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首页> 外文期刊>Journal of Geophysical Research, D. Atmospheres: JGR >Regional climate model simulation of projected 21st century climate change over an all‐Africa domain: Comparison analysis of nested and driving model results
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Regional climate model simulation of projected 21st century climate change over an all‐Africa domain: Comparison analysis of nested and driving model results

机译:全非洲范围内预计的21世纪气候变化的区域气候模型模拟:嵌套和驱动模型结果的比较分析

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We analyze a transient climate change simulation for the 21st century (1980–2100) over a large all‐Africa domain carried out with the RegCM3 regional model driven by the ECHAM5 global model. We focus the analysis on a comparison between the driving and nested model runs. For present climate, the two models show temperature and precipitation biases of similar magnitude but different spatial patterns. In particular the bias patterns in the regional model driven by ECHAM5 are more similar to those of a regional simulation driven by ERA Interim reanalysis fields than to the bias patterns in the present climate simulation by ECHAM5 itself. In the transient simulation, while the temperature changes are strongly driven by the global model, the precipitation change patterns are more different between the global and regional models, particularly over the West Africa and Sahel regions. A targeted analysis suggests that this is due to the different simulation by the two models of the local response to El Ni?o–Southern Oscillation forcing and of local soil moisture/precipitation feedbacks. Our results thus indicate that local processes and internal model physics and characteristics are important elements in determining the precipitation change signal simulated by the nested regional model in this large domain experiment, especially over equatorial and tropical regions. This adds an element of uncertainty that needs to be address through the use of ensembles of regional model experiments as planned in the Coordinated Regional Climate Downscaling Experiment (CORDEX) project.
机译:我们分析了由ECHAM5全局模型驱动的RegCM3区域模型对21世纪(1980-2100年)在整个非洲范围内进行的瞬态气候变化模拟。我们将分析的重点放在驱动模型和嵌套模型运行之间的比较上。对于当前的气候,这两个模型显示出相似的温度和降水偏差但空间格局不同。特别是,由ECHAM5驱动的区域模型中的偏差模式与由ERA中期再分析场驱动的区域模拟中的偏差模式相比,与由ECHAM5本身进行的当前气候模拟中的偏差模式更相似。在瞬态模拟中,虽然温度变化是由全球模型强烈驱动的,但全球和区域模型之间的降水变化模式差异更大,尤其是在西非和萨赫勒地区。一项有针对性的分析表明,这是由于两个模型对厄尔尼诺-南方涛动强迫的局部响应和局部土壤水分/降水反馈的模拟不同所致。因此,我们的结果表明,在此大范围实验中,特别是在赤道和热带地区,局部过程和内部模型的物理特性是决定嵌套区域模型模拟的降水变化信号的重要因素。这增加了不确定性因素,需要按照协调的区域气候缩减实验(CORDEX)项目的计划,通过使用区域模型实验的集合来解决。

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