The Eldgja eruption: timing, long-range impacts and influence on the Christianisation of Iceland
Identifikátory výsledku
Kód výsledku v IS VaVaI
<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F00216224%3A14310%2F18%3A00113401" target="_blank" >RIV/00216224:14310/18:00113401 - isvavai.cz</a>
Nalezeny alternativní kódy
RIV/86652079:_____/18:00496041
Výsledek na webu
<a href="https://link.springer.com/article/10.1007/s10584-018-2171-9" target="_blank" >https://link.springer.com/article/10.1007/s10584-018-2171-9</a>
DOI - Digital Object Identifier
<a href="http://dx.doi.org/10.1007/s10584-018-2171-9" target="_blank" >10.1007/s10584-018-2171-9</a>
Alternativní jazyky
Jazyk výsledku
angličtina
Název v původním jazyce
The Eldgja eruption: timing, long-range impacts and influence on the Christianisation of Iceland
Popis výsledku v původním jazyce
The Eldgja lava flood is considered Iceland's largest volcanic eruption of the Common Era. While it is well established that it occurred after the Settlement of Iceland (circa 874 CE), the date of this great event has remained uncertain. This has hampered investigation of the eruption's impacts, if any, on climate and society. Here, we use high-temporal resolution glaciochemical records from Greenland to show that the eruption began in spring 939 CE and continued, at least episodically, until at least autumn 940 CE. Contemporary chronicles identify the spread of a remarkable haze in 939 CE, and tree ring-based reconstructions reveal pronounced northern hemisphere summer cooling in 940 CE, consistent with the eruption's high yield of sulphur to the atmosphere. Consecutive severe winters and privations may also be associated with climatic effects of the volcanic aerosol veil. Iceland's formal conversion to Christianity dates to 999/1000 CE, within two generations or so of the Eldgja eruption. The end of the pagan pantheon is foretold in Iceland's renowned medieval poem, VC << luspa ('the prophecy of the seeress'). Several lines of the poem describe dramatic eruptive activity and attendant meteorological effects in an allusion to the fiery terminus of the pagan gods. We suggest that they draw on first-hand experiences of the Eldgja eruption and that this retrospection of harrowing volcanic events in the poem was intentional, with the purpose of stimulating Iceland's Christianisation over the latter half of the tenth century.
Název v anglickém jazyce
The Eldgja eruption: timing, long-range impacts and influence on the Christianisation of Iceland
Popis výsledku anglicky
The Eldgja lava flood is considered Iceland's largest volcanic eruption of the Common Era. While it is well established that it occurred after the Settlement of Iceland (circa 874 CE), the date of this great event has remained uncertain. This has hampered investigation of the eruption's impacts, if any, on climate and society. Here, we use high-temporal resolution glaciochemical records from Greenland to show that the eruption began in spring 939 CE and continued, at least episodically, until at least autumn 940 CE. Contemporary chronicles identify the spread of a remarkable haze in 939 CE, and tree ring-based reconstructions reveal pronounced northern hemisphere summer cooling in 940 CE, consistent with the eruption's high yield of sulphur to the atmosphere. Consecutive severe winters and privations may also be associated with climatic effects of the volcanic aerosol veil. Iceland's formal conversion to Christianity dates to 999/1000 CE, within two generations or so of the Eldgja eruption. The end of the pagan pantheon is foretold in Iceland's renowned medieval poem, VC << luspa ('the prophecy of the seeress'). Several lines of the poem describe dramatic eruptive activity and attendant meteorological effects in an allusion to the fiery terminus of the pagan gods. We suggest that they draw on first-hand experiences of the Eldgja eruption and that this retrospection of harrowing volcanic events in the poem was intentional, with the purpose of stimulating Iceland's Christianisation over the latter half of the tenth century.
Klasifikace
Druh
J<sub>imp</sub> - Článek v periodiku v databázi Web of Science
CEP obor
—
OECD FORD obor
10500 - Earth and related environmental sciences
Návaznosti výsledku
Projekt
—
Návaznosti
I - Institucionalni podpora na dlouhodoby koncepcni rozvoj vyzkumne organizace
Ostatní
Rok uplatnění
2018
Kód důvěrnosti údajů
S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů
Údaje specifické pro druh výsledku
Název periodika
Climatic Change
ISSN
0165-0009
e-ISSN
—
Svazek periodika
147
Číslo periodika v rámci svazku
3-4
Stát vydavatele periodika
NL - Nizozemsko
Počet stran výsledku
13
Strana od-do
369-381
Kód UT WoS článku
000428427200001
EID výsledku v databázi Scopus
2-s2.0-85044019279