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    Lagrangian Motions and Global Density Distributions of Floating Matter in the Ocean Simulated Using Shipdrift Data 

    Source: Journal of Physical Oceanography:;1990:;Volume( 020 ):;issue: 001:;page 125
    Author(s): Wakata, Y.; Sugimori, Y.
    Publisher: American Meteorological Society
    Abstract: The Lagrangian motions of floating matter on the sea surface were simulated by using the surface current data based on shipdrift data produced by Meehl. The validity of the simulation was confirmed by comparing the results ...
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    Unstable Coupled Atmosphere–Ocean Basin Modes in the Presence of a Spatially Varying Basic State 

    Source: Journal of the Atmospheric Sciences:;1991:;Volume( 048 ):;issue: 018:;page 2060
    Author(s): Wakata, Y.; Sarachik, E. S.
    Publisher: American Meteorological Society
    Abstract: The fundamental modes of oscillation of a coupled atmosphere?ocean basin system in the presence of a spatially varying oceanic basic state are investigated by formulating and solving an eigenvalue problem, thereby extending ...
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    Nonlinear Effects in Coupled Atmosphere-Ocean Basin Modes 

    Source: Journal of the Atmospheric Sciences:;1994:;Volume( 051 ):;issue: 006:;page 909
    Author(s): Wakata, Y.; Sarachik, E. S.
    Publisher: American Meteorological Society
    Abstract: The effect of nonlinearities on a previously investigated coupled atmosphere?ocean basin mode is examined. The nonlinearity in the thermodynamic equation for sea surface temperature arises mainly from the dependence of ...
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    On the Role of Equatorial Ocean Modes in the ENSO Cycle 

    Source: Journal of Physical Oceanography:;1991:;Volume( 021 ):;issue: 003:;page 434
    Author(s): Wakata, Y.; Sarachik, E. S.
    Publisher: American Meteorological Society
    Abstract: In order to test certain aspects of the ENSO mechanism proposed by Suarez and Schopf and by Battisti and Hirst, we force a shallow water ocean with 28 years of observed (FSU) winds and decompose both the atmospheric forcing ...
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