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    Slow Instabilities in Tropical Ocean Basin–Global Atmosphere Models 

    Source: Journal of the Atmospheric Sciences:;1988:;Volume( 045 ):;issue: 005:;page 830
    Author(s): Hirst, Anthony C.
    Publisher: American Meteorological Society
    Abstract: The effect of ocean boundaries on instability in coupled ocean-natmosphere models is determined. Eigenvalues and eigenvectors are calculated for coupled systems featuring an ocean basin bounded zonally by a flat continent. ...
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    Unstable and Damped Equatorial Modes in Simple Coupled Ocean-Atmosphere Models 

    Source: Journal of the Atmospheric Sciences:;1986:;Volume( 043 ):;issue: 006:;page 606
    Author(s): Hirst, Anthony C.
    Publisher: American Meteorological Society
    Abstract: Free equatorial modes for several simple coupled ocean-atmosphere models are determined. They are found to include unstable and damped modes of large zonal scale and long period. The influence of ocean thermo-dynamics on ...
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    Interannual Variability in a Tropical Atmosphere–Ocean Model: Influence of the Basic State, Ocean Geometry and Nonlinearity 

    Source: Journal of the Atmospheric Sciences:;1988:;Volume( 046 ):;issue: 012:;page 1687
    Author(s): Battisti, David S.; Hirst, Anthony C.
    Publisher: American Meteorological Society
    Abstract: The behavior of a tropical coupled atmosphere/ocean model is analyzed for a range of different background states and ocean geometries. The model is essentially that of Cane and Zebiak for the tropical Pacific, except only ...
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    Intraseasonal and Interannual Oscillations in Coupled Ocean-Atmosphere Models 

    Source: Journal of Climate:;1990:;volume( 003 ):;issue: 007:;page 713
    Author(s): Hirst, Anthony C.; Lau, K-M.
    Publisher: American Meteorological Society
    Abstract: This study investigates the behavior of coupled ocean-atmosphere models in an environment where atmospheric wave speeds are considerably reduced from their dry atmospheric values, by, for example, condensation-moisture ...
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    Deep-Water Properties and Surface Buoyancy Flux as Simulated by a Z-Coordinate Model Including Eddy-Induced Advection 

    Source: Journal of Physical Oceanography:;1996:;Volume( 026 ):;issue: 007:;page 1320
    Author(s): Hirst, Anthony C.; McDougall, Trevor J.
    Publisher: American Meteorological Society
    Abstract: A parameterization for the adiabatic transport effect of eddies is introduced into a World Ocean model based on the Bryan-Cox code. The model topography is only lightly smoothed and retains realistic sill depths and ...
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    The Role of Indonesian Throughflow in a Global Ocean GCM 

    Source: Journal of Physical Oceanography:;1993:;Volume( 023 ):;issue: 006:;page 1057
    Author(s): Hirst, Anthony C.; Godfrey, J. S.
    Publisher: American Meteorological Society
    Abstract: The effect of the Indonesian Throughflow on the World Ocean circulation is examined by a series of experiments with a global ocean GCM. The principal objective is to gain an understanding of how ocean flows respond to the ...
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    Meridional Overturning and Dianeutral Transport in a z-Coordinate Ocean Model Including Eddy-Induced Advection 

    Source: Journal of Physical Oceanography:;1998:;Volume( 028 ):;issue: 006:;page 1205
    Author(s): Hirst, Anthony C.; McDougall, Trevor J.
    Publisher: American Meteorological Society
    Abstract: The present study examines the marked changes in the patterns of meridional overturning and dianeutral motion that occur upon introduction of the Gent and McWilliams (GM) scheme for eddy-induced transport into a coarse-resolution ...
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    The Meridional Overturning Cells of a World Ocean Model in Neutral Density Coordinates 

    Source: Journal of Physical Oceanography:;1996:;Volume( 026 ):;issue: 005:;page 775
    Author(s): Hirst, Anthony C.; Jackett, David R.; McDougall, Trevor J.
    Publisher: American Meteorological Society
    Abstract: A comparison is made of the meridional overturning circulation in a coarse-resolution World Ocean model when the integration is performed along (i) level, (ii) potential density, and (iii) neutral density surfaces. In the ...
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    The Seasonal Footprinting Mechanism in the CSIRO General Circulation Models 

    Source: Journal of Climate:;2003:;volume( 016 ):;issue: 016:;page 2653
    Author(s): Vimont, Daniel J.; Battisti, David S.; Hirst, Anthony C.
    Publisher: American Meteorological Society
    Abstract: An influence of midlatitude atmospheric variability on interannual ENSO and decadal ENSO-like variability is established and investigated in the Commonwealth Scientific and Industrial Research Organisation (CSIRO) coupled ...
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    Comparison of a Coupled Ocean–Atmosphere Model with and without Oceanic Eddy-Induced Advection. Part I: Ocean Spinup and Control Integrations 

    Source: Journal of Climate:;2000:;volume( 013 ):;issue: 001:;page 139
    Author(s): Hirst, Anthony C.; O’Farrell, Siobhan P.; Gordon, Hal B.
    Publisher: American Meteorological Society
    Abstract: The Gent and McWilliams (GM) parameterization for large-scale water transport caused by mesoscale oceanic eddies is introduced into the oceanic component of the Commonwealth Scientific and Industrial Research Organisation ...
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