Detailed Information on Publication Record
2010
European floods during the winter 1783/1784: scenarios of an extreme event during the "Little Ice Age"
BRÁZDIL, Rudolf, Gaston R. DEMARÉE, Mathias DEUTSCH, Emmanuel GARNIER, Andrea KISS et. al.Basic information
Original name
European floods during the winter 1783/1784: scenarios of an extreme event during the "Little Ice Age"
Authors
BRÁZDIL, Rudolf (203 Czech Republic, guarantor), Gaston R. DEMARÉE (56 Belgium), Mathias DEUTSCH (276 Germany), Emmanuel GARNIER (250 France), Andrea KISS (348 Hungary), Jürg LUTERBACHER (756 Switzerland), Neil MACDONALD (826 United Kingdom of Great Britain and Northern Ireland), Christian ROHR (40 Austria), Petr DOBROVOLNÝ (203 Czech Republic), Petr KOLÁŘ (203 Czech Republic) and Kateřina CHROMÁ (203 Czech Republic)
Edition
Theor. Appl. Climatol. 2010, 0177-798X
Other information
Language
English
Type of outcome
Článek v odborném periodiku
Field of Study
10500 1.5. Earth and related environmental sciences
Country of publisher
Austria
Confidentiality degree
není předmětem státního či obchodního tajemství
References:
Impact factor
Impact factor: 1.684
RIV identification code
RIV/00216224:14310/10:00043406
Organization unit
Faculty of Science
UT WoS
000274719000013
Keywords in English
Europe; floods; extreme events; Little Ice Age
Tags
International impact, Reviewed
Změněno: 29/9/2010 14:26, prof. RNDr. Petr Dobrovolný, CSc.
Abstract
V originále
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.
Links
MSM0021622412, plan (intention) |
|