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    Stochastic Form of the Growth of Wind Waves in a Single-Parameter Representation with Physical Implications

    Source: Journal of Physical Oceanography:;1978:;Volume( 008 ):;issue: 003::page 494
    Author:
    Toba, Yoshiaki
    DOI: 10.1175/1520-0485(1978)008<0494:SFOTGO>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: It is shown that a simple relation, E* = 5.1 ? 10?2 σm*?3 for describing the conditions of growing wind waves, is supported by various available data, where E* = g2E/u*4 is dimensionless energy. σm* = u*σm/g the dimensionless angular frequency at the maximum of the energy spectrum, g the acceleration of gravity and u* the friction velocity of the air. This expression is an alternative form of the relation between dimensionless wave height and period, H* ? T*3/2, which was previously proposed by the author (Toba, 1972) for energy-containing waves, and is extended to individual waves in the wind-wave field in a statistical sense. It is also shown, supported by various data, that the essential part of the one-dimensional energy spectra of growing wind waves should have the form g*u*σ?4 for the high-frequency tail of the frequency spectrum, where g* is g expanded to include the surface tension. This is the form previously proposed by the author (Toba, 1973b) as the one-dimensional spectral form consistent with the above power law relationship, instead of the g2σ?5 form proposed by Phillips (1958). By use of the power-law relationship for E*, it is shown that the proportion of that part of momentum which is retained as wave momentum to the total momentum transferred from the wind to the sea can be expressed by a function of σm*, which has essentially the same physical meaning as C/U, the ratio between the phase velocity of the energy containing wave and the wind speed. The value of the proportion decreases from about 6% in the form of an error function of C/U. A prediction equation for the growth of wind waves by a single-parameter representation is proposed, in which the rate of change of E* is expressed by a formulation including the error function or by a simple stochastic form. The integration of the equation for the case of fetch-limited conditions is in excellent agreement with data compiled by Hasselmann et al. (1973). Reviewing results of recent wind-wave tunnel experiments, emphasis is given on the fact that wind waves are strongly nonlinear phenomena, especially for C/U ? 1. A discussion is presented from this standpoint as to the physical basis for the existence of the simple power law relationship. the spectral form of g*u*σ?4 and the stochastic form of the growth equation, and a systematic derivation of these relationships and equations is attempted.
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      Stochastic Form of the Growth of Wind Waves in a Single-Parameter Representation with Physical Implications

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4162639
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    contributor authorToba, Yoshiaki
    date accessioned2017-06-09T14:44:47Z
    date available2017-06-09T14:44:47Z
    date copyright1978/05/01
    date issued1978
    identifier issn0022-3670
    identifier otherams-25814.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4162639
    description abstractIt is shown that a simple relation, E* = 5.1 ? 10?2 σm*?3 for describing the conditions of growing wind waves, is supported by various available data, where E* = g2E/u*4 is dimensionless energy. σm* = u*σm/g the dimensionless angular frequency at the maximum of the energy spectrum, g the acceleration of gravity and u* the friction velocity of the air. This expression is an alternative form of the relation between dimensionless wave height and period, H* ? T*3/2, which was previously proposed by the author (Toba, 1972) for energy-containing waves, and is extended to individual waves in the wind-wave field in a statistical sense. It is also shown, supported by various data, that the essential part of the one-dimensional energy spectra of growing wind waves should have the form g*u*σ?4 for the high-frequency tail of the frequency spectrum, where g* is g expanded to include the surface tension. This is the form previously proposed by the author (Toba, 1973b) as the one-dimensional spectral form consistent with the above power law relationship, instead of the g2σ?5 form proposed by Phillips (1958). By use of the power-law relationship for E*, it is shown that the proportion of that part of momentum which is retained as wave momentum to the total momentum transferred from the wind to the sea can be expressed by a function of σm*, which has essentially the same physical meaning as C/U, the ratio between the phase velocity of the energy containing wave and the wind speed. The value of the proportion decreases from about 6% in the form of an error function of C/U. A prediction equation for the growth of wind waves by a single-parameter representation is proposed, in which the rate of change of E* is expressed by a formulation including the error function or by a simple stochastic form. The integration of the equation for the case of fetch-limited conditions is in excellent agreement with data compiled by Hasselmann et al. (1973). Reviewing results of recent wind-wave tunnel experiments, emphasis is given on the fact that wind waves are strongly nonlinear phenomena, especially for C/U ? 1. A discussion is presented from this standpoint as to the physical basis for the existence of the simple power law relationship. the spectral form of g*u*σ?4 and the stochastic form of the growth equation, and a systematic derivation of these relationships and equations is attempted.
    publisherAmerican Meteorological Society
    titleStochastic Form of the Growth of Wind Waves in a Single-Parameter Representation with Physical Implications
    typeJournal Paper
    journal volume8
    journal issue3
    journal titleJournal of Physical Oceanography
    identifier doi10.1175/1520-0485(1978)008<0494:SFOTGO>2.0.CO;2
    journal fristpage494
    journal lastpage507
    treeJournal of Physical Oceanography:;1978:;Volume( 008 ):;issue: 003
    contenttypeFulltext
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