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    Abrupt Transitions and Hysteresis in Thermohaline Laboratory Models 

    Source: Journal of Physical Oceanography:;2009:;Volume( 039 ):;issue: 005:;page 1231
    Author(s): Whitehead, J. A.
    Publisher: American Meteorological Society
    Abstract: As a driving parameter is slowly altered, thermohaline ocean circulation models show either a smooth evolution of a mode of flow or an abrupt transition of temperature and salinity fields from one mode to another. An abrupt ...
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    Constant Potential Vorticity Hydraulically Controlled Flow—Complexities from Passage Shape 

    Source: Journal of Physical Oceanography:;2003:;Volume( 033 ):;issue: 001:;page 305
    Author(s): Whitehead, J. A.
    Publisher: American Meteorological Society
    Abstract: Velocity, surface height profiles, and volume flux are calculated for critically controlled flow of a layer of rotating fluid from a channel to an exit passage. The upstream fluid possesses constant potential vorticity. ...
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    CORRIGENDUM 

    Source: Journal of Physical Oceanography:;2003:;Volume( 033 ):;issue: 005:;page 1142
    Author(s): Whitehead, J. A.
    Publisher: American Meteorological Society
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    A Laboratory Model of Cooling over the Continental Shelf 

    Source: Journal of Physical Oceanography:;1993:;Volume( 023 ):;issue: 011:;page 2412
    Author(s): Whitehead, J. A.
    Publisher: American Meteorological Society
    Abstract: A laboratory experiment is conducted where hot water is cooled by exposure to air in a cylindrical rotating tank with a flat shallow outer ?continental shelf? region next to a sloping ?continental slope? bottom and a flat ...
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    A Laboratory Model of Vertical Ocean Circulation Driven by Mixing 

    Source: Journal of Physical Oceanography:;2008:;Volume( 038 ):;issue: 005:;page 1091
    Author(s): Whitehead, J. A.; Wang, Wei
    Publisher: American Meteorological Society
    Abstract: A model of deep ocean circulation driven by turbulent mixing is produced in a long, rectangular laboratory tank. The salinity difference is substituted for the thermal difference between tropical and polar regions. Freshwater ...
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    Eddy Shedding from a Boundary Current around a Cape over a Sloping Bottom 

    Source: Journal of Physical Oceanography:;2000:;Volume( 030 ):;issue: 007:;page 1514
    Author(s): Cenedese, C.; Whitehead, J. A.
    Publisher: American Meteorological Society
    Abstract: The authors discuss laboratory experiments that elucidate the mechanism of formation and westward drift of anticyclonic baroclinic vortices from a buoyant surface current flowing along a lateral boundary and around a cape. ...
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    A Laboratory Model of Thermocline Depth and Exchange Fluxes across Circumpolar Fronts 

    Source: Journal of Physical Oceanography:;2004:;Volume( 034 ):;issue: 003:;page 656
    Author(s): Cenedese, Claudia; Marshall, John; Whitehead, J. A.
    Publisher: American Meteorological Society
    Abstract: A laboratory experiment has been constructed to investigate the possibility that the equilibrium depth of a circumpolar front is set by a balance between the rate at which potential energy is created by mechanical and ...
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    Rotating Convection Driven by Differential Bottom Heating 

    Source: Journal of Physical Oceanography:;1999:;Volume( 029 ):;issue: 006:;page 1208
    Author(s): Park, Young-Gyu; Whitehead, J. A.
    Publisher: American Meteorological Society
    Abstract: Convection experiments were carried out in a rectangular tank as a model of oceanic meridional overturning circulation. The objective was finding a relation between the meridional heat flux and thermal forcing. To make the ...
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    Antarctic Bottom Water Flux in the Equatorial Western Atlantic 

    Source: Journal of Physical Oceanography:;1997:;Volume( 027 ):;issue: 009:;page 1903
    Author(s): Hall, Melinda M.; McCartney, Michael; Whitehead, J. A.
    Publisher: American Meteorological Society
    Abstract: A moored array at the equator in the western basin of the Atlantic provides a 604-day time series of abyssal currents and temperatures spanning the full breadth of the Antarctic Bottom Water (AABW) flowing from the Brazil ...
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    A Dense Current Flowing down a Sloping Bottom in a Rotating Fluid 

    Source: Journal of Physical Oceanography:;2004:;Volume( 034 ):;issue: 001:;page 188
    Author(s): Cenedese, C.; Whitehead, J. A.; Ascarelli, T. A.; Ohiwa, M.
    Publisher: American Meteorological Society
    Abstract: A density-driven current was generated in the laboratory by releasing dense fluid over a sloping bottom in a rotating freshwater system. The behavior of the dense fluid descending the slope has been investigated by ...
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