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首页> 外文期刊>Journal of Geophysical Research, D. Atmospheres: JGR >Changing spatiotemporal patterns of precipitation extremes in China during 2071–2100 based on Earth System Models
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Changing spatiotemporal patterns of precipitation extremes in China during 2071–2100 based on Earth System Models

机译:基于地球系统模型的2071–2100年中国极端降水的时空格局变化

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摘要

Outputs of five Earth System Models (ESMs) under historical and Representative Concentration Pathways (RCPs) scenarios from the Coupled Model Intercomparison Project phase 5 multimodel data set, as well as daily precipitation from 527 rain gauge stations in China for the period of 1960–2005 are used to investigate the spatiotemporal variations of precipitation extremes over China for 2071–2100. After the evaluation of the indices by the Mann-Whitney U test and the quantile-quantile plot, the weather generator model (WGEN) is used to downscale precipitation extremes. The average of precipitation extremes and values of the 5 and 20 year return periods under RCP26 and RCP85 scenarios are analyzed. Results showed the following: (1) WGEN works well in downscaling extreme heavy precipitation indices and consecutive dry days. (2) The risks of meteorological droughts and floods resulting from extreme long-duration precipitation would decrease in southwest China, but the risks of floods due to extreme heavy precipitation would increase. In north and southeast China, the risks of droughts would decrease, but floods might occur with higher frequencies; (3) The spatiotemporal variations of averages and values of 5 year return period extreme precipitation would be similar, but those of 20 year return period would be a little different: The 20 year consecutive dry days would decrease faster, and the 20 year values of other indices would increase relatively slower. (4) The spatial patterns of changes in precipitation extremes under RCP26 and RCP85 would be similar, but the changes in RCP85 would be intensifying.
机译:耦合模型比对项目第5阶段多模型数据集在历史和代表性集中路径(RCP)情景下的五个地球系统模型(ESM)的输出,以及1960-2005年期间中国527个雨量计站的日降水量用于调查2071–2100年中国极端降水的时空变化。在通过Mann-Whitney U检验和分位数-分位数图对指标进行评估之后,使用天气生成器模型(WGEN)来降低极端降水。分析了RCP26和RCP85情景下极端降水的平均值和5年和20年回归期的值。结果表明:(1)WGEN在降低极端强降水指数和连续干旱天数方面表现良好。 (2)在西南地区,由于极端长期降雨而造成的气象干旱和洪水的风险将降低,但由于极端强降水而导致的洪水风险将增加。在中国的北部和东南部,干旱的风险将降低,但洪水的发生频率可能​​更高。 (3)5年回归期极端降水的平均值和值的时空变化相似,但20年回归期的平均值和值的时空变化略有不同:连续20年的干旱天数减少得更快,而20年的干旱天数则减少。其他指数的增长相对较慢。 (4)RCP26和RCP85下的极端降水变化的空间格局相似,但RCP85的变化将加剧。

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