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    Monotone Advection on the Sphere: An Eulerian Versus Semi-Lagrangian Approach

    Source: Journal of the Atmospheric Sciences:;1991:;Volume( 048 ):;issue: 006::page 793
    Author:
    Smolarkiewicz, Piotr K.
    ,
    Rasch, Philip J.
    DOI: 10.1175/1520-0469(1991)048<0793:MAOTSA>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: The purpose of this paper is twofold. First, a formalism is presented that extends the conceptual framework identified by Ritchie as the ?semi-Lagrangian method without interpolation.? While his words for this concept refer to a particular class of semi-Lagrangian approximations, the idea is actually much more general. The formalism may be used to convert any advection algorithm into the semi-Lagrangian format, and it makes most algorithms sufficient for the integration of flows characterized by large Courant numbers. The formalism is presented in an arbitrary curvilinear system of coordinates. Second, exploiting the generality of the theoretical considerations, the formalism is implemented in solving a practical problem of scalar advection in spherical geometry. Rather than elaborating on Ritchie's semi-Lagrangian techniques employing centered-in-time differencing, the focus is on the alternative of forward-in-time, dissipative finite-difference schemes. This class of schemes offers attractive computational properties in terms of the solutions' accuracy and preservation of a sign or monotonicity.
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      Monotone Advection on the Sphere: An Eulerian Versus Semi-Lagrangian Approach

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4156737
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    contributor authorSmolarkiewicz, Piotr K.
    contributor authorRasch, Philip J.
    date accessioned2017-06-09T14:30:15Z
    date available2017-06-09T14:30:15Z
    date copyright1991/03/01
    date issued1991
    identifier issn0022-4928
    identifier otherams-20501.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4156737
    description abstractThe purpose of this paper is twofold. First, a formalism is presented that extends the conceptual framework identified by Ritchie as the ?semi-Lagrangian method without interpolation.? While his words for this concept refer to a particular class of semi-Lagrangian approximations, the idea is actually much more general. The formalism may be used to convert any advection algorithm into the semi-Lagrangian format, and it makes most algorithms sufficient for the integration of flows characterized by large Courant numbers. The formalism is presented in an arbitrary curvilinear system of coordinates. Second, exploiting the generality of the theoretical considerations, the formalism is implemented in solving a practical problem of scalar advection in spherical geometry. Rather than elaborating on Ritchie's semi-Lagrangian techniques employing centered-in-time differencing, the focus is on the alternative of forward-in-time, dissipative finite-difference schemes. This class of schemes offers attractive computational properties in terms of the solutions' accuracy and preservation of a sign or monotonicity.
    publisherAmerican Meteorological Society
    titleMonotone Advection on the Sphere: An Eulerian Versus Semi-Lagrangian Approach
    typeJournal Paper
    journal volume48
    journal issue6
    journal titleJournal of the Atmospheric Sciences
    identifier doi10.1175/1520-0469(1991)048<0793:MAOTSA>2.0.CO;2
    journal fristpage793
    journal lastpage810
    treeJournal of the Atmospheric Sciences:;1991:;Volume( 048 ):;issue: 006
    contenttypeFulltext
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    DSpace software copyright © 2002-2015  DuraSpace
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