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    The Low-Frequency Residual Circulation in Knight Inlet, British Columbia 

    Source: Journal of Physical Oceanography:;1995:;Volume( 025 ):;issue: 005:;page 747
    Author(s): Baker, Peter; Pond, Stephen
    Publisher: American Meteorological Society
    Abstract: Many aspects Of the low-frequency response of a stratified inlet have not been previously observed because of the lack of simultaneous observations of runoff, wind, currents, and density over the entire body of water. ...
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    On the Mellor–Yamada Turbulence Closure Scheme: The Surface Boundary Condition for q2 

    Source: Journal of Physical Oceanography:;1997:;Volume( 027 ):;issue: 010:;page 2081
    Author(s): Stacey, Michael W.; Pond, Stephen
    Publisher: American Meteorological Society
    Abstract: A numerical model that uses a level-2½ turbulence closure scheme is used to compare two boundary conditions for the turbulent energy at the air?sea interface. One boundary condition, the most commonly used, sets the turbulent ...
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    Tidal Energy Dissipation at the Sill of Sechelt Inlet, British Columbia 

    Source: Journal of Physical Oceanography:;2001:;Volume( 031 ):;issue: 012:;page 3365
    Author(s): Tinis, Scott W.; Pond, Stephen
    Publisher: American Meteorological Society
    Abstract: The energy budget of a tidally active, shallow silled fjord is discussed. Constriction of the flow over the shallow sill causes a reduction in tidal amplitude and a phase lag across the sill. A generalized expression for ...
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    A Numerical Model of the Circulation in Knight Inlet, British Columbia, Canada 

    Source: Journal of Physical Oceanography:;1995:;Volume( 025 ):;issue: 006:;page 1037
    Author(s): Stacey, Michael W.; Pond, Stephen; Nowak, Zenon P.
    Publisher: American Meteorological Society
    Abstract: During spring 1988 (a period of low freshwater runoff) and summer 1989 (a period of high freshwater runoff), month-long observations of velocity, temperature, and salinity were made throughout the water column in Knight ...
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    Note on the Kinetic Energy Spectrum of Coastal Winds 

    Source: Monthly Weather Review:;1972:;volume( 100 ):;issue: 009:;page 671
    Author(s): FRYE, DANIEL E.; POND, STEPHEN; ELLIOTT, WILLIAM P.
    Publisher: American Meteorological Society
    Abstract: An examination of the spectrum of winds along the Oregon coast shows a major diurnal peak at a period of 24 hr and a small microscale peak at about 50 s. The 24-hr peak is thought to be associated with the diurnal variation ...
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    An Analysis of the Low-Frequency Current Fluctuations in the Strait of Georgia, from June 1984 until January 1985 

    Source: Journal of Physical Oceanography:;1987:;Volume( 017 ):;issue: 003:;page 326
    Author(s): Stacey, Michael W.; Pond, Stephen; LeBlond, Paul H.; Freeland, Howard J.; Farmer, David M.
    Publisher: American Meteorological Society
    Abstract: A description of the low-frequency (ap;10 to 30 days period) current fluctuations in the Strait of Georgia is presented. Velocity time series from four cyclesonde moorings and five current meter mooring, spanning the time ...
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