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Evaluation of CMIP6 precipitation simulations across different climatic zones: Uncertainty and model intercomparison

机译:不同气候区CMIP6降水模拟的评价:不确定性和模型兼容性

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This study analyzes the performance of precipitation estimates from historical runs of the CMIP6 (Climate Model Intercomparison Project Phase 6) over the climatic regions of Iran. In order to capture the spatio-temporal precipitation patterns, using a set of evaluation metrics, 12 GCMs (General Circulation Models) are compared to the observation data from the GPCC (Global Precipitation Climatology Centre) at the common 1 degrees spatial resolution for 1950-2014. A comprehensive assessment is performed at different temporal scales including monthly, seasonal and annual. Results indicate that the reliability of precipitation estimates varies significantly across space and time. The CMIP6 models best reproduce the climatological features of precipitation and its spatio-temporal changes over the arid and hyper arid areas of the country. The outputs of the models exhibit less systematic biases in the arid zone. In addition, a strong underestimation is detected throughout the rainiest zone, indicating high uncertainty in wet regions. All models tend to show some level of underestimation in summer months with the lowest rainfall. The findings illustrate substantial inter-model variability over different climatic zones. Each of the CMIP6 models appears to be more suitable in a specific climatic zone. The models that performed reasonably well in the humid zone (CNRM-CM6-1 and MRI-ESM2-0), did not perform well in the hyper arid and arid zones. Similarly, models (HadGEM3-GC31-LL, BCC-CSM2-MR, and CanESM5) that performed well in the arid and hyper arid zones did not perform as well in the humid zone. Results inform what types of models are suitable for different climate zones.
机译:本研究分析了在伊朗气候区域的CMIP6(气候模型相互比较项目阶段6)的历史历史估计的性能。为了使用一组评估度量来捕获时空降水模式,将12个GCM(一般循环模型)与GPCC(全球降水升温中心)的观察数据进行比较,以便在1950年的共同空间分辨率下2014年。在不同的时间尺度上进行综合评估,包括每月,季节性和年度。结果表明,降水估计的可靠性在空间和时间上变化显着。 CMIP6型号最佳再现降水的气候功能及其在国家干旱地区的干旱地区的时间变化。模型的输出在干旱区中表现出较差的系统偏差。此外,在最衰落的区域中检测到强烈的低估,表明湿地区的高不确定性。所有型号往往在夏季展示一些低估水平,降雨量最低。结果说明了不同气候区域的模型间互换性。每个CMIP6型号似乎更适合于特定气候区域。在潮湿区(CNRM-CM6-1和MRI-ESM2-0)中相当良好地进行的模型在超干旱和干旱区域中表现不佳。类似地,在干旱和超干旱区中表现良好的模型(Hadgem3-GC31-LL,BCC-CSM2-MR和CANESM5)在潮湿区内没有表现。结果通知哪种类型的模型适用于不同的气候区。

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