics/restrictedAccess CC-BY article Verlagsveröffentlichung article Text doc-type:article 2022 ftnonlinearchiv https://doi.org/10.5194/egusphere-2022-660 2022-07-31T23:11:44Z 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 propose 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 Ensemble Kalman filter from July to December 2016, two assimilation runs 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 areas and put the latest product to its advantage. The time series of Freshwater Content (FWC) further show that its seasonal cycle can be adjusted by assimilation of the SSS products, which is encouraging for its use in a long-time reanalysis to monitor the Arctic water cycle. Article in Journal/Newspaper Arctic Arctic Ocean Sea ice Niedersächsisches Online-Archiv NOA Arctic Arctic Ocean
spellingShingle article
Verlagsveröffentlichung
Xie, Jiping
Raj, Roshin P.
Bertino, Laurent
Martínez, Justino
Gabarró, Carolina
Catany, Rafael
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 article
Verlagsveröffentlichung
topic_facet article
Verlagsveröffentlichung
url https://doi.org/10.5194/egusphere-2022-660
https://noa.gwlb.de/receive/cop_mods_00061926
https://egusphere.copernicus.org/preprints/egusphere-2022-660/egusphere-2022-660.pdf