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    Vertical Mixing in the Equatorial Pacific along 150°W in March 1988 

    Source: Journal of Physical Oceanography:;1996:;Volume( 026 ):;issue: 003:;page 373
    Author(s): Carr, Mary-Elena; Oakey, Neil S.; Lewis, Marlon R.
    Publisher: American Meteorological Society
    Abstract: A meridional transect along 150°W in March 1988 revealed a statistically significant maximum in turbulent kinetic energy dissipation, ? at 1°S?0° between 40-m and 60-m depth. The wind stress and buoyancy flux were poorly ...
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    Estimates of Dissipation in the Ocean Mixed Layer Using a Quasi-Horizontal Microstructure Profiler 

    Source: Journal of Physical Oceanography:;2001:;Volume( 031 ):;issue: 004:;page 992
    Author(s): Greenan, Blair J. W.; Oakey, Neil S.; Dobson, Fred W.
    Publisher: American Meteorological Society
    Abstract: Some recent measurements of the mixed layer in oceans and lakes have indicated that the rate of the dissipation of turbulent kinetic energy, ε, is much higher than expected from a purely shear-driven wall layer. This ...
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    Stirring by Small-Scale Vortices Caused by Patchy Mixing 

    Source: Journal of Physical Oceanography:;2005:;Volume( 035 ):;issue: 007:;page 1245
    Author(s): Sundermeyer, Miles A.; Ledwell, James R.; Oakey, Neil S.; Greenan, Blair J. W.
    Publisher: American Meteorological Society
    Abstract: Evidence is presented that lateral dispersion on scales of 1?10 km in the stratified waters of the continental shelf may be significantly enhanced by stirring by small-scale geostrophic motions caused by patches of mixed ...
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    A Microstructure Instrument for Profiling Oceanic Turbulence in Coastal Bottom Boundary Layers 

    Source: Journal of Atmospheric and Oceanic Technology:;1987:;volume( 004 ):;issue: 002:;page 288
    Author(s): Dewey, Richard K.; Crawford, William R.; Gargett, Ann E.; Oakey, Neil S.
    Publisher: American Meteorological Society
    Abstract: A free-falling instrument has been built to measure temperature, salinity and turbulent shear from near surface to within 15 cm of the ocean bottom. A probe guard mounted at the lower end of the instrument protects sensitive ...
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