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    On the Fluid Dynamical Theory of Turbulent Gas Transfer Across an Air-Sea Interface in the Presence of Breaking Wind-Waves 

    Source: Journal of Physical Oceanography:;1984:;Volume( 014 ):;issue: 005:;page 960
    Author(s): Kitaigorodskii, S. A.
    Publisher: American Meteorological Society
    Abstract: It is shown that in order to describe the transfer of gases in the liquid near the air-sea interface, the vertical structure of three-dimensional small-scale turbulence in turbulent patches generated by breaking waves must ...
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    On the Theory of the Equilibrium Range in the Spectrum of Wind-Generated Gravity Waves 

    Source: Journal of Physical Oceanography:;1983:;Volume( 013 ):;issue: 005:;page 816
    Author(s): Kitaigorodskii, S. A.
    Publisher: 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 ...
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    Wave-Turbulence interactions in the Upper Ocean. Part I: The Energy Balance of the Interacting Fields of Surface Wind Waves and Wind-Induced Three-Dimensional Turbulence 

    Source: Journal of Physical Oceanography:;1983:;Volume( 013 ):;issue: 011:;page 1977
    Author(s): Kitaigorodskii, S. A.; Lumley, J. L.
    Publisher: American Meteorological Society
    Abstract: We analyze in detail the budget of total and fluctuating energy in the surface layer of the ocean. We suggest a rational scheme for separating the budget of turbulence from that of random wind-generated surface waves, and ...
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    The Dissipation Range of Wind-Wave Spectra Observed on a Lake 

    Source: Journal of Physical Oceanography:;1990:;Volume( 020 ):;issue: 009:;page 1264
    Author(s): Hansen, C.; Katsaros, K. B.; Kitaigorodskii, S. A.; Larsen, S. E.
    Publisher: American Meteorological Society
    Abstract: Based on an interpretation of a field experiment it is argued that, due to breaking of wind waves in deep water, the dissipation of energy is restricted to a range of frequencies ? > ?g, much higher than the frequency ?m ...
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    Wave-Turbulence Interactions in the Upper Ocean. Part II. Statistical Characteristics of Wave and Turbulent Components of the Random Velocity Field in the Marine Surface Layer 

    Source: Journal of Physical Oceanography:;1983:;Volume( 013 ):;issue: 011:;page 1988
    Author(s): Kitaigorodskii, S. A.; Donelan, M. A.; Lumley, J. L.; Terray, E. A.
    Publisher: American Meteorological Society
    Abstract: We present the results of an analysis of field data collected by Donelan who used a miniature drag sphere to measure velocities beneath wind waves on Lake Ontario. Linear statistical techniques are used to separate the ...
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    Estimates of Kinetic Energy Dissipation under Breaking Waves 

    Source: Journal of Physical Oceanography:;1996:;Volume( 026 ):;issue: 005:;page 792
    Author(s): Terray, E.A.; Donelan, M.A.; Agrawal, Y.C.; Drennan, W.M.; Kahma, K.K.; Williams, A.J.; Hwang, P.A.; Kitaigorodskii, S.A.
    Publisher: American Meteorological Society
    Abstract: The dissipation of kinetic energy at the surface of natural water bodies has important consequences for many Physical and biochemical processes including wave dynamics, gas transfer, mixing of nutrients and pollutants, and ...
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    Reply 

    Source: Journal of Physical Oceanography:;1997:;Volume( 027 ):;issue: 010:;page 2308
    Author(s): Terray, E. A.; Donelan, M. A.; Agrawal, Y. C.; Drennan, W. M.; Kahma, K. K.; Williams, A. J.; Hwang, P. A.; Kitaigorodskii, S. A.
    Publisher: American Meteorological Society
    Abstract: No abstract available
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