A theory for the evolution of wind-generated gravity-wave spectra due to dissipation

DOI10.1080/03091928108208774zbMath0468.76022OpenAlexW1995163239WikidataQ114640770 ScholiaQ114640770MaRDI QIDQ3922365

H. Naeser

Publication date: 1981

Published in: Geophysical & Astrophysical Fluid Dynamics (Search for Journal in Brave)

Full work available at URL: https://doi.org/10.1080/03091928108208774

zbMATH Keywords

nonlinear interactionsocean wave spectrawind generated wavesroles of dissipation

Mathematics Subject Classification ID

Hydrology, hydrography, oceanography (86A05) Water waves, gravity waves; dispersion and scattering, nonlinear interaction (76B15)

Cites Work

• Why ripples become sweiis, and swells in shallow water decay rapidly
• Spin and angular momentum in gravity waves
• A new model for nonlinear wind waves. Part 1. Physical model and experimental evidence
• The disintegration of wave trains on deep water Part 1. Theory

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