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    Microstructure Estimates of Turbulent Salinity Flux and the Dissipation Spectrum of Salinity 

    Source: Journal of Physical Oceanography:;2002:;Volume( 032 ):;issue: 008:;page 2312
    Author(s): Nash, Jonathan D.; Moum, James N.
    Publisher: American Meteorological Society
    Abstract: Direct determination of the irreversible turbulent flux of salinity in the ocean has not been possible because of the complexity of measuring salinity on the smallest scales over which it mixes. Presented is an analysis ...
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    Estimating Salinity Variance Dissipation Rate from Conductivity Microstructure Measurements 

    Source: Journal of Atmospheric and Oceanic Technology:;1999:;volume( 016 ):;issue: 002:;page 263
    Author(s): Nash, Jonathan D.; Moum, James N.
    Publisher: American Meteorological Society
    Abstract: At the smallest length scales, conductivity measurements include a contribution from salinity fluctuations in the inertial?convective and viscous?diffusive ranges of the turbulent scalar variance spectrum. Interpreting ...
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    Estimating Internal Wave Energy Fluxes in the Ocean 

    Source: Journal of Atmospheric and Oceanic Technology:;2005:;volume( 022 ):;issue: 010:;page 1551
    Author(s): Nash, Jonathan D.; Alford, Matthew H.; Kunze, Eric
    Publisher: American Meteorological Society
    Abstract: Energy flux is a fundamental quantity for understanding internal wave generation, propagation, and dissipation. In this paper, the estimation of internal wave energy fluxes ?u?p?? from ocean observations that may be sparse ...
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    A Coupled Model for Laplace's Tidal Equations in a Fluid with One Horizontal Dimension and Variable Depth 

    Source: Journal of Physical Oceanography:;2013:;Volume( 043 ):;issue: 008:;page 1780
    Author(s): Kelly, Samuel M.; Jones, Nicole L.; Nash, Jonathan D.
    Publisher: American Meteorological Society
    Abstract: ide?topography interactions dominate the transfer of tidal energy from large to small scales. At present, it is poorly understood how low-mode internal tides reflect and scatter along the continental margins. Here, the ...
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    The Cascade of Tidal Energy from Low to High Modes on a Continental Slope 

    Source: Journal of Physical Oceanography:;2012:;Volume( 042 ):;issue: 007:;page 1217
    Author(s): Kelly, Samuel M.; Nash, Jonathan D.; Martini, Kim I.; Alford, Matthew H.; Kunze, Eric
    Publisher: American Meteorological Society
    Abstract: he linear transfer of tidal energy from large to small scales is quantified for small tidal excursion over a near-critical continental slope. A theoretical framework for low-wavenumber energy transfer is derived from ?flat ...
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    Measurement of Tidal Form Drag Using Seafloor Pressure Sensors 

    Source: Journal of Physical Oceanography:;2013:;Volume( 043 ):;issue: 006:;page 1150
    Author(s): Warner, Sally J.; MacCready, Parker; Moum, James N.; Nash, Jonathan D.
    Publisher: American Meteorological Society
    Abstract: s currents flow over rough topography, the pressure difference between the up- and downstream sides results in form drag?a force that opposes the flow. Measuring form drag is valuable because it can be used to estimate the ...
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    The Unpredictable Nature of Internal Tides on Continental Shelves 

    Source: Journal of Physical Oceanography:;2012:;Volume( 042 ):;issue: 011:;page 1981
    Author(s): Nash, Jonathan D.; Kelly, Samuel M.; Shroyer, Emily L.; Moum, James N.; Duda, Timothy F.
    Publisher: American Meteorological Society
    Abstract: ackets of nonlinear internal waves (NLIWs) in a small area of the Mid-Atlantic Bight were 10 times more energetic during a local neap tide than during the preceding spring tide. This counterintuitive result cannot be ...
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    Internal Bores and Breaking Internal Tides on the Oregon Continental Slope 

    Source: Journal of Physical Oceanography:;2012:;Volume( 043 ):;issue: 001:;page 120
    Author(s): Martini, Kim I.; Alford, Matthew H.; Kunze, Eric; Kelly, Samuel M.; Nash, Jonathan D.
    Publisher: American Meteorological Society
    Abstract: bservations of breaking internal tides on the Oregon continental slope during a 40-day deployment of 5 moorings along 43°12?N are presented. Remotely generated internal tides shoal onto the slope, steepen, break, and form ...
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    Controls on Turbulent Mixing in a Strongly Stratified and Sheared Tidal River Plume 

    Source: Journal of Physical Oceanography:;2016:;Volume( 046 ):;issue: 008:;page 2373
    Author(s): Jurisa, Joseph T.; Nash, Jonathan D.; Moum, James N.; Kilcher, Levi F.
    Publisher: American Meteorological Society
    Abstract: onsiderable effort has been made to parameterize turbulent kinetic energy (TKE) dissipation rate ε and mixing in buoyant plumes and stratified shear flows. Here, a parameterization based on Kunze et al. is examined, which ...
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    A Thermocouple Probe for High-Speed Temperature Measurement in the Ocean 

    Source: Journal of Atmospheric and Oceanic Technology:;1999:;volume( 016 ):;issue: 011:;page 1474
    Author(s): Nash, Jonathan D.; Caldwell, Douglas R.; Zelman, Michael J.; Moum, James N.
    Publisher: American Meteorological Society
    Abstract: A fast-response chromel?constantan thermocouple sensor was constructed for use on the microstructure profiler Chameleon and used for 60 ocean profiles off the coast of Oregon. The stability of the thermocouple was compared ...
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