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contributor authorZhu, Xiaojie
contributor authorLiu, Zhengyu
date accessioned2017-06-09T16:23:34Z
date available2017-06-09T16:23:34Z
date copyright2009/03/01
date issued2009
identifier issn0894-8755
identifier otherams-67039.pdf
identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4208442
description abstractThe trend of sea surface temperature (SST) in the twentieth century is examined in observations and the Intergovernmental Panel on Climate Change (IPCC) twentieth-century simulations. The observed SST neither shows a clear signal of the enhanced equatorial response (EER) warming nor exhibits a clear trend of the El Niño?like warming in the last century. Similarly, the IPCC simulations show neither a clear EER warming nor an El Niño?like warming in the last century. Furthermore, the comparison of heat fluxes in model simulations of the global warming scenario and the twentieth century indicates that the aerosol cooling effect, opposite to the greenhouse gases warming effect, plays an important role in the twentieth century and explains the EER-like signal in the twentieth-century simulations. Therefore, a conclusion that the IPCC model simulations of the twentieth century are consistent with observations within the error bars as well as the future projection of the EER warming pattern in the global warming scenario are validated.
publisherAmerican Meteorological Society
titleTropical SST Response to Global Warming in the Twentieth Century
typeJournal Paper
journal volume22
journal issue5
journal titleJournal of Climate
identifier doi10.1175/2008JCLI2164.1
journal fristpage1305
journal lastpage1312
treeJournal of Climate:;2009:;volume( 022 ):;issue: 005
contenttypeFulltext


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