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首页> 外文期刊>Journal of Climate >Heavy precipitation events in a warmer climate: results from CMIP5 models.
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Heavy precipitation events in a warmer climate: results from CMIP5 models.

机译:气候变暖时的强降水事件:来自CMIP5模型的结果。

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In this work, the authors investigate possible changes in the distribution of heavy precipitation events under a warmer climate, using the results of a set of 20 climate models taking part in phase 5 of Coupled Model Intercomparison Project (CMIP5). Future changes are evaluated as the difference between the last four decades of the twenty-first century and the twentieth century, assuming the representative concentration pathway 8.5 (RCP8.5) scenario. As a measure of the width of the right tail of the precipitation distribution, the authors use the difference between the 99th and the 90th percentiles. Despite a slight tendency to underestimate the observed heavy precipitation, the considered CMIP5 models well represent the observed patterns in terms of the ensemble average, during both boreal summer and winter seasons for the 1997-2005 period. Future changes in average precipitation are consistent with previous findings based on models from phase 3 of CMIP (CMIP3). CMIP5 models show a projected increase for the end of the twenty-first century of the width of the right tail of the precipitation distribution, particularly pronounced over India, Southeast Asia, Indonesia, and central Africa during boreal summer, as well as over South America and southern Africa during boreal winter.Digital Object Identifier http://dx.doi.org/10.1175/JCLI-D-12-00850.1
机译:在这项工作中,作者使用参与耦合模型比较项目(CMIP5)阶段5的20种气候模型的结果,研究了气候变暖下强降水事件分布的可能变化。假设有代表性的浓缩途径8.5(RCP8.5),则将未来的变化评估为二十一世纪最后四十年与二十世纪之间的差异。作者使用第99个百分位数和第90个百分位数之间的差异作为降水分布右尾宽度的度量。尽管略有低估了观测到的强降水的趋势,但考虑到的CMIP5模型可以很好地代表1997-2005年夏季和冬季的总体平均观测模式。未来平均降水量的变化与基于CMIP第三阶段(CMIP3)模型的先前发现一致。 CMIP5模型显示,在二十一世纪末,降水分布右尾的宽度预计会增加,在北方夏季以及印度,东南亚,印度尼西亚和中部非洲以及北美地区尤为明显和北方冬季的南部非洲。数字对象标识符http://dx.doi.org/10.1175/JCLI-D-12-00850.1

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