Phase‐Resolved Swells Across Ocean Basins in SWOT Altimetry Data: Revealing Centimeter‐Scale Wave Heights Including Coastal Reflection

Author:

Ardhuin Fabrice1ORCID,Molero Beatriz2,Bohé Alejandro3,Nouguier Frédéric1ORCID,Collard Fabrice4,Houghton Isabel5ORCID,Hay Andrea67ORCID,Legresy Benoit678ORCID

Affiliation:

1. Laboratoire d’Océanographie Physique et Spatiale (LOPS) Univ. Brest CNRS IRD Ifremer IUEM Brest France

2. CLS Ramonville St Agne France

3. CNES Toulouse France

4. ODL Locmaria‐Plouzane France

5. Sofar Ocean Technologies San Francisco CA USA

6. School of Geography, Planning, and Spatial Sciences University of Tasmania Hobart TAS Australia

7. Commonwealth Scientific and Industrial Research Organisation Hobart TAS Australia

8. Integrated Marine Observing System Hobart TAS Australia

Abstract

AbstractSevere storms produce ocean waves with periods of 18–26 s, corresponding to wavelengths 500–1,055 m. These waves radiate globally as swell, generating microseisms and affecting coastal areas. Despite their significance, long waves often elude detection by existing remote sensing systems when their height is below 0.2 m. The new Surface Water Ocean Topography (SWOT) satellite offers a breakthrough by resolving these waves in global sea level measurements. Here we show that SWOT can detect 25‐s waves with heights as low as 3 cm, and resolves period and direction better than in situ buoys. SWOT provides detailed maps of wave height, wavelength, and direction across ocean basins. These measurements unveil intricate spatial patterns, shedding light on wave generation in storms, currents that influence propagation, and refraction, diffraction and reflection in shallow regions. Notably, the magnitude of reflections exceeds previous expectations, illustrating SWOT's transformative impact.

Funder

European Space Agency

Centre National d’Etudes Spatiales

Publisher

American Geophysical Union (AGU)

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