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    Turbulence Process Domination under the Combined Forcings of Wind Stress, the Langmuir Vortex Force, and Surface Cooling 

    Source: Journal of Physical Oceanography:;2013:;Volume( 044 ):;issue: 001:;page 44
    Author(s): Gargett, A. E.; Grosch, C. E.
    Publisher: American Meteorological Society
    Abstract: urbulence in the ocean surface layer is generated by time-varying combinations of destabilizing surface buoyancy flux, wind stress forcing, and wave forcing through a vortex force associated with the surface wave field. ...
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    Why Do LES of Langmuir Supercells Not Include Rotation? 

    Source: Journal of Physical Oceanography:;2016:;Volume( 046 ):;issue: 012:;page 3595
    Author(s): Grosch, C. E.; Gargett, A. E.
    Publisher: American Meteorological Society
    Abstract: xisting large-eddy simulations (LES) of Langmuir supercells (LS) do not include rotational terms. Despite the fact that the actual coastal ocean is certainly affected by rotation, such simulations are found to provide ...
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    Reconstructing Basin-Scale Eulerian Velocity Fields from Simulated Drifter Data 

    Source: Journal of Physical Oceanography:;2001:;Volume( 031 ):;issue: 005:;page 1361
    Author(s): Toner, M.; Kirwan, A. D.; Lipphardt, B. L.; Poje, A. C.; Jones, C. K. R. T.; Grosch, C. E.
    Publisher: American Meteorological Society
    Abstract: A single-layer, reduced-gravity, double-gyre primitive equation model in a 2000 km ? 2000 km square domain is used to test the accuracy and sensitivity of time-dependent Eulerian velocity fields reconstructed from numerically ...
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    DSpace software copyright © 2002-2015  DuraSpace
    نرم افزار کتابخانه دیجیتال "دی اسپیس" فارسی شده توسط یابش برای کتابخانه های ایرانی | تماس با یابش
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