Abstract
Breaking waves dissipate energy in the oceanic surface layer (top few meters) and also support the air-sea momentum flux. Spectrally resolved energy dissipation and momentum flux are extracted from open ocean observations of the breaking crest length distribution Λ(c). This concept, first introduced by Duncan and Phillips more than 2 decades ago, includes an unknown proportionality factor b. Independent estimates of direct turbulence measurements are used to evaluate this proportionality factor.
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Gemmrich, J. (2007). Momentum Flux and Energy Dissipation Associated with Breaking Waves. In: Garbe, C.S., Handler, R.A., Jähne, B. (eds) Transport at the Air-Sea Interface. Environmental Science and Engineering. Springer, Berlin, Heidelberg. https://doi.org/10.1007/978-3-540-36906-6_9
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DOI: https://doi.org/10.1007/978-3-540-36906-6_9
Publisher Name: Springer, Berlin, Heidelberg
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