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    Response of the Separated Western Boundary Current to Harmonic and Stochastic Wind Stress Variations in a 1.5-Layer Ocean Model 

    Source: Journal of Physical Oceanography:;2005:;Volume( 035 ):;issue: 008:;page 1341
    Author(s): Sirven, J.
    Publisher: American Meteorological Society
    Abstract: A time-dependent version of the Parsons model (geostrophic 1.5-layer model of the ventilated thermocline) has been developed to investigate the response of the midlatitude ocean to wind stress variations in a simple ...
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    Variability of the Thermocline Due to a Sudden Change in the Ekman Pumping 

    Source: Journal of Physical Oceanography:;2000:;Volume( 030 ):;issue: 007:;page 1776
    Author(s): Sirven, J.; Frankignoul, C.
    Publisher: American Meteorological Society
    Abstract: The thermocline variability caused by a sudden variation of the Ekman pumping is studied, using a 2.5-layer geostrophic model that represents the ventilated and the shadow zones of a subtropical gyre and baroclinic Rossby ...
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    An Idealized Model Study of the Mass and Heat Transports between the Subpolar and Subtropical Gyres 

    Source: Journal of Physical Oceanography:;2001:;Volume( 031 ):;issue: 010:;page 2903
    Author(s): Herbaut, C.; Sirven, J.; Czaja, A.
    Publisher: American Meteorological Society
    Abstract: The response of an ocean model of the subtropical and subpolar gyres to idealized surface forcing anomalies that mimic the thermal and mechanical forcing associated with the North Atlantic Oscillation (NAO) is analyzed. ...
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    Response of a Simplified Oceanic General Circulation Model to Idealized NAO-like Stochastic Forcing 

    Source: Journal of Physical Oceanography:;2002:;Volume( 032 ):;issue: 011:;page 3182
    Author(s): Herbaut, C.; Sirven, J.; Février, S.
    Publisher: American Meteorological Society
    Abstract: The response of a simplified model of the subtropical and subpolar gyres to a mechanical stochastic forcing that mimics the North Atlantic Oscillation (NAO) is studied. An internal damped mode of oscillation with a 22?24-yr ...
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    Spectrum of Wind-Driven Baroclinic Fluctuations of the Ocean in the Midlatitudes 

    Source: Journal of Physical Oceanography:;2002:;Volume( 032 ):;issue: 008:;page 2405
    Author(s): Sirven, J.; Frankignoul, C.; de Coëtlogon, G.; Taillandier, V.
    Publisher: American Meteorological Society
    Abstract: In the midlatitudes, the thermocline depth variations are largely due to Rossby waves of first baroclinic mode forced by stochastic wind stress. The frequency spectrum of this oceanic response is investigated with a simple ...
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