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    A Mechanistic Model of Ocean Interdecadal Thermohaline Oscillations 

    Source: Journal of Physical Oceanography:;1995:;Volume( 025 ):;issue: 012:;page 3239
    Author(s): Yin, F. L.
    Publisher: American Meteorological Society
    Abstract: Oceanic interdecadal thermohaline oscillations are studied in the context of a conceptual two box model. In this mechanistic model, two essential processes associated with convection, subsurface advective heating and surface ...
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    Dynamics and Heat Balance of Steady Equatorial Undercurrents 

    Source: Journal of Physical Oceanography:;1993:;Volume( 023 ):;issue: 008:;page 1647
    Author(s): Yin, F. L.; Sarachik, E. S.
    Publisher: American Meteorological Society
    Abstract: A two-dimensional (in a vertical and meridional plane) model for steady equatorial undercurrents is described. Compared to the primitive equation model, the zonal pressure gradient and associated zonal temperature gradients ...
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    Interdecadal Thermohaline Oscillations in a Sector Ocean General Circulation Model: Advective and Convective Processes 

    Source: Journal of Physical Oceanography:;1995:;Volume( 025 ):;issue: 011:;page 2465
    Author(s): Yin, F. L.; Sarachik, E. S.
    Publisher: American Meteorological Society
    Abstract: Oceanic interdecadal thermohaline oscillations are investigated with a coarse-resolution version of the Geophysical Fluid Dynamics Laboratory Modular Ocean Model. The geometry of the model is a box with a depth of 5000 m ...
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    Equilibrium Response of Ocean Deep-Water Circulation to Variations in Ekman Pumping and Deep-Water Sources 

    Source: Journal of Physical Oceanography:;1992:;Volume( 022 ):;issue: 010:;page 1129
    Author(s): Yin, F. L.; Fung, I. Y.; Chu, C. K.
    Publisher: American Meteorological Society
    Abstract: A multilayer ocean model that is physically simple and computationally efficient is developed for studies of competition and interaction among deep-water sources in determining ocean circulation. The model is essentially ...
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