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The surface climatology of the eastern Mediterranean region obtained in a three-member ensemble climate change simulation experiment

机译:三元整体气候变化模拟实验获得的地中海东部地区的表面气候

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Two configurations of RegCM3 regional climate model (RCM) have been used todownscale results of two atmosphere-ocean global climate model (AOGCM)simulations of the current (1961–1990) and future climates (2071–2100) overthe eastern Mediterranean (EM) region. The RCM domain covering the EM regionfrom northern Africa to central part of Asia Minor with grid spacing of 50 kmwas used. Three sets of RCM simulations were completed. Results of theRCM experiment support earlier projections of a temperature (annualprecipitation) increase (decrease) to the end of 21st century over theEM. The roles of several major factors in controlling uncertainty of theclimate change estimates are evaluated. The main uncertainty factors appear to be associatedwith possible inadequacies in RCM description of the EM-climate-controllingdevelopments over remotely located areas as well as those in the simulationsof the global climate and its trends by the AOGCMs.
机译:RegCM3区域气候模型(RCM)的两种配置已用于缩减东地中海(EM)地区当前(1961-1990)和未来气候(2071-2100)的两种大气-海洋全球气候模型(AOGCM)模拟的结果。使用了从北部非洲到小亚细亚中部的EM地区的RCM域,网格间距为50 km。完成了三组RCM仿真。 RCM实验的结果支持了到21世纪末整个EM的温度(年降水量)增加(降低)的早期预测。评估了几个主要因素在控制气候变化估计值不确定性中的作用。主要的不确定因素似乎与RCM描述偏远地区的EM气候控制发展以及AOGCM模拟全球气候及其趋势中的不足有关。

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