European floods during the winter 1783/1784: scenarios of an
extreme event during the

J 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.

Základní údaje

Originální název

European floods during the winter 1783/1784: scenarios of an extreme event during the "Little Ice Age"

Autoři

BRÁZDIL, Rudolf; Gaston R. DEMARÉE; Mathias DEUTSCH; Emmanuel GARNIER; Andrea KISS; Jürg LUTERBACHER; Neil MACDONALD; Christian ROHR; Petr DOBROVOLNÝ; Petr KOLÁŘ a Kateřina CHROMÁ

Vydání

Theor. Appl. Climatol. 2010, 0177-798X

Další údaje

Jazyk

angličtina

Typ výsledku

Článek v odborném periodiku

Obor

10500 1.5. Earth and related environmental sciences

Stát vydavatele

Rakousko

Utajení

není předmětem státního či obchodního tajemství

Odkazy

URL

Impakt faktor

Impact factor: 1.684

Označené pro přenos do RIV

Ano

Kód RIV

RIV/00216224:14310/10:00043406

Organizační jednotka

Přírodovědecká fakulta

UT WoS

000274719000013

Klíčová slova anglicky

Europe; floods; extreme events; Little Ice Age

Příznaky

Mezinárodní význam, Recenzováno

Změněno: 29. 9. 2010 14:26, prof. RNDr. Petr Dobrovolný, CSc.

Anotace

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.

Návaznosti

MSM0021622412, záměr

Název: Interakce mezi chemickými látkami, prostředím a biologickými systémy a jejich důsledky na globální, regionální a lokální úrovni (INCHEMBIOL) (Akronym: INCHEMBIOL)

Investor: Ministerstvo školství, mládeže a tělovýchovy ČR, Interakce mezi chemickými látkami, prostředím a biologickými systémy a jejich důsledky na globální , regionální a lokální úrovni

Citovat

BRÁZDIL, Rudolf; Gaston R. DEMARÉE; Mathias DEUTSCH; Emmanuel GARNIER; Andrea KISS; Jürg LUTERBACHER; Neil MACDONALD; Christian ROHR; Petr DOBROVOLNÝ; Petr KOLÁŘ a Kateřina CHROMÁ. European floods during the winter 1783/1784: scenarios of an extreme event during the "Little Ice Age". Theor. Appl. Climatol. 2010, roč. 100, 1-2, s. 163-189. ISSN 0177-798X.

@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 a Kateřina CHROMÁ. European floods during the winter 1783/1784: scenarios of an extreme event during the ''Little Ice Age''. \textit{Theor. Appl. Climatol.}. 2010, roč.~100, 1-2, s.~163-189. ISSN~0177-798X.

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