SODA4: a mesoscale ocean/sea ice reanalysis 1980-2024

Fuente: arXiv
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Main Authors: Chepurin, Gennady A., Carton, James A., Sun, Luyu, Penny, Stephen G.
Format: Preprint
Published: 2025
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author Chepurin, Gennady A.
Carton, James A.
Sun, Luyu
Penny, Stephen G.
author_facet Chepurin, Gennady A.
Carton, James A.
Sun, Luyu
Penny, Stephen G.
contents This paper describes the new Simple Ocean Data Assimilation version 4 (SODA4) global eddy-resolving ocean/sea ice reanalysis that spans the 45-year period 1980-2024. The reanalysis is constructed using GFDL MOM5/SIS1 numerics and ECMWF ERA5 forcings with surface and subsurface temperature and salinity observations as constraints within an optimal interpolation data assimilation algorithm. The method of construction and resulting output files are described. Comparison of the SODA4 temperature and salinity fields to observations and to the UK Met Office EN4 temperature and salinity analyses in the upper ocean shows SODA4 has marginal bias and exhibits more regional variability, with less of an imprint of the sparse and inhomogeneous distribution of observations. Comparison of transports across major ocean sections and passages are generally consistent with independent moored observations.
format Preprint
id arxiv_https___arxiv_org_abs_2508_17462
institution arXiv
publishDate 2025
record_format arxiv
spellingShingle SODA4: a mesoscale ocean/sea ice reanalysis 1980-2024
Chepurin, Gennady A.
Carton, James A.
Sun, Luyu
Penny, Stephen G.
Atmospheric and Oceanic Physics
This paper describes the new Simple Ocean Data Assimilation version 4 (SODA4) global eddy-resolving ocean/sea ice reanalysis that spans the 45-year period 1980-2024. The reanalysis is constructed using GFDL MOM5/SIS1 numerics and ECMWF ERA5 forcings with surface and subsurface temperature and salinity observations as constraints within an optimal interpolation data assimilation algorithm. The method of construction and resulting output files are described. Comparison of the SODA4 temperature and salinity fields to observations and to the UK Met Office EN4 temperature and salinity analyses in the upper ocean shows SODA4 has marginal bias and exhibits more regional variability, with less of an imprint of the sparse and inhomogeneous distribution of observations. Comparison of transports across major ocean sections and passages are generally consistent with independent moored observations.
title SODA4: a mesoscale ocean/sea ice reanalysis 1980-2024
topic Atmospheric and Oceanic Physics
url https://arxiv.org/abs/2508.17462