Haslinger Klaus, Breinl Korbinian, Pavlin Lovrenc, Pistotnik Georg, Bertola Miriam, Olefs Marc, Greilinger Marion, Schöner Wolfgang, Blöschl Günter
Department for Climate Impact Research, GeoSphere Austria - Federal Agency for Geology, Geophysics, Climatology and Meteorology, Vienna, Austria.
Directorate for Water Balance, Federal Ministry Republic of Austria for Agriculture, Forestry, Regions and Water Management, Vienna, Austria.
Nature. 2025 Mar;639(8055):667-672. doi: 10.1038/s41586-025-08647-2. Epub 2025 Mar 12.
Climate change is expected to increase heavy rainfall with concomitant increases in flooding. Causes of increased heavy rainfall include the higher water-holding capacity of a warmer atmosphere and changes in atmospheric circulation patterns, which may translate into future heavy rainfall increases in most of Europe. However, gathering evidence on the time evolution of past changes has been hampered by data limitations and measurement uncertainties, in particular for short rainfall durations, such as 1 h. Here we show an 8% increase in daily and 15% increase in hourly heavy rainfall over the last four decades by analysing a new dataset comprising 883 stations in Austria from 1900 to 2023. These increases are fully consistent between two independent networks and occurred after a retarding phase between 1960 and 1980. Hourly heavy rainfall changes are aligned with temperature increases with the sensitivity of a 7% increase per 1 °C of warming, in line with Clausius-Clapeyron scaling. Daily heavy rainfall changes, however, are aligned with atmospheric circulation indices with little correlation to air temperature, which suggests a bigger role of atmospheric circulation modes than previously thought. The daily heavy rainfall changes are remarkably consistent with observed flood increases of about 8% in large catchments. The hourly heavy rainfall changes are similarly consistent with flood changes in small catchments, although the flood increase is stronger (25% over the last four decades). Climate adaptation measures in flood management may therefore be more pressing for rivers draining smaller catchment areas than for large rivers.
预计气候变化将增加强降雨,并随之增加洪水发生的频率。强降雨增加的原因包括温暖大气更高的持水能力以及大气环流模式的变化,这可能导致欧洲大部分地区未来强降雨增加。然而,过去变化的时间演变证据收集工作受到数据限制和测量不确定性的阻碍,特别是对于短降雨持续时间,如1小时的情况。在这里,我们通过分析一个新数据集(该数据集包含奥地利从1900年到2023年的883个站点)表明,在过去四十年中,日强降雨增加了8%,小时强降雨增加了15%。这些增加在两个独立网络之间完全一致,并且在1960年至1980年的一个延迟阶段之后出现。小时强降雨变化与温度升高一致,升温1°C时增加7%的敏感性,符合克劳修斯 - 克拉佩龙标度关系。然而,日强降雨变化与大气环流指数一致,与气温相关性很小,这表明大气环流模式的作用比以前认为的更大。日强降雨变化与大集水区观测到的约8%的洪水增加显著一致。小时强降雨变化同样与小集水区的洪水变化一致,尽管洪水增加更强(在过去四十年中增加了25%)。因此,对于流经较小集水区的河流,洪水管理中的气候适应措施可能比对大型河流更为紧迫。