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    Estuarine Adjustment 

    Source: Journal of Physical Oceanography:;2007:;Volume( 037 ):;issue: 008:;page 2133
    Author(s): MacCready, Parker
    Publisher: American Meteorological Society
    Abstract: Subtidal adjustment of estuarine salinity and circulation to changing river flow or tidal mixing is explored using a simplified numerical model. The model employs tidally averaged, width-averaged physics, following Hansen ...
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    Calculating Estuarine Exchange Flow Using Isohaline Coordinates 

    Source: Journal of Physical Oceanography:;2011:;Volume( 041 ):;issue: 006:;page 1116
    Author(s): MacCready, Parker
    Publisher: American Meteorological Society
    Abstract: method for calculating subtidal estuarine exchange flow using an isohaline framework is described, and the results are compared with those of the more commonly used Eulerian method of salt flux decomposition. Concepts are ...
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    Estuarine Adjustment to Changes in River Flow and Tidal Mixing 

    Source: Journal of Physical Oceanography:;1999:;Volume( 029 ):;issue: 004:;page 708
    Author(s): MacCready, Parker
    Publisher: American Meteorological Society
    Abstract: The adjustment of estuarine circulation and density to changes in river flow and tidal mixing is investigated using analytical and numerical models. Tidally averaged momentum and salinity equations in a rectangular estuary ...
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    Stratified Flow along a Corrugated Slope: Separation Drag and Wave Drag 

    Source: Journal of Physical Oceanography:;2001:;Volume( 031 ):;issue: 010:;page 2824
    Author(s): MacCready, Parker; Pawlak, Geno
    Publisher: American Meteorological Society
    Abstract: Lee wave generation and horizontal flow separation in stratified flow along a slope, with corrugations or a ridge running directly downslope, are explored using analytical and numerical methods. Both of these processes are ...
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    The Shelf Sources of Estuarine Inflow 

    Source: Journal of Physical Oceanography:;2021:;volume( 051 ):;issue: 007:;page 2407
    Author(s): Brasseale, Elizabeth;MacCready, Parker
    Publisher: American Meteorological Society
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    Slippery Bottom Boundary Layers on a Slope 

    Source: Journal of Physical Oceanography:;1993:;Volume( 023 ):;issue: 001:;page 5
    Author(s): MacCready, Parker; Rhines, Peter B.
    Publisher: American Meteorological Society
    Abstract: The turbulent bottom boundary layer for rotating, stratified flow along a slope is explored through theory and numerical simulation. The model flow begins with a uniform current along constant-depth contours and with flat ...
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    Tilted Baroclinic Tidal Vortices 

    Source: Journal of Physical Oceanography:;2009:;Volume( 039 ):;issue: 002:;page 333
    Author(s): Canals, Miguel; Pawlak, Geno; MacCready, Parker
    Publisher: American Meteorological Society
    Abstract: The structure of baroclinic vortices generated by horizontal flow separation past a sloping headland in deep, stably stratified waters is investigated. The most distinctive feature of these eddies is that their cores are ...
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    The Mechanical Energy Budget of a Regional Ocean Model 

    Source: Journal of Physical Oceanography:;2016:;Volume( 046 ):;issue: 009:;page 2719
    Author(s): MacCready, Parker; Giddings, Sarah N.
    Publisher: American Meteorological Society
    Abstract: method is presented for calculating a complete, numerically closed, mechanical energy budget in a realistic simulation of circulation in a coastal?estuarine domain. The budget is formulated in terms of the ?local? available ...
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    Meridional Transport across a Zonal Channel: Topographic Localization 

    Source: Journal of Physical Oceanography:;2001:;Volume( 031 ):;issue: 006:;page 1427
    Author(s): MacCready, Parker; Rhines, Peter B.
    Publisher: American Meteorological Society
    Abstract: Experiments are performed using a two-layer isopycnic numerical model in a zonal channel with a large meridional topographic ridge in the lower layer. The model is forced only by a steady meridional volume transport in the ...
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    Boundary Layer Forcing of a Semidiurnal, Cross-Channel Seiche 

    Source: Journal of Physical Oceanography:;2005:;Volume( 035 ):;issue: 009:;page 1518
    Author(s): Martin, Wayne; MacCready, Parker; Dewey, Richard
    Publisher: American Meteorological Society
    Abstract: The outer Strait of Juan de Fuca is a stratified, tidal channel about 100 km long, 20 km wide, and 200 m deep. Tidal currents of O(0.5 m s?1) occur at both diurnal and semidiurnal periods and there is a pronounced spring?neap ...
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