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首页> 外文期刊>International Journal of Climatology: A Journal of the Royal Meteorological Society >Extreme precipitation events under climate change in the Iberian Peninsula
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Extreme precipitation events under climate change in the Iberian Peninsula

机译:Iberian半岛气候变化下的极端降水事件

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摘要

Precipitation is one of the most important atmospheric variables to assess, particularly in the context of climate change. This study evaluates future changes in precipitation over the Iberian Peninsula (IP) under the RCP8.5 scenario. Changes are assessed for two future climate periods namely (2046-2065) and (2081-2100), relative to a recent reference climate (1986-2005). Here we introduce the concept of precipitation episodes (PEs) and estimate their statistical properties for the present climate and, their changes for future climate scenarios. PEs are defined by considering a full range of durations as well as intensities. This constitutes a novel approach to estimate changes with relevance, for example, for water resources applications. The climate simulations are performed with the Weather Research and Forecast (WRF) model. These are compared with an ensemble of other similar simulations from the Coordinated Downscaling Experiment initiative. This was done to evaluate the performance of the WRF model and also to estimate uncertainty of the derived future projections. Since models may present systematic errors, results from all simulations were previously bias corrected relative to observations using the same quantile mapping method. Under climate change, a great part of the region is expected to experience reduced annual precipitation of approximately 20-40% and reaching 80% in summer by the end of the XXI century. For the PEs, a large reduction in the average number of days and duration of all types of PEs is expected across all seasons and regions. The average intensity of episodes is projected to increase in winter and spring and decrease in summer. These results imply that climate change will likely influence precipitation and precipitation extremes in the 21st century, mostly in southern areas. These, together with projected warming may amplify desertification already taking place in the southern regions of the IP and cause stresses to water resources.
机译:降水是评估中最重要的大气变量之一,特别是在气候变化的背景下。本研究评估了RCP8.5情景下伊比利亚半岛(IP)降水的未来变化。相对于最近的参考气候(1986-2005),对未来的两个气候期和(2081-2100)进行评估改变。在这里,我们介绍了降水剧集(PE)的概念,并估计了目前气候的统计特性,以及他们对未来气候情景的变化。通过考虑全范围的持续时间以及强度来定义PE。这构成了一种新的方法来估计相关性的变化,例如,用于水资源应用。气候仿真是用天气研究和预测(WRF)模型进行的。将这些与来自协调的缩小实验倡议的其他类似仿真的集合进行比较。这是为了评估WRF模型的性能以及估计衍生的未来预测的不确定性。由于模型可能出现系统错误,因此所有模拟的结果先前偏置相对于使用相同的定量映射方法的观察结果校正。根据气候变化,该地区的大部分预计将在XXI世纪末举行约20-40%的年降水量约为20-40%,达到80%。对于PE,在所有季节和地区都预计所有类型PE的平均天数和持续时间的大幅减少。剧集的平均强度被预计冬季和春季和夏季减少。这些结果意味着气候变化可能会影响21世纪的降水和降水,主要是在南部地区。这些,与预计的变暖一起可以放大已经在IP的南部地区进行的荒漠化,并对水资源引起压力。

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