Detailed Information on Publication Record
2017
Climatic and other responses to the Lakagígar 1783 and Tambora 1815 volcanic eruptions in the Czech Lands
BRÁZDIL, Rudolf, Ladislava ŘEZNÍČKOVÁ, Hubert VALÁŠEK, Lukáš DOLÁK, Oldřich KOTYZA et. al.Basic information
Original name
Climatic and other responses to the Lakagígar 1783 and Tambora 1815 volcanic eruptions in the Czech Lands
Authors
BRÁZDIL, Rudolf (203 Czech Republic, guarantor, belonging to the institution), Ladislava ŘEZNÍČKOVÁ (203 Czech Republic, belonging to the institution), Hubert VALÁŠEK (203 Czech Republic), Lukáš DOLÁK (203 Czech Republic, belonging to the institution) and Oldřich KOTYZA (203 Czech Republic)
Edition
Geografie, Prague, Česká geografická společnost, 2017, 1212-0014
Other information
Language
English
Type of outcome
Článek v odborném periodiku
Field of Study
10510 Climatic research
Country of publisher
Czech Republic
Confidentiality degree
není předmětem státního či obchodního tajemství
Impact factor
Impact factor: 0.745
RIV identification code
RIV/00216224:14310/17:00094809
Organization unit
Faculty of Science
UT WoS
000404784100002
Keywords in English
Lakagígar eruption; Tambora eruption; climatic effects; human impacts; Czech Lands
Změněno: 1/11/2019 14:53, Mgr. Michal Petr
Abstract
V originále
Using documentary data and long-term temperature and precipitation series for the years 1775-2007, climatic, weather and other phenomena in the Czech Lands following the 1783 Lakagígar eruption in Iceland and the 1815 Tambora eruption in Indonesia are investigated. The Lakagígar eruption had clear post volcanic effects on the weather in central Europe (dry fog, heavy thunderstorms, optical phenomena), with the occurrence of significant cold temperature anomalies in winter 1783/84, spring 1785 and the summer and autumn of 1786. The Tambora eruption was not accompanied by any particular weather phenomena, but was followed by an extremely cold summer in 1816. A comparison of the two eruptions shows that the effects of the Lakagígar eruption were climatologically stronger than those of the Tambora eruption.
Links
GA13-19831S, research and development project |
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