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Changes in flood frequencies in Switzerland since 1500

机译:1500年以来瑞士洪水频率的变化

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In northern Switzerland, an accumulation of large flood events has occurred since the 1970s, preceded by a prolonged period with few floods (Schmocker-Fackel and Naef, 2010). How have Swiss flood frequencies changed over the past 500 years? And how does the recent increase in flood frequencies compare with other periods in this half millennium? We collected historical flood data for 14 Swiss catchments dating back to 1500 AC. All catchments experienced marked fluctuations in flood frequencies, and we were able to identify four periods of frequent flooding in northern Switzerland, lasting between 30 and 100 years (1560-1590, 1740-1790, 1820-1940 and since 1970). The current period of increased flood frequencies has not yet exceeded those observed in the past. We tested whether the flood frequency fluctuation could be explained with generalised climatic indices like solar activity or the NAO. The first three periods of low flood frequency in Switzerland correspond to periods of low solar activity. However, after 1810 no relationship between solar activity and flood frequency was found, nor could a relationship be established between reconstructed NAO indices or reconstructed Swiss temperatures. We found re-occurring spatial patterns of flood frequencies on a European scale, with the Swiss periods of frequent flooding often in phase with those in the Czech Republic, Italy and Spain and less often with those in Germany. The pattern of flooding in northern Switzerland and the Czech Republic seem to be rather similar, although the individual flood events do not match. This comparison of flooding patterns in different European countries suggests that changes in large scale atmospheric circulation are responsible for the flood frequency fluctuations.
机译:在瑞士北部,自1970年代以来,发生了大规模的洪灾事件,随后是漫长的时期,几乎没有洪灾(Schmocker-Fackel和Naef,2010年)。在过去的500年中,瑞士的洪水频率发生了怎样的变化?与最近半个世纪的其他时期相比,最近洪水频率的增加如何?我们收集了可追溯到1500 AC的14个瑞士流域的历史洪水数据。所有流域的洪水频率都有明显的波动,我们能够确定出瑞士北部的四个频繁洪水时期,持续了30至100年(1560-1590、1740-1790、1820-1940和自1970年以来)。当前洪水频率增加的时期尚未超过过去观察到的时期。我们测试了洪水频率的波动是否可以用广义的气候指数(例如太阳活动或NAO)来解释。瑞士的洪水频率较低的前三个时段对应于太阳活动较低的时段。但是,在1810年以后,没有发现太阳活动与洪水频率之间的关系,也没有在重建的NAO指数或重建的瑞士温度之间建立关系。我们发现洪水频率在欧洲范围内再次出现,瑞士的频繁洪水时期通常与捷克共和国,意大利和西班牙的时期同相,而德国则较少。尽管个别洪水事件不尽相同,但瑞士北部和捷克共和国的洪水模式似乎相当相似。对欧洲不同国家的洪水模式的比较表明,大规模大气环流的变化是洪水频率波动的原因。

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