Deep Ocean Steric Sea Level Change in the Subtropical Northwest Atlantic Ocean

Abstract The non‐closure of the global sea level budget, detected since 2017, stimulates the need to better understand limitations of satellite altimetry and gravimetry measurements, and breakdown in situ measurement contributions and gaps. Here, temperature and salinity profiles collected in the subtropical Northwest Atlantic Ocean between 2017 and 2022 by Deep Argo floats are used to partition steric sea level variability into contributions as a function of depth. Interannual steric sea level variability near the surface is of the same order of magnitude over the western boundary and abyssal plain, but fluctuations below 2,000 m over the western boundary are seven times larger and seem affected by local wind forcing. This analysis demonstrates how Deep Argo enables new evaluation of regional sea level budgets and comparison to geodetic products. Differences between float measurements and GLORYS12 highlight the need for more deep‐ocean measurements that can be assimilated in the development of ocean reanalysis products.

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Publication Details

Journal
Geophysical Research Letters
Published
2025-08-15
DOI
https://doi.org/10.1029/2024gl114158
Citations
2
Primary Topic
Geology and Paleoclimatology Research
Type
article
Field-Weighted Citation Impact
2.60

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article

Deep Ocean Steric Sea Level Change in the Subtropical Northwest Atlantic Ocean

Robin Fraudeau, Nathalie Zilberman, Jacob M. Steinberg, Michäel Ablain et al.
2 citations
Geophysical Research Letters
Geology and Paleoclimatology Research
2.60
article

Deep Ocean Steric Sea Level Change in the Subtropical Northwest Atlantic Ocean

Robin Fraudeau, Nathalie Zilberman, Jacob M. Steinberg, Michäel Ablain, William Llovel, Benoît Meyssignac
article en
2 citations

Abstract

Abstract The non‐closure of the global sea level budget, detected since 2017, stimulates the need to better understand limitations of satellite altimetry and gravimetry measurements, and breakdown in situ measurement contributions and gaps. Here, temperature and salinity profiles collected in the subtropical Northwest Atlantic Ocean between 2017 and 2022 by Deep Argo floats are used to partition steric sea level variability into contributions as a function of depth. Interannual steric sea level variability near the surface is of the same order of magnitude over the western boundary and abyssal plain, but fluctuations below 2,000 m over the western boundary are seven times larger and seem affected by local wind forcing. This analysis demonstrates how Deep Argo enables new evaluation of regional sea level budgets and comparison to geodetic products. Differences between float measurements and GLORYS12 highlight the need for more deep‐ocean measurements that can be assimilated in the development of ocean reanalysis products.

Geophysical Research LettersVol. 52(16)
Centre National de la Recherche Scientifique (FR), Université Toulouse III - Paul Sabatier (FR), Scripps Institution of Oceanography (US), Ifremer (FR), Université de Bretagne Occidentale (FR), NOAA Geophysical Fluid Dynamics Laboratory (US), Laboratory for Ocean Physics and Satellite Remote Sensing (FR), Institut Universitaire Européen de la Mer (FR), Magellium (France) (FR), Institut de Recherche pour le Développement (FR)
National Science Foundation, European Space Agency, Centre National d’Etudes Spatiales, National Oceanic and Atmospheric Administration, Global Ocean Monitoring and Observing Program
Life below water
Openalex Percentile: Top 10%
Geology and Paleoclimatology Research
2.60
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