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    The Potential Effect of GCM Uncertainties and Internal Atmospheric Variability on Anthropogenic Signal Detection

    Source: Journal of Climate:;1998:;volume( 011 ):;issue: 004::page 659
    Author:
    Barnett, Tim P.
    ,
    Hegerl, Gabriele C.
    ,
    Santer, Ben
    ,
    Taylor, Karl
    DOI: 10.1175/1520-0442(1998)011<0659:TPEOGU>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: When long integrations of climate models forced by observed boundary conditions are compared against observations, differences appear that have spatial and temporal coherence. These differences are due to several causes, the largest of which are fundamental model errors and the internal variability inherent in a GCM integration. Uncertainties in the observations themselves are small in comparison. The present paper constitutes a first attempt to compare the time dependence of these spatial difference patterns with the time dependence of simulated spatial patterns of climate change associated with anthropogenic sources. The analysis procedure was to project the model minus observed near-surface temperature difference fields onto estimates of the anthropogenic ?signal? (in this case the response to greenhouse-gas and sulfate-aerosol forcing). The temporal behavior of this projection was then compared with the estimated temporal evolution of the anthropogenic signal. Such comparisons were performed on timescales of 10, 20, and 30 yr. For trends of only 10 yr in length, the model minus observed spatial difference patterns are of the same magnitude and have the same time rate of change as the expected anthropogenic signal. In the case of 20- and 30-yr trends, the prospects are favorable for discriminating between temperature changes due to anthropogenic signal changes and changes associated with model minus observed difference structures. This suggests that attempts to quantitatively detect anthropogenic climate change should be based on temporal samples of at least several decades in length. This study also shows the importance of distinguishing between purely statistical detection and what the authors term practical prediction. It is found that the results of the detection analysis are sensitive to the spatial resolution at which it is performed: for the specific case of near-surface temperature, higher spatial resolution improves ability to discriminate between an anthropogenic signal and the type of model error/internal variability ?noise? considered here.
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      The Potential Effect of GCM Uncertainties and Internal Atmospheric Variability on Anthropogenic Signal Detection

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4188922
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    contributor authorBarnett, Tim P.
    contributor authorHegerl, Gabriele C.
    contributor authorSanter, Ben
    contributor authorTaylor, Karl
    date accessioned2017-06-09T15:38:34Z
    date available2017-06-09T15:38:34Z
    date copyright1998/04/01
    date issued1998
    identifier issn0894-8755
    identifier otherams-4947.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4188922
    description abstractWhen long integrations of climate models forced by observed boundary conditions are compared against observations, differences appear that have spatial and temporal coherence. These differences are due to several causes, the largest of which are fundamental model errors and the internal variability inherent in a GCM integration. Uncertainties in the observations themselves are small in comparison. The present paper constitutes a first attempt to compare the time dependence of these spatial difference patterns with the time dependence of simulated spatial patterns of climate change associated with anthropogenic sources. The analysis procedure was to project the model minus observed near-surface temperature difference fields onto estimates of the anthropogenic ?signal? (in this case the response to greenhouse-gas and sulfate-aerosol forcing). The temporal behavior of this projection was then compared with the estimated temporal evolution of the anthropogenic signal. Such comparisons were performed on timescales of 10, 20, and 30 yr. For trends of only 10 yr in length, the model minus observed spatial difference patterns are of the same magnitude and have the same time rate of change as the expected anthropogenic signal. In the case of 20- and 30-yr trends, the prospects are favorable for discriminating between temperature changes due to anthropogenic signal changes and changes associated with model minus observed difference structures. This suggests that attempts to quantitatively detect anthropogenic climate change should be based on temporal samples of at least several decades in length. This study also shows the importance of distinguishing between purely statistical detection and what the authors term practical prediction. It is found that the results of the detection analysis are sensitive to the spatial resolution at which it is performed: for the specific case of near-surface temperature, higher spatial resolution improves ability to discriminate between an anthropogenic signal and the type of model error/internal variability ?noise? considered here.
    publisherAmerican Meteorological Society
    titleThe Potential Effect of GCM Uncertainties and Internal Atmospheric Variability on Anthropogenic Signal Detection
    typeJournal Paper
    journal volume11
    journal issue4
    journal titleJournal of Climate
    identifier doi10.1175/1520-0442(1998)011<0659:TPEOGU>2.0.CO;2
    journal fristpage659
    journal lastpage675
    treeJournal of Climate:;1998:;volume( 011 ):;issue: 004
    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
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