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    AUV Observations of the Diurnal Surface Layer in the North Atlantic Salinity Maximum 

    Source: Journal of Physical Oceanography:;2014:;Volume( 044 ):;issue: 006:;page 1595
    Author(s): Hodges, Benjamin A.; Fratantoni, David M.
    Publisher: American Meteorological Society
    Abstract: utonomous underwater vehicle (AUV) surveys of temperature, salinity, and velocity in the upper 10 m of the ocean were carried out in low-wind conditions near the North Atlantic surface salinity maximum as part of the ...
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    North Brazil Current Ring Generation and Evolution Observed with SeaWiFS 

    Source: Journal of Physical Oceanography:;2002:;Volume( 032 ):;issue: 003:;page 1058
    Author(s): Fratantoni, David M.; Glickson, Deborah A.
    Publisher: American Meteorological Society
    Abstract: The earth's largest oceanic rings are formed by the retroflecting North Brazil Current (NBC) near 8°N in the western tropical Atlantic. The NBC flows northward across the equator and past the mouth of the Amazon River ...
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    A Deep-Towed ADCP-CTD Instrument Package Developed for Abyssal Overflow Measurements in the Northeastern Caribbean Sea 

    Source: Journal of Atmospheric and Oceanic Technology:;1996:;volume( 013 ):;issue: 003:;page 680
    Author(s): Fratantoni, David M.; Johns, William E.
    Publisher: American Meteorological Society
    Abstract: A deep-towed instrument package has been developed to study the velocity and tracer signature of abyssal overflows in the northeastern Caribbean. Primary package components include a conductivity-temperature-depth (CTD) ...
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    The Evolution and Demise of North Brazil Current Rings 

    Source: Journal of Physical Oceanography:;2006:;Volume( 036 ):;issue: 007:;page 1241
    Author(s): Fratantoni, David M.; Richardson, Philip L.
    Publisher: American Meteorological Society
    Abstract: Subsurface float and surface drifter observations illustrate the structure, evolution, and eventual demise of 10 North Brazil Current (NBC) rings as they approached and collided with the Lesser Antilles in the western ...
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    SOFAR Float Observations of an Intermediate-Depth Eastern Boundary Current and Mesoscale Variability in the Eastern Tropical Atlantic Ocean 

    Source: Journal of Physical Oceanography:;1999:;Volume( 029 ):;issue: 006:;page 1265
    Author(s): Fratantoni, David M.; Richardson, Philip L.
    Publisher: American Meteorological Society
    Abstract: Two neutrally buoyant SOFAR floats vigorously looped and meandered at depths of 950?1150 m in the eastern tropical Atlantic Ocean. The float trajectories illustrate a poleward flow along the tropical eastern boundary and ...
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    Low-Latitude Circulation and Mass Transport Pathways in a Model of the Tropical Atlantic Ocean 

    Source: Journal of Physical Oceanography:;2000:;Volume( 030 ):;issue: 008:;page 1944
    Author(s): Fratantoni, David M.; Johns, William E.; Townsend, Tamara L.; Hurlburt, Harley E.
    Publisher: American Meteorological Society
    Abstract: An eddy-resolving numerical ocean circulation model is used to investigate the pathways of low-latitude intergyre mass transport associated with the upper limb of the Atlantic meridional overturning cell (MOC). Numerical ...
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    Equilibration and Circulation of Red Sea Outflow Water in the Western Gulf of Aden 

    Source: Journal of Physical Oceanography:;2005:;Volume( 035 ):;issue: 011:;page 1963
    Author(s): Bower, Amy S.; Johns, William E.; Fratantoni, David M.; Peters, Hartmut
    Publisher: American Meteorological Society
    Abstract: Hydrographic, direct velocity, and subsurface float observations from the 2001 Red Sea Outflow Experiment (REDSOX) are analyzed to investigate the gravitational and dynamical adjustment of the Red Sea Outflow Water (RSOW) ...
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    Mixing and Entrainment in the Red Sea Outflow Plume. Part I: Plume Structure 

    Source: Journal of Physical Oceanography:;2005:;Volume( 035 ):;issue: 005:;page 569
    Author(s): Peters, Hartmut; Johns, William E.; Bower, Amy S.; Fratantoni, David M.
    Publisher: American Meteorological Society
    Abstract: When the salty and heavy water of the Red Sea exits from the Strait of Bab el Mandeb, it continues downslope into the Gulf of Aden mainly along two channels. The 130-km-long ?Northern Channel? (NC) is topographically ...
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