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    Alternative Interpretations for Microstructure Patches in the Thermocline 

    Source: Journal of Physical Oceanography:;1982:;Volume( 012 ):;issue: 004:;page 374
    Author(s): Gibson, Carl H.
    Publisher: American Meteorological Society
    Abstract: Two interpretations of microstructure patches measured in the main thermocline of the North Pacific by Gregg (1980) are questioned. He concludes that the observed microstructure is not fossil-temperature turbulence and ...
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    Direct Measurements of Turbulence in the Pacific Equatorial Undercurrent 

    Source: Journal of Physical Oceanography:;1974:;Volume( 004 ):;issue: 001:;page 104
    Author(s): Williams, Robert B.; Gibson, Carl H.
    Publisher: American Meteorological Society
    Abstract: Measurements of small-scale fluctuations of temperature are used to estimate turbulent parameters such as viscous dissipation rate (?), dissipation rate of temperature variance (?), and turbulent diffusion coefficients of ...
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    Sampling Turbulence in the Stratified Ocean: Statistical Consequences of Strong Intermittency 

    Source: Journal of Physical Oceanography:;1987:;Volume( 017 ):;issue: 010:;page 1817
    Author(s): Baker, Mark A.; Gibson, Carl H.
    Publisher: American Meteorological Society
    Abstract: Turbulence and turbulent mixing in the ocean are strongly intermittent in amplitude, space and time. The degree of intermittency is measured by the ?intermittency factor? σ2, defined as either σ2ln?, the variance of the ...
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    Structure of Marine Surface Layer Turbulence 

    Source: Journal of the Atmospheric Sciences:;1979:;Volume( 036 ):;issue: 004:;page 602
    Author(s): Schmitt, Kurt F.; Friehe, Carl A.; Gibson, Carl H.
    Publisher: American Meteorological Society
    Abstract: Measurements of turbulent wind velocity, humidity and temperature spectra for stable and unstable stratification in the atmospheric surface layer obtained during an experiment over the North Pacific Ocean are presented. ...
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