Assessing the role and consistency of satellite observation products in global physical–biogeochemical ocean reanalysis

<p>As part of the European Space Agency's Climate Change Initiative, new sets of satellite observation products have been produced for essential climate variables including ocean colour, sea surface temperature, sea level, and sea ice. These new products have been assimilated into a globa...

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Main Author: D. A. Ford
Format: Article
Language:English
Published: Copernicus Publications 2020-07-01
Series:Ocean Science
Online Access:https://os.copernicus.org/articles/16/875/2020/os-16-875-2020.pdf
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spelling doaj-31a58d7ce9e047ca8c3f8d682911b0812020-11-25T02:58:11ZengCopernicus PublicationsOcean Science1812-07841812-07922020-07-011687589310.5194/os-16-875-2020Assessing the role and consistency of satellite observation products in global physical–biogeochemical ocean reanalysisD. A. Ford<p>As part of the European Space Agency's Climate Change Initiative, new sets of satellite observation products have been produced for essential climate variables including ocean colour, sea surface temperature, sea level, and sea ice. These new products have been assimilated into a global physical–biogeochemical ocean model to create a set of 13-year reanalyses at 1<span class="inline-formula"><sup>∘</sup></span> resolution and 3-year reanalyses at <span class="inline-formula">1∕4</span><span class="inline-formula"><sup>∘</sup></span> resolution. In a series of experiments, the variables were assimilated individually and in combination in order to assess their consistency from a data assimilation perspective. The satellite products, and the reanalyses assimilating them, were found to be consistent in their representation of spatial features such as fronts, sea ice extent, and bloom activity. Assimilating multiple variables together often resulted in larger mean increments for a variable than assimilating it individually, providing information about model biases and compensating errors which could be addressed in the future development of the model and assimilation scheme. Sea surface fugacity of carbon dioxide had lower errors against independent observations in the higher-resolution simulations and was improved by assimilating ocean colour or sea ice concentration, but it was degraded by assimilating sea surface temperature or sea level anomaly. Phytoplankton biomass correlated more strongly with net air–sea heat fluxes in the reanalyses than chlorophyll concentration did, and the correlation was weakened by assimilating ocean colour data, suggesting that studies of phytoplankton bloom initiation based solely on chlorophyll data may not provide a full understanding of the underlying processes.</p>https://os.copernicus.org/articles/16/875/2020/os-16-875-2020.pdf
collection DOAJ
language English
format Article
sources DOAJ
author D. A. Ford
spellingShingle D. A. Ford
Assessing the role and consistency of satellite observation products in global physical–biogeochemical ocean reanalysis
Ocean Science
author_facet D. A. Ford
author_sort D. A. Ford
title Assessing the role and consistency of satellite observation products in global physical–biogeochemical ocean reanalysis
title_short Assessing the role and consistency of satellite observation products in global physical–biogeochemical ocean reanalysis
title_full Assessing the role and consistency of satellite observation products in global physical–biogeochemical ocean reanalysis
title_fullStr Assessing the role and consistency of satellite observation products in global physical–biogeochemical ocean reanalysis
title_full_unstemmed Assessing the role and consistency of satellite observation products in global physical–biogeochemical ocean reanalysis
title_sort assessing the role and consistency of satellite observation products in global physical–biogeochemical ocean reanalysis
publisher Copernicus Publications
series Ocean Science
issn 1812-0784
1812-0792
publishDate 2020-07-01
description <p>As part of the European Space Agency's Climate Change Initiative, new sets of satellite observation products have been produced for essential climate variables including ocean colour, sea surface temperature, sea level, and sea ice. These new products have been assimilated into a global physical–biogeochemical ocean model to create a set of 13-year reanalyses at 1<span class="inline-formula"><sup>∘</sup></span> resolution and 3-year reanalyses at <span class="inline-formula">1∕4</span><span class="inline-formula"><sup>∘</sup></span> resolution. In a series of experiments, the variables were assimilated individually and in combination in order to assess their consistency from a data assimilation perspective. The satellite products, and the reanalyses assimilating them, were found to be consistent in their representation of spatial features such as fronts, sea ice extent, and bloom activity. Assimilating multiple variables together often resulted in larger mean increments for a variable than assimilating it individually, providing information about model biases and compensating errors which could be addressed in the future development of the model and assimilation scheme. Sea surface fugacity of carbon dioxide had lower errors against independent observations in the higher-resolution simulations and was improved by assimilating ocean colour or sea ice concentration, but it was degraded by assimilating sea surface temperature or sea level anomaly. Phytoplankton biomass correlated more strongly with net air–sea heat fluxes in the reanalyses than chlorophyll concentration did, and the correlation was weakened by assimilating ocean colour data, suggesting that studies of phytoplankton bloom initiation based solely on chlorophyll data may not provide a full understanding of the underlying processes.</p>
url https://os.copernicus.org/articles/16/875/2020/os-16-875-2020.pdf
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