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Statements

Subject Item
n2:RIV%2F00216208%3A11310%2F14%3A10281681%21RIV15-MSM-11310___
rdf:type
skos:Concept n18:Vysledek
dcterms:description
This paper describes the reconstruction of the geomorphologic and landscape effects of the most catastrophic flood owing to dam failure within the territory of today's Czech Republic, namely, the Bílá Desná dam failure of 1916. Because of the realisation of the significant later transformation of the Bílá Desná river catchment almost 100 years after the flood event, the field research performed during the summer and fall of 2013 had to be supported by extensive research in regional archives for documentary data. Various data types and sources (such as court investigation notes, investigation reports for insurance companies, old maps, and old photos, as well as video and recorded testimonies of survivors) were used to reconstruct the magnitude (discharge, flood wave extent) of the flood and its effects on the channel morphology and landscape. According to the reconstruction of the dam failure, which was caused by the internal erosion of the dam, the calculated peak discharge ranged between 418.2 and 1491.7 m3sMINUS SIGN 1 and therefore exceeded the mean flow rate of the Bílá Desná River by more than 850 times. The river channel immediately upstream and downstream of the dam reclaimed its former meandering pattern with higher sinuosity, and new gravel point bars and irregular bars have been formed. Moreover, the river channel immediately below the dam shifted by up to 30 m following the flood wave. The most significant flood impacts were apparent in the village of Desná, where the flood wave, together with transported boulders (up to 2 m in diametre) and logs from sawmills situated upstream, killed 62 inhabitants and damaged or destroyed 101 buildings. The reconstructed flood wave in the towns of Desná and Tanvald exceeded the bankfull water level twice, with a width ranging between ~ 50 and 250 m in contrast to the average channel width of a few metres. This paper describes the reconstruction of the geomorphologic and landscape effects of the most catastrophic flood owing to dam failure within the territory of today's Czech Republic, namely, the Bílá Desná dam failure of 1916. Because of the realisation of the significant later transformation of the Bílá Desná river catchment almost 100 years after the flood event, the field research performed during the summer and fall of 2013 had to be supported by extensive research in regional archives for documentary data. Various data types and sources (such as court investigation notes, investigation reports for insurance companies, old maps, and old photos, as well as video and recorded testimonies of survivors) were used to reconstruct the magnitude (discharge, flood wave extent) of the flood and its effects on the channel morphology and landscape. According to the reconstruction of the dam failure, which was caused by the internal erosion of the dam, the calculated peak discharge ranged between 418.2 and 1491.7 m3sMINUS SIGN 1 and therefore exceeded the mean flow rate of the Bílá Desná River by more than 850 times. The river channel immediately upstream and downstream of the dam reclaimed its former meandering pattern with higher sinuosity, and new gravel point bars and irregular bars have been formed. Moreover, the river channel immediately below the dam shifted by up to 30 m following the flood wave. The most significant flood impacts were apparent in the village of Desná, where the flood wave, together with transported boulders (up to 2 m in diametre) and logs from sawmills situated upstream, killed 62 inhabitants and damaged or destroyed 101 buildings. The reconstructed flood wave in the towns of Desná and Tanvald exceeded the bankfull water level twice, with a width ranging between ~ 50 and 250 m in contrast to the average channel width of a few metres.
dcterms:title
The 1916 catastrophic flood following the Bílá Desná dam failure: The role of historical data sources in the reconstruction of its geomorphologic and landscape effects The 1916 catastrophic flood following the Bílá Desná dam failure: The role of historical data sources in the reconstruction of its geomorphologic and landscape effects
skos:prefLabel
The 1916 catastrophic flood following the Bílá Desná dam failure: The role of historical data sources in the reconstruction of its geomorphologic and landscape effects The 1916 catastrophic flood following the Bílá Desná dam failure: The role of historical data sources in the reconstruction of its geomorphologic and landscape effects
skos:notation
RIV/00216208:11310/14:10281681!RIV15-MSM-11310___
n3:aktivita
n19:S n19:P
n3:aktivity
P(GP13-02080P), S
n3:cisloPeriodika
December
n3:dodaniDat
n13:2015
n3:domaciTvurceVysledku
n16:3932648
n3:druhVysledku
n5:J
n3:duvernostUdaju
n14:S
n3:entitaPredkladatele
n12:predkladatel
n3:idSjednocenehoVysledku
58133
n3:idVysledku
RIV/00216208:11310/14:10281681
n3:jazykVysledku
n8:eng
n3:klicovaSlova
Reconstruction of landscape effects; Catastrophic flood; Historical data sources; Man-made dam failure
n3:klicoveSlovo
n4:Reconstruction%20of%20landscape%20effects n4:Historical%20data%20sources n4:Catastrophic%20flood n4:Man-made%20dam%20failure
n3:kodStatuVydavatele
NL - Nizozemsko
n3:kontrolniKodProRIV
[EFE2EB1B9D9D]
n3:nazevZdroje
Geomorphology
n3:obor
n7:DE
n3:pocetDomacichTvurcuVysledku
1
n3:pocetTvurcuVysledku
2
n3:projekt
n10:GP13-02080P
n3:rokUplatneniVysledku
n13:2014
n3:svazekPeriodika
226
n3:tvurceVysledku
Emmer, Adam Raška, Pavel
n3:wos
000343351300011
s:issn
0169-555X
s:numberOfPages
13
n17:doi
10.1016/j.geomorph.2014.08.002
n15:organizacniJednotka
11310