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    Latitude-Longitude Grid Suitable for Numerical Time Integration of a Global Atmospheric Model

    Source: Monthly Weather Review:;1973:;volume( 101 ):;issue: 001::page 69
    Author:
    HOLLOWAY, J. LEITH
    ,
    SPELMAN, MICHAEL J.
    ,
    MANABE, SYUKURO
    DOI: 10.1175/1520-0493(1973)101<0069:LGSFNT>2.3.CO;2
    Publisher: American Meteorological Society
    Abstract: A simple, free-surface, barotropic model and a nine-level, baroclinic model are numerically time integrated on both latitude-longitude grids and on Kurihara-type grids to compare the results obtained from the two grid systems. The prognostic variables are Fourier space-filtered in the longitudinal direction on the latitude-longitude grids to permit the use of the same time-step length on both grids. With respect to geopotential height and zonal wind distributions and to the phase speed of wave propagation, the results from the barotropic model, time-integrated on a sector latitude-longitude grid, agree better with a high-resolution control run than those computed on a modified Kurihara grid, particularly at high latitudes. The barotropic model is also time-integrated on a hemispheric, latitude-longitude grid, and the results compare well with a high-resolution control. The latter comparison is performed on initial data having strong cross-polar flow. The mean sea-level pressure distribution obtained from a 64-day time integration of the baroclinic model on a global, latitude-longitude grid is better than that derived from a similar model using a Kurihara grid of comparable resolution. For example, the tendency for the Kurihara grid model to predict excessive pressures in the north polar region is for the most part corrected by use of the latitude-longitude grid.
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      Latitude-Longitude Grid Suitable for Numerical Time Integration of a Global Atmospheric Model

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4198961
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    contributor authorHOLLOWAY, J. LEITH
    contributor authorSPELMAN, MICHAEL J.
    contributor authorMANABE, SYUKURO
    date accessioned2017-06-09T16:00:10Z
    date available2017-06-09T16:00:10Z
    date copyright1973/01/01
    date issued1973
    identifier issn0027-0644
    identifier otherams-58506.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4198961
    description abstractA simple, free-surface, barotropic model and a nine-level, baroclinic model are numerically time integrated on both latitude-longitude grids and on Kurihara-type grids to compare the results obtained from the two grid systems. The prognostic variables are Fourier space-filtered in the longitudinal direction on the latitude-longitude grids to permit the use of the same time-step length on both grids. With respect to geopotential height and zonal wind distributions and to the phase speed of wave propagation, the results from the barotropic model, time-integrated on a sector latitude-longitude grid, agree better with a high-resolution control run than those computed on a modified Kurihara grid, particularly at high latitudes. The barotropic model is also time-integrated on a hemispheric, latitude-longitude grid, and the results compare well with a high-resolution control. The latter comparison is performed on initial data having strong cross-polar flow. The mean sea-level pressure distribution obtained from a 64-day time integration of the baroclinic model on a global, latitude-longitude grid is better than that derived from a similar model using a Kurihara grid of comparable resolution. For example, the tendency for the Kurihara grid model to predict excessive pressures in the north polar region is for the most part corrected by use of the latitude-longitude grid.
    publisherAmerican Meteorological Society
    titleLatitude-Longitude Grid Suitable for Numerical Time Integration of a Global Atmospheric Model
    typeJournal Paper
    journal volume101
    journal issue1
    journal titleMonthly Weather Review
    identifier doi10.1175/1520-0493(1973)101<0069:LGSFNT>2.3.CO;2
    journal fristpage69
    journal lastpage78
    treeMonthly Weather Review:;1973:;volume( 101 ):;issue: 001
    contenttypeFulltext
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