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    Assessing Atmospheric Response to Surface Forcing in the Observations. Part II: Cross Validation of Seasonal Response Using GEFA and LIM

    Source: Journal of Climate:;2012:;volume( 025 ):;issue: 019::page 6817
    Author:
    Liu, Zhengyu
    ,
    Fan, Lei
    ,
    Shin, Sang-Ik
    ,
    Liu, Qinyu
    DOI: 10.1175/JCLI-D-11-00630.1
    Publisher: American Meteorological Society
    Abstract: he authors compared the assessment of the seasonal cycle of the atmospheric response to surface forcing in three statistical methods, generalized equilibrium feedback analysis (GEFA), linear inverse modeling (LIM), and fluctuation?dissipation theorem (FDT). These methods are applied to both a conceptual climate model and the observation. It is found that LIM and GEFA are able to reproduce the major features of the seasonal response consistently, whereas FDT tends to generate a bias of the phase of the seasonal cycle. The success of LIM and GEFA for the assessment of the seasonal response is due to the slowly varying nature of the annual cycle relative to the atmospheric response time. Therefore, the authors recommend GEFA and LIM as two independent methods for the assessment of the seasonal atmospheric response in the observation.
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      Assessing Atmospheric Response to Surface Forcing in the Observations. Part II: Cross Validation of Seasonal Response Using GEFA and LIM

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4222016
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    contributor authorLiu, Zhengyu
    contributor authorFan, Lei
    contributor authorShin, Sang-Ik
    contributor authorLiu, Qinyu
    date accessioned2017-06-09T17:05:34Z
    date available2017-06-09T17:05:34Z
    date copyright2012/10/01
    date issued2012
    identifier issn0894-8755
    identifier otherams-79256.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4222016
    description abstracthe authors compared the assessment of the seasonal cycle of the atmospheric response to surface forcing in three statistical methods, generalized equilibrium feedback analysis (GEFA), linear inverse modeling (LIM), and fluctuation?dissipation theorem (FDT). These methods are applied to both a conceptual climate model and the observation. It is found that LIM and GEFA are able to reproduce the major features of the seasonal response consistently, whereas FDT tends to generate a bias of the phase of the seasonal cycle. The success of LIM and GEFA for the assessment of the seasonal response is due to the slowly varying nature of the annual cycle relative to the atmospheric response time. Therefore, the authors recommend GEFA and LIM as two independent methods for the assessment of the seasonal atmospheric response in the observation.
    publisherAmerican Meteorological Society
    titleAssessing Atmospheric Response to Surface Forcing in the Observations. Part II: Cross Validation of Seasonal Response Using GEFA and LIM
    typeJournal Paper
    journal volume25
    journal issue19
    journal titleJournal of Climate
    identifier doi10.1175/JCLI-D-11-00630.1
    journal fristpage6817
    journal lastpage6834
    treeJournal of Climate:;2012:;volume( 025 ):;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
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