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    Marginal Ice Zone Thickness and Extent due to Wave Radiation Stress 

    Source: Journal of Physical Oceanography:;2018:;volume 048:;issue 008:;page 1885
    Author(s): Sutherland, Peter; Dumont, Dany
    Publisher: American Meteorological Society
    Abstract: AbstractOcean surface wave radiation stress represents the flux of momentum due to the waves. When waves are dissipated or reflected by sea ice, that momentum is absorbed or reflected, resulting in a horizontal forcing ...
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    Field Measurements of Surface and Near-Surface Turbulence in the Presence of Breaking Waves 

    Source: Journal of Physical Oceanography:;2015:;Volume( 045 ):;issue: 004:;page 943
    Author(s): Sutherland, Peter; Melville, W. Kendall
    Publisher: American Meteorological Society
    Abstract: ave breaking removes energy from the surface wave field and injects it into the upper ocean, where it is dissipated by viscosity. This paper presents an investigation of turbulent kinetic energy (TKE) dissipation beneath ...
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    Measuring Turbulent Kinetic Energy Dissipation at a Wavy Sea Surface 

    Source: Journal of Atmospheric and Oceanic Technology:;2015:;volume( 032 ):;issue: 008:;page 1498
    Author(s): Sutherland, Peter; Melville, W. Kendall
    Publisher: American Meteorological Society
    Abstract: ave breaking is thought to be the dominant mechanism for energy loss by the surface wave field. Breaking results in energetic and highly turbulent velocity fields, concentrated within approximately one wave height of the ...
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