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    Steady Wind-driven Upwelling in the Presence of a Baroclinic Coastally Trapped Jet 

    Source: Journal of Physical Oceanography:;1986:;Volume( 016 ):;issue: 008:;page 1359
    Author(s): Hay, A. E.; Kinsella, E. D.
    Publisher: American Meteorological Society
    Abstract: The usual two-layer model for steady wind-driven upwelling along a uniform coastline is extended to incorporate the effects of an upper-layer jet trapped against the coast. The characteristic width of the jet is the internal ...
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    A Two-Layer Model of Shelfbreak Jets with Application to the Labrador Current 

    Source: Journal of Physical Oceanography:;2001:;Volume( 031 ):;issue: 002:;page 324
    Author(s): Hukuda, H.; Hay, A. E.; Greatbatch, R. J.
    Publisher: American Meteorological Society
    Abstract: The role played by bottom friction, bottom slope, ? effect, and density mixing in exchange between the shelf and a frontal jet is examined in the light of a two-layer model. The model uses linear dynamics and bottom and ...
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    Laboratory Measurements of Coarse Sediment Bedload Transport Velocity Using a Prototype Wideband Coherent Doppler Profiler (MFDop) 

    Source: Journal of Atmospheric and Oceanic Technology:;2014:;volume( 031 ):;issue: 004:;page 999
    Author(s): Stark, N.; Hay, A. E.; Cheel, R.; Zedel, L.; Barclay, D.
    Publisher: American Meteorological Society
    Abstract: prototype wideband coherent Doppler profiler (MFDop) was tested for measuring bedload velocity of different gravel and coarse-sand-sized fractions (d = 1?32 mm) in the laboratory. The sediment was spread out on a smooth-surface ...
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    A Self-Contained Sector-Scanning Sonar for Bottom Roughness Observations as Part of Sediment Transport Studies 

    Source: Journal of Atmospheric and Oceanic Technology:;1999:;volume( 016 ):;issue: 011:;page 1830
    Author(s): Irish, J. D.; Lynch, J. F.; Traykovski, P. A.; Newhall, A. E.; Prada, K.; Hay, A. E.
    Publisher: American Meteorological Society
    Abstract: Studies and models of sediment transport in the bottom boundary layer require knowledge of the bottom roughness as a parameter affecting the suspension and transport of sediment. Knowledge of this has often been quite ...
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