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    A Simple Approximate Method of Stochastic-Dynamic Prediction for Small Initial Errors and Short Range

    Source: Monthly Weather Review:;1986:;volume( 114 ):;issue: 009::page 1709
    Author:
    Thompson, Philip D.
    DOI: 10.1175/1520-0493(1986)114<1709:ASAMOS>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: Starting with the vorticity equation for barotropic flow, we derive a system of stochastic differential equations that determines the time-evolution of the local variance of vorticity error originating in a large ensemble of initial states containing random and statistically isotropic initial errors. Those equations show that the local growth or decay of error variance depends primarily on the detailed structure of the true vorticity field; in general, the most rapid growth of error can be expected in concentrated regions of strong vorticity gradient. Those stochastic differential equations provide the basis for a simple method of stochastic-dynamic prediction. It requires only a modest increase over the total volume of computation for deterministic prediction.
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      A Simple Approximate Method of Stochastic-Dynamic Prediction for Small Initial Errors and Short Range

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    https://yetl.yabesh.ir/yetl1/handle/yetl/4201601
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    contributor authorThompson, Philip D.
    date accessioned2017-06-09T16:05:55Z
    date available2017-06-09T16:05:55Z
    date copyright1986/09/01
    date issued1986
    identifier issn0027-0644
    identifier otherams-60882.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4201601
    description abstractStarting with the vorticity equation for barotropic flow, we derive a system of stochastic differential equations that determines the time-evolution of the local variance of vorticity error originating in a large ensemble of initial states containing random and statistically isotropic initial errors. Those equations show that the local growth or decay of error variance depends primarily on the detailed structure of the true vorticity field; in general, the most rapid growth of error can be expected in concentrated regions of strong vorticity gradient. Those stochastic differential equations provide the basis for a simple method of stochastic-dynamic prediction. It requires only a modest increase over the total volume of computation for deterministic prediction.
    publisherAmerican Meteorological Society
    titleA Simple Approximate Method of Stochastic-Dynamic Prediction for Small Initial Errors and Short Range
    typeJournal Paper
    journal volume114
    journal issue9
    journal titleMonthly Weather Review
    identifier doi10.1175/1520-0493(1986)114<1709:ASAMOS>2.0.CO;2
    journal fristpage1709
    journal lastpage1715
    treeMonthly Weather Review:;1986:;volume( 114 ):;issue: 009
    contenttypeFulltext
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    DSpace software copyright © 2002-2015  DuraSpace
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