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Climate change track in river floods in Europe

机译:欧洲河流洪水中的气候变化轨迹

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A holistic perspective on changing river flood risk in Europe is provided. Economic losses from floods have increased, principally driven by the expanding exposure of assets at risk. Climate change (i.e. observed increase in precipitation intensity, decrease of snowpack and other observed climate changes) might already have had an impact on floods. However, no gauge-based evidence had been found for a climate-driven, widespread change in the magnitude/frequency of floods during the last decades. There are strong regional and sub-regional variations in the trends. Moreover, it has not been generally possible to attribute rain-generated peak streamflow trends to anthropogenic climate change. Physical reasoning suggests that projected increases in the frequency and intensity of heavy rainfall would contribute to increases in rain-generated local floods, while less snowmelt flooding and earlier spring peak flows in snowmelt-fed rivers are expected. However, there is low confidence in future changes in flood magnitude and frequency resulting from climate change. The impacts of climate change on flood characteristics are highly sensitive to the detailed nature of those changes. Discussion of projections of flood hazard in Europe is offered. Attention is drawn to a considerable uncertainty - over the last decade or so, projections of flood hazard in Europe have largely changed.
机译:提供了有关改变欧洲河流洪水风险的整体观点。洪水造成的经济损失有所增加,这主要是由于面临风险的资产不断扩大所致。气候变化(即观测到的降水强度增加,积雪减少和其他观测到的气候变化)可能已经对洪水产生了影响。但是,在过去的几十年中,没有发现基于量表的证据表明受气候驱动的洪水数量/频率的广泛变化。趋势中区域和次区域存在很大差异。此外,一般不可能将降雨产生的峰值流量趋势归因于人为气候变化。物理推理表明,预计暴雨的频率和强度的增加将有助于增加由降雨产生的局部洪水,而预计融雪河中的融雪洪水和春季高峰流量将减少。但是,人们对由于气候变化而导致的未来洪水强度和频率变化的信心不足。气候变化对洪水特征的影响对这些变化的详细性质高度敏感。提供了有关欧洲洪水灾害预测的讨论。人们已经注意到了相当大的不确定性-在过去的十年左右的时间里,欧洲对洪灾的预测已发生了很大变化。

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