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    Estimation of Diffusive Transport of Turbulent Kinetic Energy from Acoustic Doppler Current Profiler Data 

    Source: Journal of Atmospheric and Oceanic Technology:;2003:;volume( 020 ):;issue: 006:;page 927
    Author(s): Stacey, Mark T.
    Publisher: American Meteorological Society
    Abstract: The analysis of turbulent mixing has historically relied upon either indirect estimates of turbulent mixing, such as the gradient Richardson number, or measurements of small-scale shear to define turbulent dissipation ...
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    Coupling of Sea Level Rise, Tidal Amplification, and Inundation 

    Source: Journal of Physical Oceanography:;2014:;Volume( 044 ):;issue: 005:;page 1439
    Author(s): Holleman, Rusty C.; Stacey, Mark T.
    Publisher: American Meteorological Society
    Abstract: ith the global sea level rising, it is imperative to quantify how the dynamics of tidal estuaries and embayments will respond to increased depth and newly inundated perimeter regions. With increased depth comes a decrease ...
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    Turbulence Dynamics at the Shoal–Channel Interface in a Partially Stratified Estuary 

    Source: Journal of Physical Oceanography:;2013:;Volume( 043 ):;issue: 005:;page 970
    Author(s): Collignon, Audric G.; Stacey, Mark T.
    Publisher: American Meteorological Society
    Abstract: urbulence observations at the shoal?channel interface in South San Francisco Bay are described and analyzed in this work. Profiles of turbulent kinetic energy (TKE) shear production and dissipation rate are estimated from ...
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    Intratidal Dynamics of Fronts and Lateral Circulation at the Shoal–Channel Interface in a Partially Stratified Estuary 

    Source: Journal of Physical Oceanography:;2012:;Volume( 042 ):;issue: 005:;page 869
    Author(s): Collignon, Audric G.; Stacey, Mark T.
    Publisher: American Meteorological Society
    Abstract: n partially stratified shoal?channel estuaries, variations in bathymetry at the shoal?channel interface generate horizontal shears and density gradients, and foam lines characteristic of convergence fronts are frequently ...
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    The Scaling and Structure of the Estuarine Bottom Boundary Layer 

    Source: Journal of Physical Oceanography:;2005:;Volume( 035 ):;issue: 001:;page 55
    Author(s): Stacey, Mark T.; Ralston, David K.
    Publisher: American Meteorological Society
    Abstract: A two-week dataset from a partially and periodically stratified estuary quantifies variability in the turbulence across the tidal and spring?neap time scales. These observations have been fit with a two-parameter model of ...
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    Observations of Turbulence in a Partially Stratified Estuary 

    Source: Journal of Physical Oceanography:;1999:;Volume( 029 ):;issue: 008:;page 1950
    Author(s): Stacey, Mark T.; Monismith, Stephen G.; Burau, Jon R.
    Publisher: American Meteorological Society
    Abstract: The authors present a field study of estuarine turbulence in which profiles of Reynolds stresses were directly measured using an ADCP throughout a 25-h tidal day. The dataset that is discussed quantifies turbulent mixing ...
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    Dispersive Fluxes between the Coastal Ocean and a Semienclosed Estuarine Basin 

    Source: Journal of Physical Oceanography:;2007:;Volume( 037 ):;issue: 006:;page 1645
    Author(s): Fram, Jonathan P.; Martin, Maureen A.; Stacey, Mark T.
    Publisher: American Meteorological Society
    Abstract: Scalar exchange between San Francisco Bay and the coastal ocean is examined using shipboard observations made across the Golden Gate Channel. The study consists of experiments during each of the following three ?seasons?: ...
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    Lateral Circulation Generates Flood Tide Stratification and Estuarine Exchange Flow in a Curved Tidal Inlet 

    Source: Journal of Physical Oceanography:;2014:;Volume( 045 ):;issue: 003:;page 638
    Author(s): Becherer, Johannes; Stacey, Mark T.; Umlauf, Lars; Burchard, Hans
    Publisher: American Meteorological Society
    Abstract: ross-channel transect measurements of microstructure and velocity in a well-mixed and curved tidal inlet in the German Wadden Sea show the occurrence of significant late flood stratification. This stratification is found ...
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    An Evaluation of χT Estimation Techniques: Implications for Batchelor Fitting and ε 

    Source: Journal of Atmospheric and Oceanic Technology:;2009:;volume( 026 ):;issue: 008:;page 1652
    Author(s): Steinbuck, Jonah V.; Stacey, Mark T.; Monismith, Stephen G.
    Publisher: American Meteorological Society
    Abstract: Techniques for the accurate estimation of the dissipation rate of temperature variance ?T from temperature microstructure measurements are synthesized and evaluated. The techniques focus on the treatment of contamination ...
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    Using Depth-Normalized Coordinates to Examine Mass Transport Residual Circulation in Estuaries with Large Tidal Amplitude Relative to the Mean Depth 

    Source: Journal of Physical Oceanography:;2013:;Volume( 044 ):;issue: 001:;page 128
    Author(s): Giddings, Sarah N.; Monismith, Stephen G.; Fong, Derek A.; Stacey, Mark T.
    Publisher: American Meteorological Society
    Abstract: esidual (subtidal) circulation profiles in estuaries with a large tidal amplitude-to-depth ratio often are quite complex and do not resemble the traditional estuarine gravitational circulation profile. This paper describes ...
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