Climatic effects and impacts of the 1815 eruption of Mount Tambora in the Czech Lands
Identifikátory výsledku
Kód výsledku v IS VaVaI
<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F86652079%3A_____%2F16%3A00467437" target="_blank" >RIV/86652079:_____/16:00467437 - isvavai.cz</a>
Nalezeny alternativní kódy
RIV/00216224:14310/16:00087996
Výsledek na webu
<a href="http://dx.doi.org/10.5194/cp-12-1361-2016" target="_blank" >http://dx.doi.org/10.5194/cp-12-1361-2016</a>
DOI - Digital Object Identifier
<a href="http://dx.doi.org/10.5194/cp-12-1361-2016" target="_blank" >10.5194/cp-12-1361-2016</a>
Alternativní jazyky
Jazyk výsledku
angličtina
Název v původním jazyce
Climatic effects and impacts of the 1815 eruption of Mount Tambora in the Czech Lands
Popis výsledku v původním jazyce
The eruption of Mount Tambora in Indonesia in 1815 was one of the most powerful of its kind in recorded history. This contribution addresses climatic responses to it, the post-eruption weather, and its impacts on human life in the Czech Lands. The climatic effects are evaluated in terms of air temperature and precipitation on the basis of long-term homogenised series from the Prague-Klementinum and Brno meteorological stations, and mean Czech series in the short term (1810-1820) and long term (1800-2010). This analysis is complemented by other climatic and environmental data derived from rich documentary evidence. Czech documentary sources make no direct mention of the Tambora eruption, neither do they relate any particular weather phenomena to it, but they record an extremely wet summer for 1815 and an extremely cold summer for 1816 (the 'Year Without a Summer') that contributed to bad grain harvests and widespread grain price increases in 1817. Possible reasons for the cold summers in the first decade of the 19th century reflected in the contemporary press included comets, sunspot activity, long-term cooling and finally as late as 1817 earthquakes with volcanic eruptions.
Název v anglickém jazyce
Climatic effects and impacts of the 1815 eruption of Mount Tambora in the Czech Lands
Popis výsledku anglicky
The eruption of Mount Tambora in Indonesia in 1815 was one of the most powerful of its kind in recorded history. This contribution addresses climatic responses to it, the post-eruption weather, and its impacts on human life in the Czech Lands. The climatic effects are evaluated in terms of air temperature and precipitation on the basis of long-term homogenised series from the Prague-Klementinum and Brno meteorological stations, and mean Czech series in the short term (1810-1820) and long term (1800-2010). This analysis is complemented by other climatic and environmental data derived from rich documentary evidence. Czech documentary sources make no direct mention of the Tambora eruption, neither do they relate any particular weather phenomena to it, but they record an extremely wet summer for 1815 and an extremely cold summer for 1816 (the 'Year Without a Summer') that contributed to bad grain harvests and widespread grain price increases in 1817. Possible reasons for the cold summers in the first decade of the 19th century reflected in the contemporary press included comets, sunspot activity, long-term cooling and finally as late as 1817 earthquakes with volcanic eruptions.
Klasifikace
Druh
J<sub>x</sub> - Nezařazeno - Článek v odborném periodiku (Jimp, Jsc a Jost)
CEP obor
EH - Ekologie – společenstva
OECD FORD obor
—
Návaznosti výsledku
Projekt
Výsledek vznikl pri realizaci vícero projektů. Více informací v záložce Projekty.
Návaznosti
I - Institucionalni podpora na dlouhodoby koncepcni rozvoj vyzkumne organizace
Ostatní
Rok uplatnění
2016
Kód důvěrnosti údajů
S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů
Údaje specifické pro druh výsledku
Název periodika
Climate of the Past
ISSN
1814-9324
e-ISSN
—
Svazek periodika
12
Číslo periodika v rámci svazku
6
Stát vydavatele periodika
DE - Spolková republika Německo
Počet stran výsledku
14
Strana od-do
1361-1374
Kód UT WoS článku
000379420600005
EID výsledku v databázi Scopus
2-s2.0-84975799340