Submesoscale Air‐Sea Interactions as Revealed by SWOT

Abstract At midlatitudes, air‐sea interactions have been documented in numerical models, in situ campaigns and satellite observations down to the ocean mesoscales. However little is known about scales of a few kilometers (the submesoscales). The new satellite mission Surface Water and Ocean Topography (SWOT) provides a global coverage of these scales by measuring sea surface height. Through the radar backscatter coefficient, it also provides surface wind speed at the same resolution. Here, we examine situations in the Gulf Stream and Kuroshio Extension regions where SWOT as well as scatterometer winds and sea surface temperature (SST) at kilometer scale were available. A good correspondence between winds from SWOT and scatterometer is found at the mesoscales. More importantly, the signature of SST anomalies is found in SWOT winds down to 10 km scales, confirming the effect of the ocean on the atmosphere at those scales. SWOT therefore opens new opportunities for the study of submesoscale air‐sea interactions from space.

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Publication Details

Journal
Geophysical Research Letters
Published
2025-10-21
DOI
https://doi.org/10.1029/2025gl116017
Citations
2
Primary Topic
Oceanographic and Atmospheric Processes
Type
article
Field-Weighted Citation Impact
3.59
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article

Submesoscale Air‐Sea Interactions as Revealed by SWOT

Mohamed Kaouah, Céline Dablemont, Guillaume Lapeyre, Lionel Renault et al.
2 citations
Geophysical Research Letters
Oceanographic and Atmospheric Processes
3.59
article

Submesoscale Air‐Sea Interactions as Revealed by SWOT

Mohamed Kaouah, Céline Dablemont, Guillaume Lapeyre, Lionel Renault, Xavier Perrot
article en
2 citations

Abstract

Abstract At midlatitudes, air‐sea interactions have been documented in numerical models, in situ campaigns and satellite observations down to the ocean mesoscales. However little is known about scales of a few kilometers (the submesoscales). The new satellite mission Surface Water and Ocean Topography (SWOT) provides a global coverage of these scales by measuring sea surface height. Through the radar backscatter coefficient, it also provides surface wind speed at the same resolution. Here, we examine situations in the Gulf Stream and Kuroshio Extension regions where SWOT as well as scatterometer winds and sea surface temperature (SST) at kilometer scale were available. A good correspondence between winds from SWOT and scatterometer is found at the mesoscales. More importantly, the signature of SST anomalies is found in SWOT winds down to 10 km scales, confirming the effect of the ocean on the atmosphere at those scales. SWOT therefore opens new opportunities for the study of submesoscale air‐sea interactions from space.

Geophysical Research LettersVol. 52(20)
Centre National de la Recherche Scientifique (FR), Université Toulouse III - Paul Sabatier (FR), Université Fédérale de Toulouse Midi-Pyrénées (FR), Université Paris Sciences et Lettres (FR), École Normale Supérieure - PSL (FR), Sorbonne Université (FR), Laboratoire d’Études en Géophysique et Océanographie Spatiales (FR), Institut des Sciences Moléculaires d'Orsay (FR), Institut de Recherche pour le Développement (FR)
Openalex Percentile: Top 7%
Oceanographic and Atmospheric Processes
3.59
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