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    A Numerical Investigation of Effects of a Tilt of the Zero Wind Stress Curl Line on the Subduction Process 

    Source: Journal of Physical Oceanography:;1997:;Volume( 027 ):;issue: 006:;page 897
    Author(s): Inui, Tomoko; Hanawa, Kimio
    Publisher: American Meteorological Society
    Abstract: A three-dimensional ocean general circulation model is used to investigate the effects of an idealized, nonzonal wind stress curl on the subduction process in the subtropical gyre. Idealized zonal winds are used to force ...
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    Midlatitude Wind Forcing and Subduction of Temperature Anomalies 

    Source: Journal of Physical Oceanography:;2002:;Volume( 032 ):;issue: 003:;page 1094
    Author(s): Inui, Tomoko; Liu, Zhengyu
    Publisher: American Meteorological Society
    Abstract: An OGCM (MOM1) is used to examine the oceanic response to localized anomalous surface wind and buoyancy forcings. Wind stress and surface cooling anomalies are imposed at several different locations with respect to the ...
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    Subtropical Countercurrent in an Idealized Ocean GCM 

    Source: Journal of Physical Oceanography:;1999:;Volume( 029 ):;issue: 006:;page 1303
    Author(s): Kubokawa, Atsushi; Inui, Tomoko
    Publisher: American Meteorological Society
    Abstract: In the North Pacific, there is a shallow eastward current called the subtropical countercurrent, which flows across the central subtropical gyre. The present article studies the generation mechanism of the subtropical ...
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    A Numerical Investigation of the Subduction Process in Response to an Abrupt Intensification of the Westerlies 

    Source: Journal of Physical Oceanography:;1999:;Volume( 029 ):;issue: 008:;page 1993
    Author(s): Inui, Tomoko; Takeuchi, Kensuke; Hanawa, Kimio
    Publisher: American Meteorological Society
    Abstract: A three-dimensional ocean general circulation model, forced by idealized zonal winds, is used to investigate the effect of an abrupt intensification of westerly winds on the subduction process. Four experiments are carried ...
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