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    Spinup of Source-driven Circulation in an Abyssal Basin in the Presence of Bottom Topography 

    Source: Journal of Physical Oceanography:;1991:;Volume( 021 ):;issue: 010:;page 1501
    Author(s): Kawase, Mitsuhiro; Straub, David
    Publisher: American Meteorological Society
    Abstract: Spinup of the circulation driven by an inflow into an abyssal basin containing a simple large-scale topographic feature is studied, using an inverted one-and-a-half-layer shallow-water model. Two types of topography, one ...
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    On the Transport and Angular Momentum Balance of Channel Models of the Antarctic Circumpolar Current 

    Source: Journal of Physical Oceanography:;1993:;Volume( 023 ):;issue: 004:;page 776
    Author(s): Straub, David N.
    Publisher: American Meteorological Society
    Abstract: Angular momentum balances are discussed, both in general as well as in the context of simple channel models of the Antarctic Circumpolar Current (ACC). Particular emphasis is placed on the close relationship between the ...
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    Forced Near-Inertial Motion and Dissipation of Low-Frequency Kinetic Energy in a Wind-Driven Channel Flow 

    Source: Journal of Physical Oceanography:;2015:;Volume( 046 ):;issue: 001:;page 79
    Author(s): Taylor, Stephanne; Straub, David
    Publisher: American Meteorological Society
    Abstract: sing primitive equation simulations, a zonally periodic channel is considered. The channel flow is forced by a combination of steady and high-frequency winds. The high-frequency forcing excites near-inertial motion, and ...
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    Effects of Adding Forced Near-Inertial Motion to a Wind-Driven Channel Flow 

    Source: Journal of Physical Oceanography:;2020:;volume( 50 ):;issue: 010:;page 2983
    Author(s): Taylor, Stephanne;Straub, David
    Publisher: American Meteorological Society
    Abstract: An eddy-resolving primitive equation ocean model is used to examine energy transfers between frequency bands. Steady wind forcing is used to drive a geostrophic channel to which high-frequency winds are added. This excites ...
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    Instability of 2D Flows to Hydrostatic 3D Perturbations 

    Source: Journal of the Atmospheric Sciences:;2003:;Volume( 060 ):;issue: 001:;page 79
    Author(s): Straub, David N.
    Publisher: American Meteorological Society
    Abstract: Considered here is the evolution of three-dimensional perturbations to the hydrostatic equations linearized about a two-dimensional base state U. Motivated by an argument by T. Warn, this study begins with the nonrotating, ...
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    Simple Models of Flow over Deep Ocean Sills: Planetary and Semigeostrophic Solutions 

    Source: Journal of Physical Oceanography:;1998:;Volume( 028 ):;issue: 005:;page 971
    Author(s): Straub, David N.
    Publisher: American Meteorological Society
    Abstract: Simple inverted reduced-gravity models of flow over deep ocean sills are considered, with emphasis placed on the case for which sills are wide with respect to the abyssal Rossby radius. When the length scale of the flow ...
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    Near-Inertial Oscillations and the Damping of Midlatitude Gyres: A Modeling Study 

    Source: Journal of Physical Oceanography:;2009:;Volume( 039 ):;issue: 009:;page 2338
    Author(s): Gertz, Aaron; Straub, David N.
    Publisher: American Meteorological Society
    Abstract: The classic wind-driven double-gyre problem for a homogeneous (unstratified) thin aspect ratio fluid is considered, but allowing for the flow to be depth dependent. Linear free modes for which the vertical wavenumber kz ? ...
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    Basin and Channel Contributions to a Model Antarctic Circumpolar Current 

    Source: Journal of Physical Oceanography:;2009:;Volume( 039 ):;issue: 004:;page 986
    Author(s): Nadeau, Louis-Philippe; Straub, David N.
    Publisher: American Meteorological Society
    Abstract: The idea that basinlike dynamics may play a major role in determining the Antarctic Circumpolar Current (ACC) transport is revisited. A simple analytic model is developed to describe the relationship between the wind stress ...
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    Influence of Wind Stress, Wind Stress Curl, and Bottom Friction on the Transport of a Model Antarctic Circumpolar Current 

    Source: Journal of Physical Oceanography:;2012:;Volume( 042 ):;issue: 001:;page 207
    Author(s): Nadeau, Louis-Philippe; Straub, David N.
    Publisher: American Meteorological Society
    Abstract: ddy-permitting simulations of a wind-driven quasigeostrophic model in an idealized Southern Ocean setting are used to attempt to describe what sets the wind-driven circumpolar transport of the Antarctic Circumpolar Current ...
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    Energy Fluxes in the Quasigeostrophic Double Gyre Problem 

    Source: Journal of Physical Oceanography:;2014:;Volume( 044 ):;issue: 006:;page 1505
    Author(s): Straub, David N.; Nadiga, Balasubramanya T.
    Publisher: American Meteorological Society
    Abstract: he classic baroclinic, wind-driven, double gyre problem is considered over a range of deformation radii, wind stress amplitudes, and bottom friction coefficients with the aim of better understanding the transfer of energy ...
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