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    The Community Climate System Model, Version 2

    Source: Journal of Climate:;2004:;volume( 017 ):;issue: 019::page 3666
    Author:
    Kiehl, Jeffrey T.
    ,
    Gent, Peter R.
    DOI: 10.1175/1520-0442(2004)017<3666:TCCSMV>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: The Community Climate System Model, version 2 (CCSM2) is briefly described. A 1000-yr control simulation of the present day climate has been completed without flux adjustments. Minor modifications were made at year 350, which included all five components using the same physical constants. There are very small trends in the upper-ocean, sea ice, atmosphere, and land fields after year 150 of the control simulation. The deep ocean has small but significant trends; however, these are not large enough that the control simulation could not be continued much further. The equilibrium climate sensitivity of CCSM2 is 2.2 K, which is slightly larger than the Climate System Model, version 1 (CSM1) value of 2.0 K. Several aspects of the control simulation's mean climate and interannual variability are described, and good and bad properties of the control simulation are documented. In particular, several aspects of the simulation, especially in the Arctic region, are much improved over those obtained in CSM1. Other aspects, such as the tropical Pacific region simulation, have not been improved much compared to those in CSM1. Priorities for further model development are discussed in the conclusions section.
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      The Community Climate System Model, Version 2

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4208645
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    contributor authorKiehl, Jeffrey T.
    contributor authorGent, Peter R.
    date accessioned2017-06-09T16:24:09Z
    date available2017-06-09T16:24:09Z
    date copyright2004/10/01
    date issued2004
    identifier issn0894-8755
    identifier otherams-6722.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4208645
    description abstractThe Community Climate System Model, version 2 (CCSM2) is briefly described. A 1000-yr control simulation of the present day climate has been completed without flux adjustments. Minor modifications were made at year 350, which included all five components using the same physical constants. There are very small trends in the upper-ocean, sea ice, atmosphere, and land fields after year 150 of the control simulation. The deep ocean has small but significant trends; however, these are not large enough that the control simulation could not be continued much further. The equilibrium climate sensitivity of CCSM2 is 2.2 K, which is slightly larger than the Climate System Model, version 1 (CSM1) value of 2.0 K. Several aspects of the control simulation's mean climate and interannual variability are described, and good and bad properties of the control simulation are documented. In particular, several aspects of the simulation, especially in the Arctic region, are much improved over those obtained in CSM1. Other aspects, such as the tropical Pacific region simulation, have not been improved much compared to those in CSM1. Priorities for further model development are discussed in the conclusions section.
    publisherAmerican Meteorological Society
    titleThe Community Climate System Model, Version 2
    typeJournal Paper
    journal volume17
    journal issue19
    journal titleJournal of Climate
    identifier doi10.1175/1520-0442(2004)017<3666:TCCSMV>2.0.CO;2
    journal fristpage3666
    journal lastpage3682
    treeJournal of Climate:;2004:;volume( 017 ):;issue: 019
    contenttypeFulltext
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    DSpace software copyright © 2002-2015  DuraSpace
    نرم افزار کتابخانه دیجیتال "دی اسپیس" فارسی شده توسط یابش برای کتابخانه های ایرانی | تماس با یابش
    yabeshDSpacePersian