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Statements

Subject Item
n2:RIV%2F00216224%3A14310%2F10%3A00043406%21RIV11-MSM-14310___
rdf:type
skos:Concept n17:Vysledek
dcterms:description
The Lakagígar eruption in Iceland during 1783 was followed by the severe winter of 1783/1784, which was characterised by low temperatures, frozen soils, icebound watercourses and high rates of snow accumulation across much of Europe. Sudden warming coupled with rainfall led to rapid snowmelt, resulting in a series of flooding phases across much of Europe. The second phase at the turn of February-March 1784 was of greater extent, generated by the melting of an unusually large accumulation of snow and river ice, affecting catchments across France and Central Europe (where it is still considered as one of the most disastrous known floods), throughout the Danube catchment and in southeast Central Europe. The impacts and consequences of the floods on both local and regional scales were reflected in the economic and societal responses, material damage and human losses. The winter of 1783/1784 can be considered as typical, if severe, for the Little Ice Age period across much of Europe. The Lakagígar eruption in Iceland during 1783 was followed by the severe winter of 1783/1784, which was characterised by low temperatures, frozen soils, icebound watercourses and high rates of snow accumulation across much of Europe. Sudden warming coupled with rainfall led to rapid snowmelt, resulting in a series of flooding phases across much of Europe. The second phase at the turn of February-March 1784 was of greater extent, generated by the melting of an unusually large accumulation of snow and river ice, affecting catchments across France and Central Europe (where it is still considered as one of the most disastrous known floods), throughout the Danube catchment and in southeast Central Europe. The impacts and consequences of the floods on both local and regional scales were reflected in the economic and societal responses, material damage and human losses. The winter of 1783/1784 can be considered as typical, if severe, for the Little Ice Age period across much of Europe.
dcterms:title
European floods during the winter 1783/1784: scenarios of an extreme event during the %22Little Ice Age%22 European floods during the winter 1783/1784: scenarios of an extreme event during the %22Little Ice Age%22
skos:prefLabel
European floods during the winter 1783/1784: scenarios of an extreme event during the %22Little Ice Age%22 European floods during the winter 1783/1784: scenarios of an extreme event during the %22Little Ice Age%22
skos:notation
RIV/00216224:14310/10:00043406!RIV11-MSM-14310___
n3:aktivita
n7:Z
n3:aktivity
Z(MSM0021622412)
n3:cisloPeriodika
1-2
n3:dodaniDat
n11:2011
n3:domaciTvurceVysledku
n4:6007929 Kiss, Andrea n4:2672537 Rohr, Christian n4:1593552 n4:1020048
n3:druhVysledku
n12:J
n3:duvernostUdaju
n9:S
n3:entitaPredkladatele
n15:predkladatel
n3:idSjednocenehoVysledku
257720
n3:idVysledku
RIV/00216224:14310/10:00043406
n3:jazykVysledku
n16:eng
n3:klicovaSlova
Europe; floods; extreme events; Little Ice Age
n3:klicoveSlovo
n5:Little%20Ice%20Age n5:floods n5:extreme%20events n5:Europe
n3:kodStatuVydavatele
AT - Rakouská republika
n3:kontrolniKodProRIV
[C5BE6A17CCA8]
n3:nazevZdroje
Theor. Appl. Climatol.
n3:obor
n18:DG
n3:pocetDomacichTvurcuVysledku
6
n3:pocetTvurcuVysledku
11
n3:rokUplatneniVysledku
n11:2010
n3:svazekPeriodika
100
n3:tvurceVysledku
Garnier, Emmanuel Dobrovolný, Petr Chromá, Kateřina Demarée, Gaston R. Macdonald, Neil Kolář, Petr Brázdil, Rudolf Kiss, Andrea Deutsch, Mathias Luterbacher, Jürg Rohr, Christian
n3:wos
000274719000013
n3:zamer
n6:MSM0021622412
s:issn
0177-798X
s:numberOfPages
27
n14:organizacniJednotka
14310