Department of Environmental Engineering (DTU Environment), Technical University of Denmark, Miljoevej, Bldg 113, DK-2800, Kgs. Lyngby, Denmark.
Water Sci Technol. 2009;60(9):2205-16. doi: 10.2166/wst.2009.650.
In this study the potential increase of extreme precipitation in a future warmer European climate has been examined. Output from the regional climate model (RCM) HIRHAM4 covering Europe has been analysed for two periods, a control period 1961-1990 and a scenario 2071-2100, the latter following the IPCC scenario A2. The model has a resolution of about 12 km, which is unique compared with existing RCM studies that typically operate at 25-50 km scale, and make the results relevant to hydrological phenomena occurring at the spatial scale of the infrastructure designed to drain off rainfall in large urban areas. Extreme events with one- and 24-hour duration were extracted using the Partial Duration Series approach, a Generalized Pareto Distribution was fitted to the data and T-year events for return periods from 2 to 100 years were calculated for the control and scenario period in model cells across Europe. The analysis shows that there will be an increase of the intensity of extreme events generally in Europe; Scandinavia will experience the highest increase and southern Europe the lowest. A 20 year 1-hour precipitation event will for example become a 4 year event in Sweden and a 10 year event in Spain. Intensities for short durations and high return periods will increase the most, which implies that European urban drainage systems will be challenged in the future.
本研究考察了未来更暖的欧洲气候中极端降水增加的可能性。分析了覆盖欧洲的区域气候模型(RCM)HIRHAM4 的输出结果,该模型分为两个时期,控制期为 1961-1990 年,情景期为 2071-2100 年,后者遵循 IPCC 情景 A2。该模型的分辨率约为 12 公里,与现有 RCM 研究相比具有独特性,现有 RCM 研究通常在 25-50 公里的范围内运行,这使得研究结果与在大型城市地区设计用于排雨的基础设施的空间尺度上发生的水文现象相关。使用部分持续时间序列方法提取了持续时间为 1 小时和 24 小时的极端事件,对数据进行了广义帕累托分布拟合,并计算了控制期和情景期模型单元中返回期为 2 年至 100 年的 T 年事件。分析表明,欧洲的极端事件强度普遍将增加;斯堪的纳维亚将经历最大的增加,而南欧将经历最小的增加。例如,瑞典的 20 年 1 小时降水事件将成为 4 年事件,西班牙的 10 年事件将成为 4 年事件。短时间和高返回期的强度增加最大,这意味着欧洲的城市排水系统在未来将面临挑战。