No upward trends in the occurrence of extreme floods in central Europe

被引:290
作者
Mudelsee, M
Börngen, M
Tetzlaff, G
Grünewald, U
机构
[1] Univ Leipzig, Inst Meteorol, D-04103 Leipzig, Germany
[2] Tech Univ Cottbus, Inst Hydrol, D-03103 Cottbus, Germany
关键词
D O I
10.1038/nature01928
中图分类号
O [数理科学和化学]; P [天文学、地球科学]; Q [生物科学]; N [自然科学总论];
学科分类号
07 ; 0710 ; 09 ;
摘要
Extreme river floods have been a substantial natural hazard in Europe over the past centuries(1), and radiative effects of recent anthropogenic changes in atmospheric composition are expected to cause climate changes, especially enhancement of the hydrological cycle(2), leading to an increased flood risk(3,4). For the past few decades, however, observations from Europe(1,5-7) do not show a clear increase in flood occurrence rate. Here we present longer-term records of winter and summer floods in two of the largest rivers in central Europe, the Elbe and Oder rivers. For the past 80 to 150 yr, we find a decrease in winter flood occurrence in both rivers, while summer floods show no trend, consistent with trends in extreme precipitation occurrence. The reduction in winter flood occurrence can partly be attributed to fewer events of strong freezing-following such events, breaking river ice at the end of the winter may function as a water barrier and enhance floods severely. Additionally, we detect significant long-term changes in flood occurrence rates in the sixteenth to nineteenth centuries, and conclude that reductions in river length, construction of reservoirs and deforestation have had minor effects on flood frequency.
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页码:166 / 169
页数:4
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