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    Global Climate Model Performance over Alaska and Greenland

    Source: Journal of Climate:;2008:;volume( 021 ):;issue: 023::page 6156
    Author:
    Walsh, John E.
    ,
    Chapman, William L.
    ,
    Romanovsky, Vladimir
    ,
    Christensen, Jens H.
    ,
    Stendel, Martin
    DOI: 10.1175/2008JCLI2163.1
    Publisher: American Meteorological Society
    Abstract: The performance of a set of 15 global climate models used in the Coupled Model Intercomparison Project is evaluated for Alaska and Greenland, and compared with the performance over broader pan-Arctic and Northern Hemisphere extratropical domains. Root-mean-square errors relative to the 1958?2000 climatology of the 40-yr ECMWF Re-Analysis (ERA-40) are summed over the seasonal cycles of three variables: surface air temperature, precipitation, and sea level pressure. The specific models that perform best over the larger domains tend to be the ones that perform best over Alaska and Greenland. The rankings of the models are largely unchanged when the bias of each model?s climatological annual mean is removed prior to the error calculation for the individual models. The annual mean biases typically account for about half of the models? root-mean-square errors. However, the root-mean-square errors of the models are generally much larger than the biases of the composite output, indicating that the systematic errors differ considerably among the models. There is a tendency for the models with smaller errors to simulate a larger greenhouse warming over the Arctic, as well as larger increases of Arctic precipitation and decreases of Arctic sea level pressure, when greenhouse gas concentrations are increased. Because several models have substantially smaller systematic errors than the other models, the differences in greenhouse projections imply that the choice of a subset of models may offer a viable approach to narrowing the uncertainty and obtaining more robust estimates of future climate change in regions such as Alaska, Greenland, and the broader Arctic.
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      Global Climate Model Performance over Alaska and Greenland

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    contributor authorWalsh, John E.
    contributor authorChapman, William L.
    contributor authorRomanovsky, Vladimir
    contributor authorChristensen, Jens H.
    contributor authorStendel, Martin
    date accessioned2017-06-09T16:23:34Z
    date available2017-06-09T16:23:34Z
    date copyright2008/12/01
    date issued2008
    identifier issn0894-8755
    identifier otherams-67038.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4208441
    description abstractThe performance of a set of 15 global climate models used in the Coupled Model Intercomparison Project is evaluated for Alaska and Greenland, and compared with the performance over broader pan-Arctic and Northern Hemisphere extratropical domains. Root-mean-square errors relative to the 1958?2000 climatology of the 40-yr ECMWF Re-Analysis (ERA-40) are summed over the seasonal cycles of three variables: surface air temperature, precipitation, and sea level pressure. The specific models that perform best over the larger domains tend to be the ones that perform best over Alaska and Greenland. The rankings of the models are largely unchanged when the bias of each model?s climatological annual mean is removed prior to the error calculation for the individual models. The annual mean biases typically account for about half of the models? root-mean-square errors. However, the root-mean-square errors of the models are generally much larger than the biases of the composite output, indicating that the systematic errors differ considerably among the models. There is a tendency for the models with smaller errors to simulate a larger greenhouse warming over the Arctic, as well as larger increases of Arctic precipitation and decreases of Arctic sea level pressure, when greenhouse gas concentrations are increased. Because several models have substantially smaller systematic errors than the other models, the differences in greenhouse projections imply that the choice of a subset of models may offer a viable approach to narrowing the uncertainty and obtaining more robust estimates of future climate change in regions such as Alaska, Greenland, and the broader Arctic.
    publisherAmerican Meteorological Society
    titleGlobal Climate Model Performance over Alaska and Greenland
    typeJournal Paper
    journal volume21
    journal issue23
    journal titleJournal of Climate
    identifier doi10.1175/2008JCLI2163.1
    journal fristpage6156
    journal lastpage6174
    treeJournal of Climate:;2008:;volume( 021 ):;issue: 023
    contenttypeFulltext
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    DSpace software copyright © 2002-2015  DuraSpace
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