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    Comment on “A Positive Definite Advection Scheme Obtained by Nonlinear Renormalization of the Advective Fluxes” 

    Source: Monthly Weather Review:;1989:;volume( 117 ):;issue: 011:;page 2626
    Author(s): Smolarkiewicz, Piotr K.
    Publisher: American Meteorological Society
    Abstract: No abstract available.
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    The Multi-Dimensional Crowley Advection Scheme 

    Source: Monthly Weather Review:;1982:;volume( 110 ):;issue: 012:;page 1968
    Author(s): Smolarkiewicz, Piotr K.
    Publisher: American Meteorological Society
    Abstract: The conservation form of the second-order Crowley advection scheme, as some authors have pointed out, may lead to numerical instability for multi-dimensional blows. Replacing the original second-order-accurate approximation ...
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    A Simple Positive Definite Advection Scheme with Small Implicit Diffusion 

    Source: Monthly Weather Review:;1983:;volume( 111 ):;issue: 003:;page 479
    Author(s): Smolarkiewicz, Piotr K.
    Publisher: American Meteorological Society
    Abstract: The development of negative values for positive definite scalars in the solution of the advection equation is an important difficulty in numerical modeling. This paper proposes a new positively definite advection scheme ...
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    On the Accuracy of the Crowley Advection Scheme 

    Source: Monthly Weather Review:;1985:;volume( 113 ):;issue: 008:;page 1425
    Author(s): Smolarkiewicz, Piotr K.
    Publisher: American Meteorological Society
    Abstract: The purpose of this note is to show that the popular Crowley advection scheme, which is usually considered to have first-order accuracy in time for a nonuniform velocity field, can be constructed so as to have second-order ...
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    Reply 

    Source: Monthly Weather Review:;1987:;volume( 115 ):;issue: 004:;page 901
    Author(s): Smolarkiewicz, Piotr K.
    Publisher: American Meteorological Society
    Abstract: No abstract available.
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    On Forward-in-Time Differencing for Fluids 

    Source: Monthly Weather Review:;1991:;volume( 119 ):;issue: 010:;page 2505
    Author(s): Smolarkiewicz, Piotr K.
    Publisher: American Meteorological Society
    Abstract: This note discusses the extension of the dissipative advection schemes, often referred to in meteorological literature as Crowley-type schemes, on advection equations with arbitrary forcing and/or source terms included. ...
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    Low Froude Number Flow Past Three-Dimensional Obstacles. Part I: Baroclinically Generated Lee Vortices 

    Source: Journal of the Atmospheric Sciences:;1988:;Volume( 046 ):;issue: 008:;page 1154
    Author(s): Smolarkiewicz, Piotr K.; Rotunno, Richard
    Publisher: American Meteorological Society
    Abstract: We study the flow of a density-stratified fluid past a three-dimensional obstacle, using a numerical model. Our special concern is the response of the fluid when the Froude number is near or less than unity. Linear theory ...
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    Low Froude Number Flow Past Three-Dimensional Obstacles. Part II: Upwind Flow Reversal Zone 

    Source: Journal of the Atmospheric Sciences:;1989:;Volume( 047 ):;issue: 012:;page 1498
    Author(s): Smolarkiewicz, Piotr K.; Rotunno, Richard
    Publisher: American Meteorological Society
    Abstract: The present paper contains a continuation of our study of the flow of a density-stratified fluid past three-dimensional obstacles for Froude number ?O(1). Linear theory (large Froude number) and potential-flow-type theory ...
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    Reply 

    Source: Journal of the Atmospheric Sciences:;1988:;Volume( 046 ):;issue: 023:;page 3614
    Author(s): Smolarkiewicz, Piotr K.; Rotunno, Richard
    Publisher: American Meteorological Society
    Abstract: No abstract available.
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    Vorticity Generation in the Shallow-Water Equations as Applied to Hydraulic Jumps 

    Source: Journal of the Atmospheric Sciences:;1995:;Volume( 052 ):;issue: 003:;page 320
    Author(s): Rotunno, Richard; Smolarkiewicz, Piotr K.
    Publisher: American Meteorological Society
    Abstract: The authors attempt to find a bridge between the vorticity dynamics of a finite cross-stream length hydraulic jump implied by the Navier-Stokes equations and that given by the shallow-water approximation (SWA) with the ...
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