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    Transient Climate Change in the Hadley Centre Models: The Role of Physical Processes

    Source: Journal of Climate:;2001:;volume( 014 ):;issue: 012::page 2659
    Author:
    Williams, K. D.
    ,
    Senior, C. A.
    ,
    Mitchell, J. F. B.
    DOI: 10.1175/1520-0442(2001)014<2659:TCCITH>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: A comparison of the response to increasing greenhouse gas concentrations of two versions of the Met Office's (Hadley Centre) coupled atmosphere?ocean model reveals differences that result in large local variations in the modeled impact of climate change. With the aim of understanding the important processes and feedbacks associated with climate change, and ultimately reducing uncertainty in predictions, a series of sensitivity experiments were performed using a coupled atmosphere?mixed layer ocean model. The primary differences in the atmospheric response of the coupled models studied are found to be due to changes made to the physical representation of the atmosphere rather than to the ocean. In particular, many of the different patterns of response can be explained through changes made to the boundary layer scheme combining in a nonlinear way with changes to the cloud scheme to alter the tropical temperature and precipitation response in the model. A new land surface exchange scheme largely accounts for the different Northern Hemisphere continental surface temperature response.
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      Transient Climate Change in the Hadley Centre Models: The Role of Physical Processes

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4198556
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    contributor authorWilliams, K. D.
    contributor authorSenior, C. A.
    contributor authorMitchell, J. F. B.
    date accessioned2017-06-09T15:59:09Z
    date available2017-06-09T15:59:09Z
    date copyright2001/06/01
    date issued2001
    identifier issn0894-8755
    identifier otherams-5814.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4198556
    description abstractA comparison of the response to increasing greenhouse gas concentrations of two versions of the Met Office's (Hadley Centre) coupled atmosphere?ocean model reveals differences that result in large local variations in the modeled impact of climate change. With the aim of understanding the important processes and feedbacks associated with climate change, and ultimately reducing uncertainty in predictions, a series of sensitivity experiments were performed using a coupled atmosphere?mixed layer ocean model. The primary differences in the atmospheric response of the coupled models studied are found to be due to changes made to the physical representation of the atmosphere rather than to the ocean. In particular, many of the different patterns of response can be explained through changes made to the boundary layer scheme combining in a nonlinear way with changes to the cloud scheme to alter the tropical temperature and precipitation response in the model. A new land surface exchange scheme largely accounts for the different Northern Hemisphere continental surface temperature response.
    publisherAmerican Meteorological Society
    titleTransient Climate Change in the Hadley Centre Models: The Role of Physical Processes
    typeJournal Paper
    journal volume14
    journal issue12
    journal titleJournal of Climate
    identifier doi10.1175/1520-0442(2001)014<2659:TCCITH>2.0.CO;2
    journal fristpage2659
    journal lastpage2674
    treeJournal of Climate:;2001:;volume( 014 ):;issue: 012
    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