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    Trajectories and Speeds of Wind-Driven Currents Wear the Coast 

    Source: Journal of Physical Oceanography:;1975:;Volume( 005 ):;issue: 002:;page 347
    Author(s): Murray, Stephen P.
    Publisher: American Meteorological Society
    Abstract: Detailed observation of drogue movements within 800 m of a straight shoreline indicates the primary current generated by local winds to be directed within a few degrees of parallel to the shore nearly independently of wind ...
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    Inertial Currents Over the Inner Shelf Near 30°N 

    Source: Journal of Physical Oceanography:;1978:;Volume( 008 ):;issue: 004:;page 728
    Author(s): Daddio, Ernest; Wiseman, Wm J.; Murray, Stephen P.
    Publisher: American Meteorological Society
    Abstract: Analysis of two month-long current records, one in February and one in May, from the inner shelf (28.9°N) west of the Mississippi River delta show strong oscillations in the diurnal-inertial frequency band. Lack of correlation ...
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    Hydraulic Interpretation of Direct Velocity Measurements in the Bab al Mandab 

    Source: Journal of Physical Oceanography:;1999:;Volume( 029 ):;issue: 011:;page 2769
    Author(s): Pratt, L. J.; Johns, William; Murray, Stephen P.; Katsumata, Katsurou
    Publisher: American Meteorological Society
    Abstract: Acoustic Doppler Current Profiler velocity measurements in the Bab al Mandab during the period June 1995?March 1996 are used to assess the hydraulic character of the exchange flow. The strait is 150 km long and contains ...
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    Continuous Dynamical Modes in Straits Having Arbitrary Cross Sections, with Applications to the Bab al Mandab 

    Source: Journal of Physical Oceanography:;2000:;Volume( 030 ):;issue: 010:;page 2515
    Author(s): Pratt, Larry J.; Deese, Heather E.; Murray, Stephen P.; Johns, William
    Publisher: American Meteorological Society
    Abstract: The continuous dynamical modes of the exchange flow in the Bab al Mandab are computed in an attempt to assess the hydraulic character of the flow at the sill. First, an extended version of the Taylor?Goldstein equation for ...
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