R. Brázdil, L. Řezníčková, M. Havlíček, L. Elleder
{"title":"Floods in the Czech Republic","authors":"R. Brázdil, L. Řezníčková, M. Havlíček, L. Elleder","doi":"10.1201/B12348-9","DOIUrl":null,"url":null,"abstract":"A number of disastrous floods in Czech Republic in the 1997–\n2010 period, in which lives were lost and great material damage\ndone, brought floods to the forefront of attention among\nnatural extremes in this country. This paper presents the\n1901–2010 flood series for the River Vltava (Moldau) – the\nPrague-Chuchle station; the Ohře (Eger) – Louny; the Labe\n(Elbe) – Děcin; the Odra (Oder) – Bohumin; and the Morava –\nKroměřiž. To be included in the analysis, a flood had to fulfil\nQk >= Q2, in which Qk is peak flood discharge and Q2 is the\ncalculated peak discharge rate with a return period of two\nyears. Flood patterns are influenced by climatic fluctuations\n(increase in temperatures, more-or-less stable or slightly\ndecreasing precipitation totals), changes in land-use (increase\nin the area of arable land to the 1950s followed by decrease,\nsteadily enlarging forest area, decrease in meadows and\npastures) and by human interventions on the rivers (adjustment\nof channels, water structures – mainly reservoirs, extensively\nbuilt in the 20th century). The highest decadal frequency of\nfloods occurred in the first half of the 20th century (on the\nOhře in 1911–1920, the Odra and Morava in 1931–1940, the Vltava\nand Labe in 1941–1950). While in Bohemia winter floods\n(snowmelt often accompanied by rain, ice-jams) clearly prevail,\nthe numbers of summer floods (from heavy rain spells) increases\nin the River Morava catchment and clearly predominates on the\nRiver Odra. The most disastrous floods, of July 1903,\nAugust/September 1938, March 1940, July 1997 and August 2002,\nare described in greater detail.","PeriodicalId":340268,"journal":{"name":"Changes in Flood Risk in Europe","volume":"7 1","pages":"0"},"PeriodicalIF":0.0000,"publicationDate":"1900-01-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"16","resultStr":null,"platform":"Semanticscholar","paperid":null,"PeriodicalName":"Changes in Flood Risk in Europe","FirstCategoryId":"1085","ListUrlMain":"https://doi.org/10.1201/B12348-9","RegionNum":0,"RegionCategory":null,"ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"","JCRName":"","Score":null,"Total":0}
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.