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    The Formation of Parasitic Capillary Ripples on Gravity–Capillary Waves and the Underlying Vortical Structures 

    Source: Journal of Physical Oceanography:;2009:;Volume( 039 ):;issue: 002:;page 263
    Author(s): Hung, Li-Ping; Tsai, Wu-Ting
    Publisher: American Meteorological Society
    Abstract: The evolution of moderately short, steep two-dimensional gravity?capillary waves, from the onset of the parasitic capillary ripples to a fully developed quasi-steady stage, is studied numerically using a spectrally accurate ...
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    Enhanced Energy Dissipation by Parasitic Capillaries on Short Gravity–Capillary Waves 

    Source: Journal of Physical Oceanography:;2010:;Volume( 040 ):;issue: 011:;page 2435
    Author(s): Tsai, Wu-ting; Hung, Li-ping
    Publisher: American Meteorological Society
    Abstract: The increased energy dissipation caused by the formation of parasitic capillary wavelets on moderately short, steep gravity?capillary waves is studied numerically. This study focuses on understanding the mechanism leading ...
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    Numerical Evidence of Turbulence Generated by Nonbreaking Surface Waves 

    Source: Journal of Physical Oceanography:;2014:;Volume( 045 ):;issue: 001:;page 174
    Author(s): Tsai, Wu-ting; Chen, Shi-ming; Lu, Guan-hung
    Publisher: American Meteorological Society
    Abstract: umerical simulation of monochromatic surface waves propagating over a turbulent field is conducted to reveal the mechanism of turbulence production by nonbreaking waves. The numerical model solves the primitive equations ...
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    On the Formation of Coherent Vortices beneath Nonbreaking Free-Propagating Surface Waves 

    Source: Journal of Physical Oceanography:;2017:;Volume( 047 ):;issue: 003:;page 533
    Author(s): Tsai, Wu-ting; Lu, Guan-hung; Chen, Jheng-rong; Dai, Albert; Phillips, William R. C.
    Publisher: American Meteorological Society
    Abstract: umerical simulations of monochromatic surface waves freely propagating over an initially quiescent flow field are conducted and found to reveal an array of quasi-streamwise vortices of alternating orientation in a manner ...
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