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首页> 外文期刊>International Journal of Climatology: A Journal of the Royal Meteorological Society >Near future changes of extreme precipitation over complex terrain in Central Europe derived from high resolution RCM ensemble simulations
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Near future changes of extreme precipitation over complex terrain in Central Europe derived from high resolution RCM ensemble simulations

机译:来自高分辨率RCM集成模拟的中欧复杂地形的近期极端降水变化

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摘要

An ensemble of high-resolution regional climate simulations is used to assess the effect of near future climate change on mean and extreme precipitation in a part of Central Europe with complex topography. The ensemble consists of high-resolution simulations with the COSMO-CLM (CLM) regional climate model (RCM) using several realizations of the driving general circulation models (GCMs) ECHAM5 and HadCM3. The study is focussed on the changes in the near future (2011-2040 compared to 1971-2000) which are relevant for planning purposes. The mean winter precipitation shows a spatially uniform increase, summertime mean precipitation is likely to decrease slightly. For extreme precipitation the simulations exhibit an increase on the average for both seasons, but for different reasons. The changes in winter are proportional to the increase in total precipitation, whereas in summer a broadening of the precipitation distribution is found. The spatial change patterns in summer are much more heterogeneous than in winter, with regions of significant increase and decrease sometimes close to each other. The plausibility of the findings is assessed in terms of ensemble consistency. The area mean changes found for the ensemble of CLM simulations were consistent with the change signals derived from a larger but coarser resolved ensembles using several RCMs and driving GCMs. In addition, it was found that the simulated near future precipitation changes in the study region during summer generally agree with trends observed during the last decades.
机译:一组高分辨率的区域气候模拟用于评估中欧部分地形复杂的近期气候变化对平均和极端降水的影响。该集合由COSMO-CLM(CLM)区域气候模型(RCM)的高分辨率模拟组成,其中使用了驾驶一般循环模型(GCM)ECHAM5和HadCM3的几种实现。该研究的重点是与计划目的相关的近期变化(2011-2040年与1971-2000年相比)。冬季平均降水量在空间上均匀增加,夏季平均降水量可能略有减少。对于极端降水,模拟显示两个季节的平均值都有所增加,但原因有所不同。冬季的变化与总降水量的增加成正比,而在夏季,降水量分布变宽。夏季的空间变化模式比冬季的异质性要大得多,有时显着增加和减少的区域彼此接近。根据整体一致性评估结果的合理性。对于CLM模拟集合,发现的面积平均变化与使用多个RCM和驱动GCM从较大但较粗糙的分解合奏中得出的变化信号一致。此外,还发现,夏季研究区近期模拟的近期降水变化与过去几十年的趋势基本吻合。

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