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    Comments on “ A Heat Balance for the Bering Sea Ice Edge” 

    Source: Journal of Physical Oceanography:;1986:;Volume( 016 ):;issue: 012:;page 2205
    Author(s): Kantha, Lakshmi H.
    Publisher: American Meteorological Society
    Abstract: No abstract available.
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    Comments on “Oscillatory Bottom Boundary Layers” 

    Source: Journal of Physical Oceanography:;2005:;Volume( 035 ):;issue: 007:;page 1297
    Author(s): Kantha, Lakshmi H.
    Publisher: American Meteorological Society
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    Comments on “Turbulence Closure, Steady State, and Collapse into Waves” 

    Source: Journal of Physical Oceanography:;2005:;Volume( 035 ):;issue: 001:;page 131
    Author(s): Kantha, Lakshmi H.
    Publisher: American Meteorological Society
    Abstract: Two-equation models are being increasingly used to model turbulence in geophysical flows. A salient aspect of these flows is the stable gravitational stratification, which implies that turbulent fluctuations can generate ...
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    On an Improved Model for the Turbulent PBL 

    Source: Journal of the Atmospheric Sciences:;2003:;Volume( 060 ):;issue: 017:;page 2239
    Author(s): Kantha, Lakshmi H.
    Publisher: American Meteorological Society
    Abstract: Cheng, Canuto, and Howard have presented a second-moment closure PBL model that appears to overcome some of the shortcomings of the existing Mellor and Yamada?type closure models. This note demonstrates that with a slight ...
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    Reply 

    Source: Journal of the Atmospheric Sciences:;2003:;Volume( 060 ):;issue: 024:;page 3047
    Author(s): Kantha, Lakshmi H.
    Publisher: American Meteorological Society
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    A Data-Assimilative Numerical Model of the Northern Indian Ocean 

    Source: Journal of Atmospheric and Oceanic Technology:;2000:;volume( 017 ):;issue: 011:;page 1525
    Author(s): Lopez, Joseph W.; Kantha, Lakshmi H.
    Publisher: American Meteorological Society
    Abstract: A primitive equation, three-dimensional, baroclinic circulation model has been configured for use in the North Indian Ocean. After having been spun up by climatological winds, the model was used to generate a hindcast for ...
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    Turbulent Kinetic Energy and Its Dissipation Rate in the Equatorial Mixed Layer 

    Source: Journal of Physical Oceanography:;1999:;Volume( 029 ):;issue: 009:;page 2146
    Author(s): Clayson, Carol Anne; Kantha, Lakshmi H.
    Publisher: American Meteorological Society
    Abstract: The authors apply a one-dimensional mixed layer model, based on second moment closure of turbulence, to study the characteristics of turbulence in the equatorial mixed layer. In particular, they focus on characteristics ...
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    A Diagnostic Calculation of the General Circulation in the South Atlantic Bight 

    Source: Journal of Physical Oceanography:;1982:;Volume( 012 ):;issue: 008:;page 805
    Author(s): Kantha, Lakshmi H.; Mellor, George L.; Blumberg, Alan F.
    Publisher: American Meteorological Society
    Abstract: A diagnostic calculation that involves integration of the geostrophic equations for total transport along contours of constant planetary potential vorticity (f/H) is described and applied to the South Atlantic Bight. The ...
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    The Behavior of the Bulk – Skin Sea Surface Temperature Difference under Varying Wind Speed and Heat Flux 

    Source: Journal of Physical Oceanography:;1996:;Volume( 026 ):;issue: 010:;page 1969
    Author(s): Wick, Gary A.; Emery, William J.; Kantha, Lakshmi H.; Schlüssel, Peter
    Publisher: American Meteorological Society
    Abstract: The observed and predicted response of the bulk ? skin sea surface temperature difference (δT) to changes in the wind speed and net heat flux is analyzed. Observations of δT from the northern Atlantic and tropical Pacific ...
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