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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


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