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    The Zonal Dimension of the Indian Ocean Meridional Overturning Circulation 

    Source: Journal of Physical Oceanography:;2008:;Volume( 038 ):;issue: 002:;page 359
    Author(s): Drijfhout, Sybren S.; Garabato, Alberto C. Naveira
    Publisher: American Meteorological Society
    Abstract: The three-dimensional structure of the meridional overturning circulation (MOC) in the deep Indian Ocean is investigated with an eddy-permitting ocean model. The amplitude of the modeled deep Indian Ocean MOC is 5.6 Sv (1 ...
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    The Influence of Diapycnal Mixing on Quasi-Steady Overturning States in the Indian Ocean 

    Source: Journal of Physical Oceanography:;2007:;Volume( 037 ):;issue: 009:;page 2290
    Author(s): Palmer, Matthew D.; Garabato, Alberto C. Naveira; Stark, John D.; Hirschi, Joël J-M.; Marotzke, Jochem
    Publisher: American Meteorological Society
    Abstract: A regional general circulation model (GCM) of the Indian Ocean is used to investigate the influence of prescribed diapycnal diffusivity (Kd) on quasi-steady states of the meridional overturning circulation (MOC). The model ...
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    Evolution of the Deep and Bottom Waters of the Scotia Sea, Southern Ocean, during 1995–2005 

    Source: Journal of Climate:;2008:;volume( 021 ):;issue: 013:;page 3327
    Author(s): Meredith, Michael P.; Garabato, Alberto C. Naveira; Gordon, Arnold L.; Johnson, Gregory C.
    Publisher: American Meteorological Society
    Abstract: The Southern Ocean hosts the formation of the densest layers of the oceanic overturning circulation and provides a climatically sensitive element of deep ocean ventilation. An oceanographic section across the eastern Scotia ...
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    Mesoscale Subduction at the Antarctic Polar Front Driven by Baroclinic Instability 

    Source: Journal of Physical Oceanography:;2001:;Volume( 031 ):;issue: 008:;page 2087
    Author(s): Garabato, Alberto C. Naveira; Leach, Harry; Allen, John T.; Pollard, Raymond T.; Strass, Volker H.
    Publisher: American Meteorological Society
    Abstract: A study of mesoscale subduction at the Antarctic Polar Front (PF) is conducted by use of hydrographic data from a high-resolution, quasi-synoptic survey of the front. The geostrophic velocity and isopycnal potential vorticity ...
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