On the Theory of the Equilibrium Range in the Spectrum of Wind-Generated Gravity WavesSource: Journal of Physical Oceanography:;1983:;Volume( 013 ):;issue: 005::page 816Author:Kitaigorodskii, S. A.
DOI: 10.1175/1520-0485(1983)013<0816:OTTOTE>2.0.CO;2Publisher: American Meteorological Society
Abstract: It is shown that an exact analog of Kolmogoroff's spectrum in a random field of weekly nonlinear surface gravity waves gives a spectral form for frequency spectra S(?) ? ??4 in close agreement with the results of recent observational studies. The proposed theory also indicates the existence of a ?transitional? range of wavenumbers (frequencies) where the deviation from Kolmogoroff's equilibrium is due to gravitational instability (wave breaking). Because of this it is suggested dot the equilibrium form for the spectrum of wind-generated waves has two asymptotic regimes: Kolmogoroff's and Philips' type of equilibrium with a relatively rapid transition from the first to the second. The experiments data favor such an interpretation.
|
Collections
Show full item record
contributor author | Kitaigorodskii, S. A. | |
date accessioned | 2017-06-09T14:46:34Z | |
date available | 2017-06-09T14:46:34Z | |
date copyright | 1983/05/01 | |
date issued | 1983 | |
identifier issn | 0022-3670 | |
identifier other | ams-26507.pdf | |
identifier uri | http://onlinelibrary.yabesh.ir/handle/yetl/4163409 | |
description abstract | It is shown that an exact analog of Kolmogoroff's spectrum in a random field of weekly nonlinear surface gravity waves gives a spectral form for frequency spectra S(?) ? ??4 in close agreement with the results of recent observational studies. The proposed theory also indicates the existence of a ?transitional? range of wavenumbers (frequencies) where the deviation from Kolmogoroff's equilibrium is due to gravitational instability (wave breaking). Because of this it is suggested dot the equilibrium form for the spectrum of wind-generated waves has two asymptotic regimes: Kolmogoroff's and Philips' type of equilibrium with a relatively rapid transition from the first to the second. The experiments data favor such an interpretation. | |
publisher | American Meteorological Society | |
title | On the Theory of the Equilibrium Range in the Spectrum of Wind-Generated Gravity Waves | |
type | Journal Paper | |
journal volume | 13 | |
journal issue | 5 | |
journal title | Journal of Physical Oceanography | |
identifier doi | 10.1175/1520-0485(1983)013<0816:OTTOTE>2.0.CO;2 | |
journal fristpage | 816 | |
journal lastpage | 827 | |
tree | Journal of Physical Oceanography:;1983:;Volume( 013 ):;issue: 005 | |
contenttype | Fulltext |