Responses of large volcanic eruptions in the instrumental and documentary climatic data over Central Europe
Abstract Responses of large volcanic eruptions in selected long temperature series from Austria, the Czech Republic and Germany as well as in three global radiation series in Central Europe are studied. In the example of seven large tropical eruptions (Krakatau 1883; Pelée, Soufriére and Santa María...
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crwiley:10.1002/joc.1249 2024-06-02T08:07:50+00:00 Responses of large volcanic eruptions in the instrumental and documentary climatic data over Central Europe Písek, Jan Brázdil, Rudolf 2006 http://dx.doi.org/10.1002/joc.1249 https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1002%2Fjoc.1249 https://rmets.onlinelibrary.wiley.com/doi/pdf/10.1002/joc.1249 en eng Wiley http://onlinelibrary.wiley.com/termsAndConditions#vor International Journal of Climatology volume 26, issue 4, page 439-459 ISSN 0899-8418 1097-0088 journal-article 2006 crwiley https://doi.org/10.1002/joc.1249 2024-05-03T10:56:50Z Abstract Responses of large volcanic eruptions in selected long temperature series from Austria, the Czech Republic and Germany as well as in three global radiation series in Central Europe are studied. In the example of seven large tropical eruptions (Krakatau 1883; Pelée, Soufriére and Santa María 1902; Agung, 1963; El Chichón, 1982; Mt Pinatubo, 1991) it has been demonstrated that volcanic signal in regional series is not so strongly expressed as in the hemispheric scale owing to different local effects and circulation patterns. This is also valid in the case of two further discussed eruptions of Tambora (1815) and Katmai (1912). The responses of eruptions in areas closer to Central Europe such as Iceland or Italy are more important. In nine analysed cases with VEI = 4–5 with a single exception of the Hekla eruption (1917), cold seasons were observed to follow the eruption. Responses to the Lakagígar eruption (1783) of Iceland with important impacts are also discussed in detail. Moreover, correlation between temperatures (annual and winter half‐year series) and NAOI is prevailingly smaller for the period following eruptions than in the period preceding eruptions. The importance of documentary evidence as a valuable source of the information about the impacts of volcanic eruptions is demonstrated. Copyright © 2006 Royal Meteorological Society. Article in Journal/Newspaper Hekla Iceland Wiley Online Library Lakagígar ENVELOPE(-18.110,-18.110,64.128,64.128) International Journal of Climatology 26 4 439 459 |
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Wiley Online Library |
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crwiley |
language |
English |
description |
Abstract Responses of large volcanic eruptions in selected long temperature series from Austria, the Czech Republic and Germany as well as in three global radiation series in Central Europe are studied. In the example of seven large tropical eruptions (Krakatau 1883; Pelée, Soufriére and Santa María 1902; Agung, 1963; El Chichón, 1982; Mt Pinatubo, 1991) it has been demonstrated that volcanic signal in regional series is not so strongly expressed as in the hemispheric scale owing to different local effects and circulation patterns. This is also valid in the case of two further discussed eruptions of Tambora (1815) and Katmai (1912). The responses of eruptions in areas closer to Central Europe such as Iceland or Italy are more important. In nine analysed cases with VEI = 4–5 with a single exception of the Hekla eruption (1917), cold seasons were observed to follow the eruption. Responses to the Lakagígar eruption (1783) of Iceland with important impacts are also discussed in detail. Moreover, correlation between temperatures (annual and winter half‐year series) and NAOI is prevailingly smaller for the period following eruptions than in the period preceding eruptions. The importance of documentary evidence as a valuable source of the information about the impacts of volcanic eruptions is demonstrated. Copyright © 2006 Royal Meteorological Society. |
format |
Article in Journal/Newspaper |
author |
Písek, Jan Brázdil, Rudolf |
spellingShingle |
Písek, Jan Brázdil, Rudolf Responses of large volcanic eruptions in the instrumental and documentary climatic data over Central Europe |
author_facet |
Písek, Jan Brázdil, Rudolf |
author_sort |
Písek, Jan |
title |
Responses of large volcanic eruptions in the instrumental and documentary climatic data over Central Europe |
title_short |
Responses of large volcanic eruptions in the instrumental and documentary climatic data over Central Europe |
title_full |
Responses of large volcanic eruptions in the instrumental and documentary climatic data over Central Europe |
title_fullStr |
Responses of large volcanic eruptions in the instrumental and documentary climatic data over Central Europe |
title_full_unstemmed |
Responses of large volcanic eruptions in the instrumental and documentary climatic data over Central Europe |
title_sort |
responses of large volcanic eruptions in the instrumental and documentary climatic data over central europe |
publisher |
Wiley |
publishDate |
2006 |
url |
http://dx.doi.org/10.1002/joc.1249 https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1002%2Fjoc.1249 https://rmets.onlinelibrary.wiley.com/doi/pdf/10.1002/joc.1249 |
long_lat |
ENVELOPE(-18.110,-18.110,64.128,64.128) |
geographic |
Lakagígar |
geographic_facet |
Lakagígar |
genre |
Hekla Iceland |
genre_facet |
Hekla Iceland |
op_source |
International Journal of Climatology volume 26, issue 4, page 439-459 ISSN 0899-8418 1097-0088 |
op_rights |
http://onlinelibrary.wiley.com/termsAndConditions#vor |
op_doi |
https://doi.org/10.1002/joc.1249 |
container_title |
International Journal of Climatology |
container_volume |
26 |
container_issue |
4 |
container_start_page |
439 |
op_container_end_page |
459 |
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1800752964369907712 |