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    Eddy Shedding from a Boundary Current around a Cape over a Sloping Bottom 

    Source: Journal of Physical Oceanography:;2000:;Volume( 030 ):;issue: 007:;page 1514
    Author(s): Cenedese, C.; Whitehead, J. A.
    Publisher: American Meteorological Society
    Abstract: The authors discuss laboratory experiments that elucidate the mechanism of formation and westward drift of anticyclonic baroclinic vortices from a buoyant surface current flowing along a lateral boundary and around a cape. ...
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    A Laboratory Study of Iceberg Side Melting in Vertically Sheared Flows 

    Source: Journal of Physical Oceanography:;2018:;volume 048:;issue 006:;page 1367
    Author(s): FitzMaurice, A.; Cenedese, C.; Straneo, F.
    Publisher: American Meteorological Society
    Abstract: AbstractAn earlier study indicates that the side melting of icebergs subject to vertically homogeneous horizontal velocities is controlled by two distinct regimes, which depend on the melt plume behavior and produce a ...
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    A Dense Current Flowing down a Sloping Bottom in a Rotating Fluid 

    Source: Journal of Physical Oceanography:;2004:;Volume( 034 ):;issue: 001:;page 188
    Author(s): Cenedese, C.; Whitehead, J. A.; Ascarelli, T. A.; Ohiwa, M.
    Publisher: American Meteorological Society
    Abstract: A density-driven current was generated in the laboratory by releasing dense fluid over a sloping bottom in a rotating freshwater system. The behavior of the dense fluid descending the slope has been investigated by ...
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