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Sökning: onr:"swepub:oai:DiVA.org:su-156668" > Warm summers during...

LIBRIS Formathandbok  (Information om MARC21)
FältnamnIndikatorerMetadata
00006420naa a2200565 4500
001oai:DiVA.org:su-156668
003SwePub
008180604s2018 | |||||||||||000 ||eng|
009oai:DiVA.org:kth-227217
009oai:lup.lub.lu.se:fef1917d-6990-4f64-a638-34d8717ae1c6
0247 a https://urn.kb.se/resolve?urn=urn:nbn:se:su:diva-1566682 URI
0247 a https://doi.org/10.1038/s41467-018-04071-52 DOI
0247 a https://urn.kb.se/resolve?urn=urn:nbn:se:kth:diva-2272172 URI
0247 a https://lup.lub.lu.se/record/fef1917d-6990-4f64-a638-34d8717ae1c62 URI
040 a (SwePub)sud (SwePub)kthd (SwePub)lu
041 a engb eng
042 9 SwePub
072 7a ref2 swepub-contenttype
072 7a art2 swepub-publicationtype
1001 a Schenk, Frederiku Stockholm University,KTH,Stockholms universitet,Institutionen för geologiska vetenskaper,KTH Royal Institute of Technology, Sweden,Linné Flow Center, FLOW,Stockholm Univ, Bolin Ctr Climate Res, Svante Arrhenius Vag 8, SE-10691 Stockholm, Sweden.;Stockholm Univ, Dept Geol Sci, Svante Arrhenius Vag 8, SE-10691 Stockholm, Sweden4 aut0 (Swepub:kth)u1pzw7j7
2451 0a Warm summers during the Younger Dryas cold reversal
264 c 2018-04-24
264 1b Springer Science and Business Media LLC,c 2018
338 a print2 rdacarrier
500 a QC 20180517
520 a The Younger Dryas (YD) cold reversal interrupts the warming climate of the deglaciation with global climatic impacts. The sudden cooling is typically linked to an abrupt slowdown of the Atlantic Meridional Overturning Circulation (AMOC) in response to meltwater discharges from ice sheets. However, inconsistencies regarding the YD-response of European summer temperatures have cast doubt whether the concept provides a sufficient explanation. Here we present results from a high-resolution global climate simulation together with a new July temperature compilation based on plant indicator species and show that European summers remain warm during the YD. Our climate simulation provides robust physical evidence that atmospheric blocking of cold westerly winds over Fennoscandia is a key mechanism counteracting the cooling impact of an AMOC-slowdown during summer. Despite the persistence of short warm summers, the YD is dominated by a shift to a continental climate with extreme winter to spring cooling and short growing seasons.
650 7a NATURVETENSKAPx Geovetenskap och miljövetenskap0 (SwePub)1052 hsv//swe
650 7a NATURAL SCIENCESx Earth and Related Environmental Sciences0 (SwePub)1052 hsv//eng
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
653 a Palaeoceanography
653 a Palaeoclimate
7001 a Väliranta, Minnau Univ Helsinki, Ecosyst & Environm Res Programme, Fac Biol & Environm Sci, ECRU, POB 65, FIN-00014 Helsinki, Finland.;Univ Helsinki, Helsinki Inst Sustainabil Sci HELSUS, POB 65, FIN-00014 Helsinki, Finland.,University of Helsinki4 aut
7001 a Muschitiello, Francescou Stockholm University,Stockholms universitet,Institutionen för geologiska vetenskaper,University of Cambridge, UK; Columbia University, USA,Stockholm Univ, Bolin Ctr Climate Res, Svante Arrhenius Vag 8, SE-10691 Stockholm, Sweden.;Stockholm Univ, Dept Geol Sci, Svante Arrhenius Vag 8, SE-10691 Stockholm, Sweden.;Univ Cambridge, Dept Geog, Cambridge CB2 3EN, England.;Columbia Univ, Lamont Doherty Earth Observ, 61 Route 9 W, New York, NY 10964 USA.,Lamont-Doherty Earth Observatory4 aut
7001 a Tarasov, Levu Mem Univ Newfoundland, Dept Phys & Phys Oceanog, St John, NF A1B 3X7, Canada.,Memorial University of Newfoundland4 aut
7001 a Heikkilä, Maijau Univ Helsinki, Ecosyst & Environm Res Programme, Fac Biol & Environm Sci, ECRU, POB 65, FIN-00014 Helsinki, Finland.;Univ Helsinki, Helsinki Inst Sustainabil Sci HELSUS, POB 65, FIN-00014 Helsinki, Finland.,University of Helsinki4 aut
7001 a Björck, Svanteu Stockholm University,Lunds universitet,Stockholms universitet,Institutionen för geologiska vetenskaper,Lund University, Sweden,Stockholm Univ, Bolin Ctr Climate Res, Svante Arrhenius Vag 8, SE-10691 Stockholm, Sweden.;Stockholm Univ, Dept Geol Sci, Svante Arrhenius Vag 8, SE-10691 Stockholm, Sweden.;Lund Univ, Dept Geol, Quaternary Sci, Box 117, SE-22100 Lund, Sweden.,Kvartärgeologi,Geologiska institutionen,Naturvetenskapliga fakulteten,Quaternary Sciences,Department of Geology,Faculty of Science4 aut0 (Swepub:lu)geol-sbj
7001 a Brandefelt, Jennyu Swedish Nucl Fuel & Waste Management Co SKB, Box 250, SE-10124 Stockholm, Sweden.,The Swedish Nuclear Fuel and Waste Management Company4 aut
7001 a Johansson, Arne V.,d 1953-u KTH Royal Institute of Technology,KTH,Linné Flow Center, FLOW,Mekanik4 aut0 (Swepub:kth)u1r4nbk6
7001 a Näslund, Jens-Oveu Stockholm University,Stockholms universitet,Institutionen för naturgeografi och kvartärgeologi (INK),Swedish Nuclear Fuel and Waste Management Company (SKB), Sweden,Swedish Nucl Fuel & Waste Management Co SKB, Box 250, SE-10124 Stockholm, Sweden.;Stockholm Univ, Dept Phys Geog & Quaternary Geol, Svante Arrhenius Vag 8, SE-10691 Stockholm, Sweden.,The Swedish Nuclear Fuel and Waste Management Company4 aut
7001 a Wohlfarth, Barbarau Stockholm University,Stockholms universitet,Institutionen för geologiska vetenskaper,Stockholm Univ, Bolin Ctr Climate Res, Svante Arrhenius Vag 8, SE-10691 Stockholm, Sweden.;Stockholm Univ, Dept Geol Sci, Svante Arrhenius Vag 8, SE-10691 Stockholm, Sweden.4 aut0 (Swepub:lu)geol-bwo
7102 a Stockholms universitetb Institutionen för geologiska vetenskaper4 org
7730 t Nature Communicationsd : Springer Science and Business Media LLCg 9q 9x 2041-1723
8564 u https://doi.org/10.1038/s41467-018-04071-5y Fulltext
8564 u https://www.nature.com/articles/s41467-018-04071-5.pdf
8564 u http://dx.doi.org/10.1038/s41467-018-04071-5x freey FULLTEXT
8564 8u https://urn.kb.se/resolve?urn=urn:nbn:se:su:diva-156668
8564 8u https://doi.org/10.1038/s41467-018-04071-5
8564 8u https://urn.kb.se/resolve?urn=urn:nbn:se:kth:diva-227217
8564 8u https://lup.lub.lu.se/record/fef1917d-6990-4f64-a638-34d8717ae1c6

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