Abstract
The amplitude dependences of the growth rate of water waves generated by turbulent wind are theoretically investigated within the framework of a quasilinear approximation.
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References
A. L. Fabrikant,Wave Motion,2, 355 (1980).
D. V. Chalikov,Boundary Layer Meteorology,34, 63 (1986).
M. A. Al-Zanaidi and W. H. Hui,J. Fluid Mech.,148, 225 (1984).
A. D. Jenkins,J. Phys. Oceanorg.,22, No. 8, 843 (1992).
J. W. Miles,J. Fluid Mech.,13, pt. 3, 433 (1962).
A. V. Smol'yakov,Akust. Zh.,19, No. 3, 420 (1973).
O. M. Phillips,Dynamics of the Upper Ocean [Russian translation], Gidrometeoizdat, Leningrad (1980).
V. A. Krasil'nikov and V. I. Pavlov,Byull. Mosk. Gos. Univ., Ser. Fiz. Astron.,13, No. 1, 94 (1972).
Additional information
Institute of Applied Physics, Russian Academy of Sciences, Nizhny Novgorod. Translated from Izvestiya Vysshikh Uchebnykh Zavedenii, Radiofizika, Vol. 38, Nos. 3–4, pp. 206–210, March–April, 1995.
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Reutov, V.P., Troitskaya, Y.I. Nonlinear growth rate of wind water waves and their excitation near the stability threshold. Radiophys Quantum Electron 38, 133–136 (1995). https://doi.org/10.1007/BF01037885
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DOI: https://doi.org/10.1007/BF01037885