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LIBRIS Formathandbok  (Information om MARC21)
FältnamnIndikatorerMetadata
00003890naa a2200553 4500
001oai:gup.ub.gu.se/282237
003SwePub
008240528s2019 | |||||||||||000 ||eng|
024a https://gup.ub.gu.se/publication/2822372 URI
024a https://doi.org/10.1016/j.quascirev.2019.05.0142 DOI
040 a (SwePub)gu
041 a eng
042 9 SwePub
072 7a ref2 swepub-contenttype
072 7a art2 swepub-publicationtype
100a Fang, Keyanu Gothenburg University,Göteborgs universitet,Institutionen för geovetenskaper,Department of Earth Sciences4 aut0 (Swepub:gu)xfakey
2451 0a Oceanic and atmospheric modes in the Pacific and Atlantic Oceans since the Little Ice Age (LIA): Towards a synthesis
264 1b Elsevier BV,c 2019
520 a Understanding the variability of the oceanic and atmospheric modes from the Little Ice Age (LIA,similar to 1250 - 1850) to the present can help evaluate their behaviors under future warming scenarios. Numerous proxy-based reconstructions of the oceanic and atmospheric modes were presented. It is highly needed for a synthesis study to evaluate the existing reconstructions of the dominant oceanic and atmospheric modes since the LIA. We found that the El Nino-Southern Oscillation (ENSO) reconstructions are only robust on interannual and interdecadal scales, while the reconstructed Pacific Decadal Oscillation (PDO) and Atlantic Multi-decadal Oscillation (AMO) are robust on multi-decadal (50-100 years) timescales. We generated synthesized ENSO, PDO and AMO reconstructions as the average of the existing reconstructions on the most suitable timescales identified using timescale dependent correlation methods. In the 20th century, the interannual variability and periodicity of the ENSO and the multi-decadal periodicity of the PDO and AMO were most pronounced. The ENSO shows the strongest multi-decadal periodicity from mid-18th century onwards, while the multi-decadal periodicity of the PDO and AMO was particularly low in the 18th century. Multi-decadal variations of the AMO showed a prompt and positive response to solar irradiation, while the ENSO showed a lagged and negative response to solar irradiation from the 18th century to the present. (C) 2019 Elsevier Ltd. All rights reserved.
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 Oceanic and atmospheric mode
653 a Climate reconstruction
653 a ENSO
653 a PDO
653 a AMO
653 a multidecadal oscillation
653 a climate variability
653 a decadal oscillation
653 a reconstruction
653 a temperature
653 a enso
653 a modulation
653 a millennium
653 a ad
653 a Physical Geography
653 a Geology
700a Chen, Deliang,d 1961u Gothenburg University,Göteborgs universitet,Institutionen för geovetenskaper,Department of Earth Sciences4 aut0 (Swepub:gu)xchede
700a Ilvonen, L.4 aut
700a Pasanen, L.4 aut
700a Holmstrom, L.4 aut
700a Seppa, H.4 aut
700a Huang, G.4 aut
700a Ou, Tinghaiu Gothenburg University,Göteborgs universitet,Institutionen för geovetenskaper,Department of Earth Sciences4 aut0 (Swepub:gu)xoutic
700a Linderholm, Hans W.,d 1968u Gothenburg University,Göteborgs universitet,Institutionen för geovetenskaper,Department of Earth Sciences4 aut0 (Swepub:gu)xlinha
710a Göteborgs universitetb Institutionen för geovetenskaper4 org
773t Quaternary Science Reviewsd : Elsevier BVg 215, s. 293-307q 215<293-307x 0277-3791
8564 8u https://gup.ub.gu.se/publication/282237
8564 8u https://doi.org/10.1016/j.quascirev.2019.05.014

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