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    Double-Diffusive Interleaving at the Equator 

    Source: Journal of Physical Oceanography:;1991:;Volume( 021 ):;issue: 007:;page 933
    Author(s): Richards, K. J.
    Publisher: American Meteorological Society
    Abstract: A theory for the observed interleaving of water masses at the equator is presented. Unlike layers at midlatitudes, individual layers are observed to be coherent over horizontal scales of hundreds of kilometers. To allow ...
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    The Effect of a Bottom Boundary Layer on the Stability of a Baroclinic Zonal Current 

    Source: Journal of Physical Oceanography:;1982:;Volume( 012 ):;issue: 012:;page 1493
    Author(s): Richards, K. J.
    Publisher: American Meteorological Society
    Abstract: The effect of a depth-limited bottom boundary layer on the stability of a baroclinic zonal current is investigated. The model is of a two-layer quasi-geostrophic flow. Limiting the height of the boundary layer introduces ...
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    Modeling the Benthic Boundary Layer 

    Source: Journal of Physical Oceanography:;1982:;Volume( 012 ):;issue: 005:;page 428
    Author(s): Richards, K. J.
    Publisher: American Meteorological Society
    Abstract: A second-order turbulence closure model is used to study the development of the benthic boundary layer. Results are presented on the effects of a time-dependent oscillatory forcing flow and an initially stably stratified ...
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    The Interaction between the Bottom Mixed layer and Mesoscale Motions of the Ocean: A Numerical Study 

    Source: Journal of Physical Oceanography:;1984:;Volume( 014 ):;issue: 004:;page 754
    Author(s): Richards, K. J.
    Publisher: American Meteorological Society
    Abstract: The interaction between a bottom mixed layer and a mesoscale eddy field is studied using a numerical model of a two-layer quasi-geostrophic fluid above a mixed layer. The height of the mixed layer is assumed to be restricted ...
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    Jet Structure and Scaling in Southern Ocean Models 

    Source: Journal of Physical Oceanography:;1999:;Volume( 029 ):;issue: 006:;page 1143
    Author(s): Sinha, B.; Richards, K. J.
    Publisher: American Meteorological Society
    Abstract: The jet structure of the Antarctic Circumpolar Current (ACC) simulated by two general circulation models (GCMs), FRAM (Fine Resolution Antarctic Model) and POP (Parallel Ocean Program), is examined in relation to the bottom ...
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    Grid Convergent Spray Models for Internal Combustion Engine Computational Fluid Dynamics Simulations 

    Source: Journal of Energy Resources Technology:;2014:;volume( 136 ):;issue: 001:;page 12204
    Author(s): Senecal, P. K.; Pomraning, E.; Richards, K. J.; Som, S.
    Publisher: The American Society of Mechanical Engineers (ASME)
    Abstract: A stateoftheart spray modeling methodology is presented. Key features of the methodology, such as adaptive mesh refinement (AMR), advanced liquid–gas momentum coupling, and improved distribution of the liquid phase, are ...
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    Dispersion of Tracers by Ocean Gyres 

    Source: Journal of Physical Oceanography:;1995:;Volume( 025 ):;issue: 005:;page 873
    Author(s): Richards, K. J.; Jia, Y.; Rogers, C. F.
    Publisher: American Meteorological Society
    Abstract: The dispersion of a tracer by a two-dimensional gyre circulation is studied using simple numerical models. Two approaches are taken: a random walk model formulated in a streamline coordinate system and the numerical solution ...
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    Flow and Mixing in the Rift Valley of the Mid-Atlantic Ridge 

    Source: Journal of Physical Oceanography:;2002:;Volume( 032 ):;issue: 006:;page 1763
    Author(s): Thurnherr, A. M.; Richards, K. J.; German, C. R.; Lane-Serff, G. F.; Speer, K. G.
    Publisher: American Meteorological Society
    Abstract: High levels of diapycnal mixing and geothermal heating near midocean ridges contribute to the buoyancy fluxes that are required to close the global circulation. In topographically confined areas, such as the deep median ...
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    Eddies in Numerical Models of the Antarctic Circumpolar Current and Their Influence on the Mean Flow 

    Source: Journal of Physical Oceanography:;1999:;Volume( 029 ):;issue: 003:;page 328
    Author(s): Best, S. E.; Ivchenko, V. O.; Richards, K. J.; Smith, R. D.; Malone, R. C.
    Publisher: American Meteorological Society
    Abstract: The dynamics of the Southern Ocean have been studied using two high-resolution models, namely the Fine Resolution Antarctic Model (FRAM) and the Parallel Ocean Program (POP) model. Analysis of these models includes zonal ...
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