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    Available Potential Energy and Irreversible Mixing in the Meridional Overturning Circulation 

    Source: Journal of Physical Oceanography:;2009:;Volume( 039 ):;issue: 012:;page 3130
    Author(s): Hughes, Graham O.; Hogg, Andrew Mc C.; Griffiths, Ross W.
    Publisher: American Meteorological Society
    Abstract: The overturning circulation of the global oceans is examined from an energetics viewpoint. A general framework for stratified turbulence is used for this purpose; first, it highlights the importance of available potential ...
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    The Role of Turbulent Mixing in an Overturning Circulation Maintained by Surface Buoyancy Forcing 

    Source: Journal of Physical Oceanography:;2012:;Volume( 042 ):;issue: 011:;page 1907
    Author(s): Stewart, Kial D.; Hughes, Graham O.; Griffiths, Ross W.
    Publisher: American Meteorological Society
    Abstract: he role of externally imposed rates of small-scale mixing in an overturning circulation forced by differential surface buoyancy fluxes is examined in a laboratory experiment. The circulation occupies the full volume and ...
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    Multiple Zonal Jets in a Differentially Heated Rotating Annulus 

    Source: Journal of Physical Oceanography:;2014:;Volume( 044 ):;issue: 009:;page 2273
    Author(s): Smith, Carlowen A.; Speer, Kevin G.; Griffiths, Ross W.
    Publisher: American Meteorological Society
    Abstract: laboratory experiment of multiple baroclinic zonal jets is described, thought to be dynamically similar to flow observed in the Antarctic Circumpolar Current. Differential heating sets the overall temperature difference ...
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    Adjustment of the Meridional Overturning Circulation and Its Dependence on Depth of Mixing 

    Source: Journal of Physical Oceanography:;2015:;Volume( 046 ):;issue: 003:;page 731
    Author(s): Vreugdenhil, Catherine A.; Hogg, Andrew McC.; Griffiths, Ross W.; Hughes, Graham O.
    Publisher: American Meteorological Society
    Abstract: he relative roles of advective processes and mixing on the temporal adjustment of the meridional overturning circulation are examined, in particular the effects of mixing in either the abyssal or upper ocean. Laboratory ...
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