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Evaluation of historical CMIP6 model simulations of extreme precipitation over contiguous US regions

机译:历史CMIP6模型模拟对邻近的美国地区极端降水的思考

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摘要

Simulated historical precipitation is evaluated for Coupled Model Intercomparison Project Phase 6 (CMIP6) models using precipitation indices defined by the Expert Team on Climate Change Detection and Indices. The model indices are evaluated against corresponding indices from the CPC unified gauge-based analyses of precipitation over seven geographical regions across the contiguous US (CONUS). The regions assessed match those in recent US National Climate Assessment Reports. To estimate observational uncertainty, precipitation indices for three other observational datasets (HadEx2, Livneh and PRISM) are evaluated against the CPC analyses. Both the moderate and extreme mean precipitation intensities are overestimated over the western CONUS and underestimated in the areas of the Central Great Plains (CGP) in most CMIP6 models tested. Most CMIP6 models overestimate the mean and variability of wet spell durations and underestimate the mean and variability of dry spell durations across the CONUS. Biases in interannual variability of most of the indices have similar patterns to those in corresponding mean biases. The median and interquartile model spreads in CMIP6 model biases are clearly smaller than those in CMIP5 model biases for wet spell durations. Multimodel medians of CMIP6 (CMIP6-MMM) and CMIP5 (CMIP5-MMM) have similar biases in climatology and variability but biases tend to be smaller in CMIP6-MMM. Depending on the index, extreme precipitation is slightly better in parts of the eastern half of the CONUS in CMIP6-MMM, otherwise, the biases in climatology and variability are similar to CMIP5-MMM. CMIP6-MMM performs better than individual models and even observational datasets in some cases. Differences between observational datasets for most indices are comparable to the CMIP6 interquartile model spread. The better-performing observational and model datasets are different in different parts of the CONUS.
机译:使用专家组在气候变化检测和指标上定义的降水指标来评估模拟历史降水的耦合模型离心项目阶段6(CMIP6)模型。通过基于CPC统筹规范的降水分析对七个地理区域的降水分析来评估模型指数。该区域评估与最近的美国国家气候评估报告中的地区相符。为了估算观察性不确定性,针对CPC分析评估三个其他观察数据集的降水指数(Hadex2,Livneh和Prism)。在大多数CMIP6型号测试中,中等和极端的降水强度均高估在西锥体上并低估了中央大平原(CGP)的区域。大多数CMIP6型号高估湿法持续时间的平均值和变异,低估了康明斯干法杜氏的平均值和变异性。大多数索引的持续可变性的偏差具有与相应平均偏差相似的模式。在CMIP6模型偏差中的中位数和狭隘的模型差异显然比CMIP5模型偏差的偏差均匀差异。 CMIP6(CMIP6-MMM)和CMIP5(CMIP5-MMM)的多模型中音具有相似的气候学和可变性,但在CMIP6-MMM中偏置趋于较小。根据索引,在CMIP6-MMM的锥形部分的部分地区,极端降水量稍微好转,否则,气候学和变异性的偏差类似于CMIP5-MMM。在某些情况下,CMIP6-MMM比单个模型更好地执行甚至观察数据集。大多数指数的观察数据集之间的差异与CMIP6型号的差异相当。更好的观察和模型数据集在康纳斯的不同部分不同。

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