The Impact of Surfactants on the Airflow Above Wind Waves

Abstract We investigate phase‐dependent features of the airflow above wind waves on slick‐free and slick‐covered water surfaces and relate them to small‐scale wave structures. Three surfactants with different viscoelastic properties were deployed in a wind‐wave tank, with wind speeds between and . In slick‐free conditions, the airflow exhibits pronounced phase‐locked asymmetries, including reduced wind speeds extending from the leeward side of wave crests across the troughs. Small‐scale roughness patterns, likely associated with capillary waves trailing the crests, modulate the airflow in subsequent wave phases. In contrast, surfactants suppress high‐frequency slope roughness, resulting in increased shear near the surface under nearly all conditions, suggesting a more closely attached boundary layer. Strength and persistence of these effects vary with surfactant type and wind speed, influencing both wave growth and air–sea momentum exchange.

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Publication Details

Journal
Geophysical Research Letters
Published
2026-07-16
DOI
https://doi.org/10.1029/2025gl118527
Primary Topic
Ocean Waves and Remote Sensing
Type
article
Field-Weighted Citation Impact
0.00

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article

The Impact of Surfactants on the Airflow Above Wind Waves

Martin Gade, K. Schultz, M. P. Buckley
Geophysical Research Letters
Ocean Waves and Remote Sensing
article

The Impact of Surfactants on the Airflow Above Wind Waves

Martin Gade, K. Schultz, M. P. Buckley
article en

Abstract

Abstract We investigate phase‐dependent features of the airflow above wind waves on slick‐free and slick‐covered water surfaces and relate them to small‐scale wave structures. Three surfactants with different viscoelastic properties were deployed in a wind‐wave tank, with wind speeds between and . In slick‐free conditions, the airflow exhibits pronounced phase‐locked asymmetries, including reduced wind speeds extending from the leeward side of wave crests across the troughs. Small‐scale roughness patterns, likely associated with capillary waves trailing the crests, modulate the airflow in subsequent wave phases. In contrast, surfactants suppress high‐frequency slope roughness, resulting in increased shear near the surface under nearly all conditions, suggesting a more closely attached boundary layer. Strength and persistence of these effects vary with surfactant type and wind speed, influencing both wave growth and air–sea momentum exchange.

Geophysical Research LettersVol. 53(14)
Universität Hamburg (DE), Hamburg Institut (Germany) (DE), Helmholtz-Zentrum Hereon (DE)
Deutsche Forschungsgemeinschaft
Life below water
Openalex Percentile: Top 11%
Ocean Waves and Remote Sensing
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The Impact of Surfactants on the Airflow Above Wind Waves — Martin Gade, K. Schultz, et al. · Geophysical Research Letters (2026) | TGRS Research Map | TGRS