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    Eddy Resolution versus Eddy Diffusion in a Double Gyre GCM. Part II: Mixing of Passive Tracers 

    Source: Journal of Physical Oceanography:;1994:;Volume( 024 ):;issue: 002:;page 387
    Author(s): Figueroa, Horacio A.
    Publisher: American Meteorological Society
    Abstract: The parameterization of the effect of the unresolved scales of motion on a passive tracer field in large-scale numerical ocean models is analyzed through a combination of Lagrangian and Eulerian velocities. The primitive ...
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    World Ocean Density Ratios 

    Source: Journal of Physical Oceanography:;1996:;Volume( 026 ):;issue: 002:;page 267
    Author(s): Figueroa, Horacio A.
    Publisher: American Meteorological Society
    Abstract: In this report, the potential for salt finger instability in the central water of the World Ocean is examined. The form of the temperature? salinity relationship determined from the Levitus climatological data and the ...
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    Eddy Resolution versus Eddy Diffusion in a Double Gyre GCM. Part I: The Lagrangian and Eulerian Description 

    Source: Journal of Physical Oceanography:;1994:;Volume( 024 ):;issue: 002:;page 371
    Author(s): Figueroa, Horacio A.; Olson, Donald B.
    Publisher: American Meteorological Society
    Abstract: The Lagrangian and Eulerian descriptions of the flow in a double gyre, eddy-resolving numerical simulation are compared in the context of exploring the use of drifter arrays to describe ocean circulation. The parameterization ...
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