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    On Forward-in-Time Differencing for Fluids: Stopping Criteria for Iterative Solutions of Anelastic Pressure Equations

    Source: Monthly Weather Review:;1997:;volume( 125 ):;issue: 004::page 647
    Author:
    Smolarkiewicz, Piotr K.
    ,
    Grubis̄ić, Vanda
    ,
    Margolin, Len G.
    DOI: 10.1175/1520-0493(1997)125<0647:OFITDF>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: In this note, the authors address the practical issue of selecting appropriate stopping criteria for iterative solutions to the elliptic pressure equation arising in nonoscillatory, forward-in-time Eulerian and semi-Lagrangian anelastic fluid models. Using the simple computational example of 2D thermal convection in a neutrally stratified Boussinesq fluid, it is shown that (a) converging to the machine precision is not necessary for the overall accuracy and stability of the model, and adversely affects the overall model efficiency; and (b) the semi-Lagrangian model algorithm admits fairly liberal stopping criteria compared to the Eulerian flux-form model, unless the latter is formulated in terms of field perturbations.
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      On Forward-in-Time Differencing for Fluids: Stopping Criteria for Iterative Solutions of Anelastic Pressure Equations

    URI
    http://yetl.yabesh.ir/yetl1/handle/yetl/4203812
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    • Monthly Weather Review

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    contributor authorSmolarkiewicz, Piotr K.
    contributor authorGrubis̄ić, Vanda
    contributor authorMargolin, Len G.
    date accessioned2017-06-09T16:11:14Z
    date available2017-06-09T16:11:14Z
    date copyright1997/04/01
    date issued1997
    identifier issn0027-0644
    identifier otherams-62872.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4203812
    description abstractIn this note, the authors address the practical issue of selecting appropriate stopping criteria for iterative solutions to the elliptic pressure equation arising in nonoscillatory, forward-in-time Eulerian and semi-Lagrangian anelastic fluid models. Using the simple computational example of 2D thermal convection in a neutrally stratified Boussinesq fluid, it is shown that (a) converging to the machine precision is not necessary for the overall accuracy and stability of the model, and adversely affects the overall model efficiency; and (b) the semi-Lagrangian model algorithm admits fairly liberal stopping criteria compared to the Eulerian flux-form model, unless the latter is formulated in terms of field perturbations.
    publisherAmerican Meteorological Society
    titleOn Forward-in-Time Differencing for Fluids: Stopping Criteria for Iterative Solutions of Anelastic Pressure Equations
    typeJournal Paper
    journal volume125
    journal issue4
    journal titleMonthly Weather Review
    identifier doi10.1175/1520-0493(1997)125<0647:OFITDF>2.0.CO;2
    journal fristpage647
    journal lastpage654
    treeMonthly Weather Review:;1997:;volume( 125 ):;issue: 004
    contenttypeFulltext
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