Preprints
https://doi.org/10.5194/essd-2025-510
https://doi.org/10.5194/essd-2025-510
09 Sep 2025
 | 09 Sep 2025
Status: this preprint is currently under review for the journal ESSD.

Long-Wavelength Steric Sea Level and Heat Storage Anomaly Maps by Combining Argo Temperature and Salinity Profiles with Satellite Altimetry and Gravimetry

Don P. Chambers and Sara J. Reinelt

Abstract. Argo profiles of temperature/salinity (T/S) at specific times and locations from January 2003 through December 2023 are mapped into monthly maps of steric sea level (SSL), thermosteric sea level (TSL), and Ocean Heat Content (OHC) anomalies at long wavelengths. The mapping uses a monthly satellite reference computed from the difference between satellite altimetry and gravimetry, so that in periods where there is not sufficient global Argo coverage (generally before 2007), the satellite estimate is used instead of a mean climatology. Longwave mapping is done to reduce large errors introduced by poor sampling of mesoscale eddies by the Argo floats. We demonstrate that on global- and basin-scales, the longwave mapping does not substantially affect calculations of mean SSL, TSL, or OHC changes. Monthly standard error maps from the mapping are also provided. These maps are intended for users interested in understanding global- and basin-scale sea level budgets, as well as understanding changes in ocean heat uptake.

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Don P. Chambers and Sara J. Reinelt

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Don P. Chambers and Sara J. Reinelt

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Steric Sea Level and Heat Storage Anomalies from Argo Profiles and Satellite Altimetry and Gravimetry Don P. Chambers and Sara J. Reinelt https://doi.org/10.17632/dsjkkhvywr.1

Don P. Chambers and Sara J. Reinelt

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Short summary
Monthly maps of steric sea level, thermometric sea level, and ocean heat content anomalies from January 2003 through December 2023 are described. The maps were created from a statistical combination of satellite altimetry, satellite gravimetry, and in situ Argo profiles of temperature/salinity to 2000 m depth. Data are mapped at long wavelengths to reduce contamination from mesoscale eddies. The data are intended for the study of sea level budgets and changes in ocean heat uptake.
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