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    Two Limiting Types of Oceanic Finestructures 

    Source: Journal of Physical Oceanography:;1987:;Volume( 017 ):;issue: 009:;page 1539
    Author(s): Ochoa, José
    Publisher: American Meteorological Society
    Abstract: Profiles from CTD surveys in the Northeastern Pacific are used to study temperature, salinity and density finestructures. Finestructures are defined here as those perturbations of the thermodynamic fields which are not due ...
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    Vertical Vorticity Balance in Meanders Downstream the Agulhas Retroflection 

    Source: Journal of Physical Oceanography:;2007:;Volume( 037 ):;issue: 006:;page 1740
    Author(s): Ochoa, José; Niiler, Peter P.
    Publisher: American Meteorological Society
    Abstract: The Agulhas Current flows poleward along the western boundary of the southeastern Indian Ocean where, at the southernmost latitude of the African continent, it executes a dramatic anticyclonic turn, or retroflection, to ...
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    The Ventilation of the Deep Gulf of Mexico 

    Source: Journal of Physical Oceanography:;2005:;Volume( 035 ):;issue: 010:;page 1763
    Author(s): Rivas, David; Badan, Antoine; Ochoa, José
    Publisher: American Meteorological Society
    Abstract: Recent measurements over the sill in the Yucatan Channel indicate that the deepest flows between the Caribbean Sea and the Gulf of Mexico, those that take place below the sill level at the Florida Straits, have zero mean ...
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    Lateral Friction in Reduced-Gravity Models: Parameterizations Consistent with Energy Dissipation and Conservation of Angular Momentum 

    Source: Journal of Physical Oceanography:;2011:;Volume( 041 ):;issue: 010:;page 1894
    Author(s): Ochoa, José; Sheinbaum, Julio; Jiménez, Aleph
    Publisher: American Meteorological Society
    Abstract: he f-plane reduced-gravity model has been extended with the parameterization of lateral friction in the momentum equations. The parameterization should preferably fulfill some requisites. One of them is that in the absence ...
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    Vertical Velocity and Vertical Heat Flux Observed within Loop Current Eddies in the Central Gulf of Mexico 

    Source: Journal of Physical Oceanography:;2008:;Volume( 038 ):;issue: 011:;page 2461
    Author(s): Rivas, David; Badan, Antoine; Sheinbaum, Julio; Ochoa, José; Candela, Julio
    Publisher: American Meteorological Society
    Abstract: Sixteen months of observations from a surface-to-bottom mooring in the central Gulf of Mexico show that acoustic Doppler current profilers (ADCPs) are useful for directly measuring the vertical velocity within mesoscale ...
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    Deep Currents in the Bay of Campeche 

    Source: Journal of Physical Oceanography:;2011:;Volume( 041 ):;issue: 010:;page 1902
    Author(s): Kolodziejczyk, Nicolas; Ochoa, José; Candela, Julio; Sheinbaum, Julio
    Publisher: American Meteorological Society
    Abstract: ata from five moorings deployed in the Bay of Campeche during November 2007?July 2008 are used to analyze subinertial motions of waters below 1000-m depth. To the authors? knowledge, this is the first time such a comprehensive ...
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    Near-Surface and Deep Circulation Coupling in the Western Gulf of Mexico 

    Source: Journal of Physical Oceanography:;2017:;volume 048:;issue 001:;page 145
    Author(s): Tenreiro, M.; Candela, Julio; Sanz, Enric Pallàs; Sheinbaum, Julio; Ochoa, José
    Publisher: American Meteorological Society
    Abstract: AbstractThe coupling between the upper (z < 1000-m depth) and deep (z > 1500 m) circulation in the western Gulf of Mexico (WGoM) driven by the arrival of Loop Current eddies (LCEs) is analyzed from moorings measuring ...
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    Loop Current Frontal Eddies: Formation along the Campeche Bank and Impact of Coastally Trapped Waves 

    Source: Journal of Physical Oceanography:;2016:;Volume( 046 ):;issue: 011:;page 3339
    Author(s): Jouanno, Julien; Ochoa, José; Pallàs-Sanz, Enric; Sheinbaum, Julio; Andrade-Canto, Fernando; Candela, Julio; Molines, Jean-Marc
    Publisher: American Meteorological Society
    Abstract: elocity data from a mooring array deployed northeast of the Campeche Bank (CB) show the presence of subinertial, high-frequency (below 15 days) velocity fluctuations within the core of the northward flowing Loop Current. ...
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    Deep-Water Warming in the Gulf of Mexico from 2003 to 2019 

    Source: Journal of Physical Oceanography:;2021:;volume( 051 ):;issue: 004:;page 1021
    Author(s): Ochoa, José;Ferreira-Bartrina, Vicente;Candela, Julio;Sheinbaum, Julio;López, Manuel;Pérez-Brunius, Paula;Herzka, Sharon;Amon, Rainer M.W.
    Publisher: American Meteorological Society
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    DSpace software copyright © 2002-2015  DuraSpace
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    DSpace software copyright © 2002-2015  DuraSpace
    نرم افزار کتابخانه دیجیتال "دی اسپیس" فارسی شده توسط یابش برای کتابخانه های ایرانی | تماس با یابش
    yabeshDSpacePersian