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    The Iris Hypothesis: A Negative or Positive Cloud Feedback?

    Source: Journal of Climate:;2002:;volume( 015 ):;issue: 001::page 3
    Author:
    Lin, Bing
    ,
    Wielicki, Bruce A.
    ,
    Chambers, Lin H.
    ,
    Hu, Yongxiang
    ,
    Xu, Kuan-Man
    DOI: 10.1175/1520-0442(2002)015<0003:TIHANO>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: Using the Tropical Rainfall Measuring Mission (TRMM) satellite measurements over tropical oceans, this study evaluates the iris hypothesis recently proposed by Lindzen et al. that tropical upper-tropospheric anvils act as a strong negative feedback in the global climate system. The modeled radiative fluxes of Lindzen et al. are replaced by the Clouds and the Earth's Radiant Energy System (CERES) directly observed broadband radiation fields. The observations show that the clouds have much higher albedos and moderately larger longwave fluxes than those assumed by Lindzen et al. As a result, decreases in these clouds would cause a significant but weak positive feedback to the climate system, instead of providing a strong negative feedback.
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      The Iris Hypothesis: A Negative or Positive Cloud Feedback?

    URI
    http://yetl.yabesh.ir/yetl1/handle/yetl/4199933
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    • Journal of Climate

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    contributor authorLin, Bing
    contributor authorWielicki, Bruce A.
    contributor authorChambers, Lin H.
    contributor authorHu, Yongxiang
    contributor authorXu, Kuan-Man
    date accessioned2017-06-09T16:02:14Z
    date available2017-06-09T16:02:14Z
    date copyright2002/01/01
    date issued2002
    identifier issn0894-8755
    identifier otherams-5938.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4199933
    description abstractUsing the Tropical Rainfall Measuring Mission (TRMM) satellite measurements over tropical oceans, this study evaluates the iris hypothesis recently proposed by Lindzen et al. that tropical upper-tropospheric anvils act as a strong negative feedback in the global climate system. The modeled radiative fluxes of Lindzen et al. are replaced by the Clouds and the Earth's Radiant Energy System (CERES) directly observed broadband radiation fields. The observations show that the clouds have much higher albedos and moderately larger longwave fluxes than those assumed by Lindzen et al. As a result, decreases in these clouds would cause a significant but weak positive feedback to the climate system, instead of providing a strong negative feedback.
    publisherAmerican Meteorological Society
    titleThe Iris Hypothesis: A Negative or Positive Cloud Feedback?
    typeJournal Paper
    journal volume15
    journal issue1
    journal titleJournal of Climate
    identifier doi10.1175/1520-0442(2002)015<0003:TIHANO>2.0.CO;2
    journal fristpage3
    journal lastpage7
    treeJournal of Climate:;2002:;volume( 015 ):;issue: 001
    contenttypeFulltext
    DSpace software copyright © 2002-2015  DuraSpace
    نرم افزار کتابخانه دیجیتال "دی اسپیس" فارسی شده توسط یابش برای کتابخانه های ایرانی | تماس با یابش
    yabeshDSpacePersian
     
    DSpace software copyright © 2002-2015  DuraSpace
    نرم افزار کتابخانه دیجیتال "دی اسپیس" فارسی شده توسط یابش برای کتابخانه های ایرانی | تماس با یابش
    yabeshDSpacePersian