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    Comparison of Thermal Variance Dissipation Rates from Moored and Profiling Instruments at the Equator 

    Source: Journal of Atmospheric and Oceanic Technology:;2012:;volume( 029 ):;issue: 009:;page 1347
    Author(s): Perlin, A.; Moum, J. N.
    Publisher: American Meteorological Society
    Abstract: s a quantitative test of moored mixing measurements using ?pods, a comparison experiment was conducted at 0°, 140°W in October?November 2008. The following three measurement elements were involved: (i) NOAA?s Tropical ...
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    Energy Transport by Nonlinear Internal Waves 

    Source: Journal of Physical Oceanography:;2007:;Volume( 037 ):;issue: 007:;page 1968
    Author(s): Moum, J. N.; Klymak, J. M.; Nash, J. D.; Perlin, A.; Smyth, W. D.
    Publisher: American Meteorological Society
    Abstract: Winter stratification on Oregon?s continental shelf often produces a near-bottom layer of dense fluid that acts as an internal waveguide upon which nonlinear internal waves propagate. Shipboard profiling and bottom lander ...
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    Convectively Driven Mixing in the Bottom Boundary Layer 

    Source: Journal of Physical Oceanography:;2004:;Volume( 034 ):;issue: 010:;page 2189
    Author(s): Moum, J. N.; Perlin, A.; Klymak, J. M.; Levine, M. D.; Boyd, T.; Kosro, P. M.
    Publisher: American Meteorological Society
    Abstract: Closely spaced vertical profiles through the bottom boundary layer over a sloping continental shelf during relaxation from coastal upwelling reveal structure that is consistent with convectively driven mixing. Parcels of ...
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