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    Interaction between an Island and the Ventilated Thermocline: Implications for the Hawaiian Lee Countercurrent 

    Source: Journal of Physical Oceanography:;2002:;Volume( 032 ):;issue: 012:;page 3408
    Author(s): Qiu, Bo; Durland, Theodore S.
    Publisher: American Meteorological Society
    Abstract: The ventilated thermocline theory is adapted to include the interaction between an island and the wind-driven subtropical circulation. The primary goal is an understanding of the effect of this interaction on the Hawaiian ...
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    Transmission of Subinertial Kelvin Waves through a Strait 

    Source: Journal of Physical Oceanography:;2003:;Volume( 033 ):;issue: 007:;page 1337
    Author(s): Durland, Theodore S.; Qiu, Bo
    Publisher: American Meteorological Society
    Abstract: Solutions are found for the transmission of 1½-layer subinertial Kelvin waves through an ?ideal strait? with parallel channel walls and square corner mouths. This is shown to be a wave interference problem similar to the ...
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    The Wavenumber–Frequency Content of Resonantly Excited Equatorial Waves 

    Source: Journal of Physical Oceanography:;2012:;Volume( 042 ):;issue: 011:;page 1834
    Author(s): Durland, Theodore S.; Farrar, J. Thomas
    Publisher: American Meteorological Society
    Abstract: he theoretical resonant excitation of equatorial inertia?gravity waves and mixed Rossby?gravity waves is examined. Contrary to occasionally published expectations, solutions show that winds that are broadband in both zonal ...
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    Wavenumber–Frequency Spectra of Inertia–Gravity and Mixed Rossby–Gravity Waves in the Equatorial Pacific Ocean 

    Source: Journal of Physical Oceanography:;2012:;Volume( 042 ):;issue: 011:;page 1859
    Author(s): Farrar, J. Thomas; Durland, Theodore S.
    Publisher: American Meteorological Society
    Abstract: n the 1970s and 1980s, there was considerable interest in near-equatorial variability at periods of days to weeks associated with oceanic equatorial inertia?gravity waves and mixed Rossby?gravity waves. At that time, the ...
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    Response to a Steady Poleward Outflow. Part I: The Linear, Quasigeostrophic Problem 

    Source: Journal of Physical Oceanography:;2009:;Volume( 039 ):;issue: 007:;page 1541
    Author(s): Durland, Theodore S.; Pedlosky, Joseph; Spall, Michael A.
    Publisher: American Meteorological Society
    Abstract: The response of a zonal channel to a uniform, switched-on but subsequently steady poleward outflow is presented. An eastward coastal current with a Kelvin wave?s cross-shore structure is found to be generated instantly ...
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    Response to a Steady Poleward Outflow. Part II: Oscillations and Eddies 

    Source: Journal of Physical Oceanography:;2009:;Volume( 039 ):;issue: 007:;page 1551
    Author(s): Durland, Theodore S.; Spall, Michael A.; Pedlosky, Joseph
    Publisher: American Meteorological Society
    Abstract: A conceptually simple model is presented for predicting the amplitude and periodicity of eddies generated by a steady poleward outflow in a 1½-layer ?-plane formulation. The prediction model is rooted in linear quasigeostrophic ...
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    Modification of Long Equatorial Rossby Wave Phase Speeds by Zonal Currents 

    Source: Journal of Physical Oceanography:;2011:;Volume( 041 ):;issue: 006:;page 1077
    Author(s): Durland, Theodore S.; Samelson, Roger M.; Chelton, Dudley B.; de Szoeke, Roland A.
    Publisher: American Meteorological Society
    Abstract: reviously unaddressed aspects of how equatorial currents affect long Rossby wave phase speeds are investigated using solutions of the shallow-water equations linearized about quasi-realistic currents. Modification of the ...
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