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@article{873446, author = {Brázdil, Rudolf and Demarée, Gaston R. and Deutsch, Mathias and Garnier, Emmanuel and Kiss, Andrea and Luterbacher, Jürg and Macdonald, Neil and Rohr, Christian and Dobrovolný, Petr and Kolář, Petr and Chromá, Kateřina}, article_number = {1-2}, keywords = {Europe; floods; extreme events; Little Ice Age}, language = {eng}, issn = {0177-798X}, journal = {Theor. Appl. Climatol.}, title = {European floods during the winter 1783/1784: scenarios of an extreme event during the "Little Ice Age"}, url = {http://www.springerlink.com/content/0w541g348867u448/?p=f875454dcf6d4e879b09c34578c13d33&pi=12}, volume = {100}, year = {2010} }
TY - JOUR ID - 873446 AU - Brázdil, Rudolf - Demarée, Gaston R. - Deutsch, Mathias - Garnier, Emmanuel - Kiss, Andrea - Luterbacher, Jürg - Macdonald, Neil - Rohr, Christian - Dobrovolný, Petr - Kolář, Petr - Chromá, Kateřina PY - 2010 TI - European floods during the winter 1783/1784: scenarios of an extreme event during the "Little Ice Age" JF - Theor. Appl. Climatol. VL - 100 IS - 1-2 SP - 163-189 EP - 163-189 SN - 0177798X KW - Europe KW - floods KW - extreme events KW - Little Ice Age UR - http://www.springerlink.com/content/0w541g348867u448/?p=f875454dcf6d4e879b09c34578c13d33&pi=12 N2 - 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. ER -
BRÁZDIL, Rudolf, Gaston R. DEMARÉE, Mathias DEUTSCH, Emmanuel GARNIER, Andrea KISS, Jürg LUTERBACHER, Neil MACDONALD, Christian ROHR, Petr DOBROVOLNÝ, Petr KOLÁŘ and Kateřina CHROMÁ. European floods during the winter 1783/1784: scenarios of an extreme event during the ''Little Ice Age''. \textit{Theor. Appl. Climatol.}. 2010, vol.~100, 1-2, p.~163-189. ISSN~0177-798X.
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