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越来越多的每小时大雨在奥地利反映在洪水变化
Klaus Haslinger1, Korbinian Breinl2, Lovrenc Pavlin2
1Department for Climate Impact Research, GeoSphere Austria - Federal Agency for Geology, Geophysics, Climatology and Meteorology, Vienna, Austria. klaus.haslinger@geosphere.at.
Nature
|March 13, 2025
概括
过去40年来,奥地利的暴雨量显著增加,每小时降雨量增加了15%,每天降雨量增加了8%. 这一趋势凸显了对洪水管理,特别是较小的河流流域的气候适应的迫切需要.
科学领域:
- 气候学和水文学
- 极端天气事件分析
背景情况:
- 预计气候变化将加剧暴雨事件,导致洪水增加.
- 由于数据的限制,特别是在短时间内,对过去大雨变化的归因是具有挑战性的.
- 气候变暖和循环模式的改变是增加大雨的关键因素.
研究的目的:
- 分析奥地利过去40年的暴雨变化.
- 研究大雨趋势,温度和大气循环之间的关系.
- 评估不同水域大小的降雨变化与观测到的洪水增加的一致性.
主要方法:
- 从1900年至2023年间的883个奥地利站的综合数据集进行分析.
- 两个独立的气象网络之间的趋势比较.
- 与温度数据和大气循环指数的相关性分析.
主要成果:
- 在过去的40年里,每天大雨量增加了8%,每小时大雨量增加了15%.
- 每小时的暴雨增加与温度相关 (1°C升温7%),符合克劳西乌斯-克莱佩隆尺度.
- 每天大雨的增加与大气循环指数比温度更为相关.
- 大水域的洪水增加约为8%,小水域的洪水增加约为25%,与降雨趋势是一致的.
结论:
- 近几十年来,奥地利的每日和每小时大雨量显著增加.
- 大气循环在每日大雨变化中所起的作用比之前所认为的要大.
- 气候适应措施对洪水管理至关重要,特别是由于洪水增加而导致较小的水域.
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