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    Three-Dimensional Scaling and Consistent Truncation of Global Atmospheric Models

    Source: Monthly Weather Review:;1992:;volume( 120 ):;issue: 001::page 131
    Author:
    Ji, Ming
    ,
    Baer, Ferdinand
    DOI: 10.1175/1520-0493(1992)120<0131:TDSACT>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: A three-dimensional scale index based on spherical domain and quasigeostrophic scale analysis indicates a truncation limit of global atmospheric models that includes both horizontal and vertical dimensions. Applying such a scale index, a numerical experiment is designed using a simplified adiabatic version of the National Center for Atmospheric Research (NCAR) Community Climate Model (CCM0B) to examine, incorporating nonlinear dynamics alone, whether an optimal horizontal resolution for a nine-vertical-level (modes) global general circulation model can be achieved. In establishing appropriate vertical modes that can be uniquely scaled and are independent and physically relevant, an optimal distribution of levels, which has been developed, is utilized in the experiment. The experimental results, which consist of a total of 110 individual integrations of the CCM0B with ten initial states for each of six horizontal truncations, appear to agree with the conclusions implied by the above referenced three-dimensional scale index; that is, a consistent horizontal resolution for a nine-vertical-level model should be in the range of triangular truncation T25 to T30 to yield optimal prediction results, considering, however, only the nonlinear dynamical aspect. It should be noted that due to the simplifications and idealizations made to carry out our experiment, additional studies under more realistic atmospheric conditions are necessary and are encouraged based on the results presented herein to further validate the existence of the consistency of three-dimensional model resolutions.
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      Three-Dimensional Scaling and Consistent Truncation of Global Atmospheric Models

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    contributor authorJi, Ming
    contributor authorBaer, Ferdinand
    date accessioned2017-06-09T16:08:37Z
    date available2017-06-09T16:08:37Z
    date copyright1992/01/01
    date issued1992
    identifier issn0027-0644
    identifier otherams-61901.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4202732
    description abstractA three-dimensional scale index based on spherical domain and quasigeostrophic scale analysis indicates a truncation limit of global atmospheric models that includes both horizontal and vertical dimensions. Applying such a scale index, a numerical experiment is designed using a simplified adiabatic version of the National Center for Atmospheric Research (NCAR) Community Climate Model (CCM0B) to examine, incorporating nonlinear dynamics alone, whether an optimal horizontal resolution for a nine-vertical-level (modes) global general circulation model can be achieved. In establishing appropriate vertical modes that can be uniquely scaled and are independent and physically relevant, an optimal distribution of levels, which has been developed, is utilized in the experiment. The experimental results, which consist of a total of 110 individual integrations of the CCM0B with ten initial states for each of six horizontal truncations, appear to agree with the conclusions implied by the above referenced three-dimensional scale index; that is, a consistent horizontal resolution for a nine-vertical-level model should be in the range of triangular truncation T25 to T30 to yield optimal prediction results, considering, however, only the nonlinear dynamical aspect. It should be noted that due to the simplifications and idealizations made to carry out our experiment, additional studies under more realistic atmospheric conditions are necessary and are encouraged based on the results presented herein to further validate the existence of the consistency of three-dimensional model resolutions.
    publisherAmerican Meteorological Society
    titleThree-Dimensional Scaling and Consistent Truncation of Global Atmospheric Models
    typeJournal Paper
    journal volume120
    journal issue1
    journal titleMonthly Weather Review
    identifier doi10.1175/1520-0493(1992)120<0131:TDSACT>2.0.CO;2
    journal fristpage131
    journal lastpage148
    treeMonthly Weather Review:;1992:;volume( 120 ):;issue: 001
    contenttypeFulltext
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