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    A Numerical Modeling Study of the Upwelling Source Waters along the Oregon Coast during 2005 

    Source: Journal of Physical Oceanography:;2010:;Volume( 041 ):;issue: 001:;page 88
    Author(s): Rivas, David; Samelson, R. M.
    Publisher: American Meteorological Society
    Abstract: Regional ocean circulation along the Oregon coast is studied numerically for forcing fields derived from year 2005 and climatological-mean conditions. The primary object is to study directly the Lagrangian pathways by which ...
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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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    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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    Application of Classical Coastal Trapped Wave Theory to High-Scattering Regions 

    Source: Journal of Physical Oceanography:;2019:;volume 049:;issue 009:;page 2201
    Author(s): Brunner, Kelsey; Rivas, David; Lwiza, Kamazima M. M.
    Publisher: American Meteorological Society
    Abstract: AbstractSince the 1970s, analytical models of coastal trapped waves (CTWs) have been developed using a first-order wave equation in the long-wave limit. Formulations of this kind require assumptions of a straight coastline ...
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