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dc.contributor.authorHe, Shengping
dc.contributor.authorWang, Huijun
dc.contributor.authorLi, Fei
dc.contributor.authorLi, Hui
dc.contributor.authorWang, Chi
dc.date.accessioned2021-02-19T09:45:37Z
dc.date.available2021-02-19T09:45:37Z
dc.date.created2020-04-02T10:31:02Z
dc.date.issued2020
dc.PublishedNational Science Review. 2020, 7 141-148.
dc.identifier.issn2095-5138
dc.identifier.urihttps://hdl.handle.net/11250/2729125
dc.description.abstractSolar irradiance has been universally acknowledged to be dominant by quasi-decadal variability, which has been adopted frequently to investigate its effect on climate decadal variability. As one major terrestrial energy source, solar-wind energy flux into Earth's magnetosphere (Ein) exhibits dramatic interannual variation, the effect of which on Earth's climate, however, has not drawn much attention. Based on the Ein estimated by 3D magnetohydrodynamic simulations, we demonstrate a novelty that the annual mean Ein can explain up to 25% total interannual variance of the northern-hemispheric temperature in the subsequent boreal winter. The concurrent anomalous atmospheric circulation resembles the positive phase of Arctic Oscillation/North Atlantic Oscillation. The warm anomalies in the tropic stratopause and tropopause induced by increased solar-wind–magnetosphere energy persist into the subsequent winter. Due to the dominant change in the polar vortex and mid-latitude westerly in boreal winter, a ‘top-down’ propagation of the stationary planetary wave emerges in the Northern Hemisphere and further influences the atmospheric circulation and climate.en_US
dc.language.isoengen_US
dc.publisherOxford University Pressen_US
dc.rightsNavngivelse 4.0 Internasjonal*
dc.rights.urihttp://creativecommons.org/licenses/by/4.0/deed.no*
dc.titleSolar-wind–magnetosphere energy influences the interannual variability of the northern-hemispheric winter climateen_US
dc.typeJournal articleen_US
dc.typePeer revieweden_US
dc.description.versionpublishedVersionen_US
dc.rights.holderCopyright The Author(s) 2019.en_US
cristin.ispublishedtrue
cristin.fulltextoriginal
cristin.qualitycode1
dc.identifier.doi10.1093/nsr/nwz082
dc.identifier.cristin1804912
dc.source.journalNational Science Reviewen_US
dc.source.407
dc.source.pagenumber141-148en_US
dc.identifier.citationNational Science Review. 2020, 7 (1), 141–148.en_US
dc.source.volume7en_US
dc.source.issue1en_US


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Navngivelse 4.0 Internasjonal
Except where otherwise noted, this item's license is described as Navngivelse 4.0 Internasjonal