Floods in the Czech Republic

R. Brázdil, L. Řezníčková, M. Havlíček, L. Elleder
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引用次数: 16

Abstract

A number of disastrous floods in Czech Republic in the 1997– 2010 period, in which lives were lost and great material damage done, brought floods to the forefront of attention among natural extremes in this country. This paper presents the 1901–2010 flood series for the River Vltava (Moldau) – the Prague-Chuchle station; the Ohře (Eger) – Louny; the Labe (Elbe) – Děcin; the Odra (Oder) – Bohumin; and the Morava – Kroměřiž. To be included in the analysis, a flood had to fulfil Qk >= Q2, in which Qk is peak flood discharge and Q2 is the calculated peak discharge rate with a return period of two years. Flood patterns are influenced by climatic fluctuations (increase in temperatures, more-or-less stable or slightly decreasing precipitation totals), changes in land-use (increase in the area of arable land to the 1950s followed by decrease, steadily enlarging forest area, decrease in meadows and pastures) and by human interventions on the rivers (adjustment of channels, water structures – mainly reservoirs, extensively built in the 20th century). The highest decadal frequency of floods occurred in the first half of the 20th century (on the Ohře in 1911–1920, the Odra and Morava in 1931–1940, the Vltava and Labe in 1941–1950). While in Bohemia winter floods (snowmelt often accompanied by rain, ice-jams) clearly prevail, the numbers of summer floods (from heavy rain spells) increases in the River Morava catchment and clearly predominates on the River Odra. The most disastrous floods, of July 1903, August/September 1938, March 1940, July 1997 and August 2002, are described in greater detail.
捷克共和国发生洪水
1997年至2010年期间,捷克共和国发生了多次灾难性的洪水,造成人员伤亡和巨大的物质损失,使洪水成为这个国家最受关注的自然极端事件。本文介绍了伏尔塔瓦河(莫尔道)-布拉格-丘奇勒站1901 - 2010年的洪水序列;Ohře (Eger) - Louny;河(易北河)-湖;奥德拉(奥得语)-波胡敏;和莫拉瓦-Kroměřiž。要纳入分析,洪水必须满足Qk >= Q2,其中Qk为洪峰流量,Q2为计算出的两年回复期洪峰流量。洪水模式受气候波动(气温升高,降水总量或多或少保持稳定或略有减少)、土地利用变化(到20世纪50年代耕地面积增加,随后减少,森林面积稳步扩大,草地和牧场减少)以及人类对河流的干预(河道、水结构——主要是20世纪广泛修建的水库)的影响。年代际频率最高的洪水发生在20世纪上半叶(theOhře上1911-1920年,Odra和Morava在1931-1940年,Vltavaand Labe在1941-1950年)。在波西米亚,冬季洪水(融雪经常伴有雨水和冰塞)明显盛行,而夏季洪水(来自暴雨)的数量在摩拉瓦河流域增加,并明显在奥德拉河占主导地位。更详细地描述了1903年7月、1938年8月/ 9月、1940年3月、1997年7月和2002年8月发生的最严重的洪水。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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