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    Vorticity and Vertical Circulation at an Ocean Front 

    Source: Journal of Physical Oceanography:;1992:;Volume( 022 ):;issue: 006:;page 609
    Author(s): Pollard, R. T.; Regier, L. A.
    Publisher: American Meteorological Society
    Abstract: Density and velocity data with 4-km horizontal resolution from a survey of a front during FASINEX (Frontal Air-Sea Interaction Experiment) are combined to describe the structure of the top 300 m of the ocean. The geostrophic ...
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    Comparison of Shipboard Acoustic Doppler Current Profiler and Moored Current Measurements in the Equatorial Pacific 

    Source: Journal of Atmospheric and Oceanic Technology:;1987:;volume( 004 ):;issue: 004:;page 742
    Author(s): Chereskin, T. K.; Halpern, D.; Regier, L. A.
    Publisher: American Meteorological Society
    Abstract: Depth-averaged current shears computed from shipboard acoustic Doppler current profiler (ADCP) and moored Savonius rotor and vane vector-averaging current meter (VACM) measurements are compared at 35, 62.5, 100 and 140 m ...
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    The Autonomous Lagrangian Circulation Explorer (ALACE) 

    Source: Journal of Atmospheric and Oceanic Technology:;1992:;volume( 009 ):;issue: 003:;page 264
    Author(s): Davis, R. E.; Regier, L. A.; Dufour, J.; Webb, D. C.
    Publisher: American Meteorological Society
    Abstract: The autonomous Lagrangian circulation explorer (ALACE) is a subsurface float that cycles vertically from a depth where it is neutrally buoyant to the surface where it is located by, and relays data to, System Argos satellites. ...
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    Does Ocean Turbulence Peak at the Equator? 

    Source: Journal of Physical Oceanography:;1986:;Volume( 016 ):;issue: 011:;page 1991
    Author(s): Moum, J. N.; Caldwell, D. R.; Paulson, C. A.; Chereskin, T. V.; Regier, L. A.
    Publisher: American Meteorological Society
    Abstract: A 3°N to 3°S transect of the equator at 140°15'W was made in November 1984. Vertical profiles of temperature, conductivity and turbulent dissipation were obtained at approximately 1 km intervals. Contrary to previous ...
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