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WFRF:(Churakova Sidorova Olga V.)
 

Sökning: WFRF:(Churakova Sidorova Olga V.) > Prominent role of v...

LIBRIS Formathandbok  (Information om MARC21)
FältnamnIndikatorerMetadata
00004733naa a2200685 4500
001oai:gup.ub.gu.se/298534
003SwePub
008240528s2020 | |||||||||||000 ||eng|
009oai:DiVA.org:su-190698
0247 a https://gup.ub.gu.se/publication/2985342 URI
0247 a https://doi.org/10.1016/j.dendro.2020.1257572 DOI
0247 a https://urn.kb.se/resolve?urn=urn:nbn:se:su:diva-1906982 URI
040 a (SwePub)gud (SwePub)su
041 a eng
042 9 SwePub
072 7a ref2 swepub-contenttype
072 7a art2 swepub-publicationtype
1001 a Büntgen, Ulf4 aut
2451 0a Prominent role of volcanism in Common Era climate variability and human history
264 1b Elsevier BV,c 2020
520 a © 2020 Elsevier GmbH Climate reconstructions for the Common Era are compromised by the paucity of annually-resolved and absolutely-dated proxy records prior to medieval times. Where reconstructions are based on combinations of different climate archive types (of varying spatiotemporal resolution, dating uncertainty, record length and predictive skill), it is challenging to estimate past amplitude ranges, disentangle the relative roles of natural and anthropogenic forcing, or probe deeper interrelationships between climate variability and human history. Here, we compile and analyse updated versions of all the existing summer temperature sensitive tree-ring width chronologies from the Northern Hemisphere that span the entire Common Era. We apply a novel ensemble approach to reconstruct extra-tropical summer temperatures from 1 to 2010 CE, and calculate uncertainties at continental to hemispheric scales. Peak warming in the 280s, 990s and 1020s, when volcanic forcing was low, was comparable to modern conditions until 2010 CE. The lowest June–August temperature anomaly in 536 not only marks the beginning of the coldest decade, but also defines the onset of the Late Antique Little Ice Age (LALIA). While prolonged warmth during Roman and medieval times roughly coincides with the tendency towards societal prosperity across much of the North Atlantic/European sector and East Asia, major episodes of volcanically-forced summer cooling often presaged widespread famines, plague outbreaks and political upheavals. Our study reveals a larger amplitude of spatially synchronized summer temperature variation during the first millennium of the Common Era than previously recognised.
650 7a NATURVETENSKAPx Geovetenskap och miljövetenskapx Klimatforskning0 (SwePub)105012 hsv//swe
650 7a NATURAL SCIENCESx Earth and Related Environmental Sciencesx Climate Research0 (SwePub)105012 hsv//eng
650 7a NATURVETENSKAPx Geovetenskap och miljövetenskap0 (SwePub)1052 hsv//swe
650 7a NATURAL SCIENCESx Earth and Related Environmental Sciences0 (SwePub)1052 hsv//eng
653 a Climate reconstruction
653 a Dendroclimatology
653 a Human history
653 a Northern Hemisphere
653 a Tree-ring width
653 a Volcanic eruptions
653 a Climate reconstruction
7001 a Arseneault, Dominique4 aut
7001 a Boucher, Étienne4 aut
7001 a Churakova (Sidorova), Olga V.4 aut
7001 a Gennaretti, Fabio4 aut
7001 a Crivellaro, Alan4 aut
7001 a Hughes, Malcolm K.4 aut
7001 a Kirdyanov, Alexander V.4 aut
7001 a Klippel, Lara4 aut
7001 a Krusic, Paul J.u Stockholms universitet,Institutionen för naturgeografi,University of Cambridge, UK4 aut0 (Swepub:su)pakru
7001 a Linderholm, Hans W.,d 1968u Gothenburg University,Göteborgs universitet,Institutionen för geovetenskaper,Department of Earth Sciences4 aut0 (Swepub:gu)xlinha
7001 a C. Ljungqvist, Fredriku Stockholms universitet,Historiska institutionen,Swedish Collegium for Advanced Study, Sweden4 aut0 (Swepub:su)fchar
7001 a Ludescher, Josef4 aut
7001 a McCormick, Michael4 aut
7001 a Myglan, Vladimir S.4 aut
7001 a Nicolussi, Kurt4 aut
7001 a Piermattei, Alma4 aut
7001 a Oppenheimer, Clive4 aut
7001 a Reinig, Frederick4 aut
7001 a Sigl, Michael4 aut
7001 a Vaganov, Eugene A.4 aut
7001 a Esper, Jan4 aut
7102 a Stockholms universitetb Institutionen för naturgeografi4 org
7730 t Dendrochronologiad : Elsevier BVg 64q 64x 1125-7865x 1612-0051
8564 u https://doi.org/10.1016/j.dendro.2020.125757
8564 u https://doi.org/10.1016/j.dendro.2020.125757y Fulltext
8564 8u https://gup.ub.gu.se/publication/298534
8564 8u https://doi.org/10.1016/j.dendro.2020.125757
8564 8u https://urn.kb.se/resolve?urn=urn:nbn:se:su:diva-190698

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