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    Diagnosing Diapycnal Mixing from Passive Tracers 

    Source: Journal of Physical Oceanography:;2021:;volume( 051 ):;issue: 003:;page 757
    Author(s): Ruan, Xiaozhou;Ferrari, Raffaele
    Publisher: American Meteorological Society
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    On the Pathways of Wind-Driven Coastal Upwelling: Nonlinear Momentum Flux and Baroclinic Instability 

    Source: Journal of Physical Oceanography:;2024:;volume( 054 ):;issue: 001:;page 63
    Author(s): Li, Dou; Ruan, Xiaozhou
    Publisher: American Meteorological Society
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    Bottom Boundary Potential Vorticity Injection from an Oscillating Flow: A PV Pump 

    Source: Journal of Physical Oceanography:;2016:;Volume( 046 ):;issue: 011:;page 3509
    Author(s): Ruan, Xiaozhou; Thompson, Andrew F.
    Publisher: American Meteorological Society
    Abstract: ceanic boundary currents over the continental slope exhibit variability with a range of time scales. Numerical studies of steady, along-slope currents over a sloping bathymetry have shown that cross-slope Ekman transport ...
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    The Evolution and Arrest of a Turbulent Stratified Oceanic Bottom Boundary Layer over a Slope: Upslope Regime and PV Dynamics 

    Source: Journal of Physical Oceanography:;2021:;volume( 051 ):;issue: 004:;page 1077
    Author(s): Ruan, Xiaozhou;Thompson, Andrew F.;Taylor, John R.
    Publisher: American Meteorological Society
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    The Evolution and Arrest of a Turbulent Stratified Oceanic Bottom Boundary Layer over a Slope: Downslope Regime 

    Source: Journal of Physical Oceanography:;2019:;volume( 049 ):;issue: 002:;page 469
    Author(s): Ruan, Xiaozhou;Thompson, Andrew F.;Taylor, John R.
    Publisher: American Meteorological Society
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    The Evolution and Arrest of a Turbulent Stratified Oceanic Bottom Boundary Layer over a Slope: Downslope Regime 

    Source: Journal of Physical Oceanography:;2018:;volume 049:;issue 002:;page 469
    Author(s): Ruan, Xiaozhou; Thompson, Andrew F.; Taylor, John R.
    Publisher: American Meteorological Society
    Abstract: The dynamics of a stratified oceanic bottom boundary layer (BBL) over an insulating, sloping surface depend critically on the intersection of density surfaces with the bottom. For an imposed along-slope flow, the cross-slope ...
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