Comments on “Estimates of Kinetic Energy Dissipation under Breaking Waves”

Gerrit Burgers Oceanographic Research Division, KNMI, De Bilt, the Netherlands

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Abstract

It is noted that the results of recent experiments on the enhancement of turbulent kinetic energy (TKE) dissipation below surface waves can be stated as follows. TKE dissipation is enhanced by a factor 15Hws/z at depths 0.5Hws < z < 20Hws with respect to the wall-layer result ϵ = u3w/κz, where uw is the friction velocity in water and Hws is the significant windsea wave height. For open ocean conditions, this reduces in most cases to an enhancement factor 106u2w/gzu210/gz.

Corresponding author address: Dr. Gerrit Burgers, Oceanographic Research Division, KNMI, P.O. Box 201, 3730 AE De Bilt, the Netherlands.

Abstract

It is noted that the results of recent experiments on the enhancement of turbulent kinetic energy (TKE) dissipation below surface waves can be stated as follows. TKE dissipation is enhanced by a factor 15Hws/z at depths 0.5Hws < z < 20Hws with respect to the wall-layer result ϵ = u3w/κz, where uw is the friction velocity in water and Hws is the significant windsea wave height. For open ocean conditions, this reduces in most cases to an enhancement factor 106u2w/gzu210/gz.

Corresponding author address: Dr. Gerrit Burgers, Oceanographic Research Division, KNMI, P.O. Box 201, 3730 AE De Bilt, the Netherlands.

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  • Agrawal, Y. C., E. A. Terray, M. A. Donelan, P. A. Hwang, A. J. Williams III, W. M. Drennan, K. K. Kahma, and S. A. Kitaigorodskii, 1992: Enhanced dissipation of kinetic energy beneath surface waves. Nature,359, 219–220.

  • Drennan, W. M., M. A. Donelan, E. A. Terray, and K. B. Katsaros, 1996: Oceanic turbulence dissipation measurements in SWADE. J. Phys. Oceanogr.,26, 808–815.

  • Terray, E. A., M. A. Donelan, Y. C. Agrawal, W. M. Drennan, K. K. Kahma, A. J. Williams III, P. A. Hwang, and S. A. Kitaigorodskii, 1996: Estimates of kinetic energy dissipation under breaking waves. J. Phys. Oceanogr.,26, 792–807.

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