Please use this identifier to cite or link to this item: http://doi.org/10.25358/openscience-5758
Full metadata record
DC FieldValueLanguage
dc.contributor.authorDeiniger, Michael-
dc.contributor.authorMcDermott, Frank-
dc.contributor.authorCruz, Francisco W.-
dc.contributor.authorBernal, Juan Pablo-
dc.contributor.authorMudelsee, Manfred-
dc.contributor.authorVonhof, Hubert-
dc.contributor.authorMillo, Christian-
dc.contributor.authorSpötl, Christoph-
dc.contributor.authorTreble, Pauline C.-
dc.contributor.authorPickering, Robyn-
dc.contributor.authorScholz, Denis-
dc.date.accessioned2021-04-22T10:43:02Z-
dc.date.available2021-04-22T10:43:02Z-
dc.date.issued2020-
dc.identifier.urihttps://openscience.ub.uni-mainz.de/handle/20.500.12030/5767-
dc.description.abstractAtmospheric circulation is a fundamental component of Earth’s climate system, transporting energy poleward to partially offset the latitudinal imbalance in insolation. Changes in the latitudinal distribution of insolation thus force variations in atmospheric circulation, in turn altering regional hydroclimates. Here we demonstrate that regional hydroclimates controlled by the Northern Hemisphere mid-latitude storm tracks and the African and South American Monsoons changed synchronously during the last 10 kyrs. We argue that these regional hydroclimate variations are connected and reflect the adjustment of the atmospheric poleward energy transport to the evolving differential heating of the Northern and Southern Hemispheres. These results indicate that changes in latitudinal insolation gradients and associated variations in latitudinal temperature gradients exert important control on atmospheric circulation and regional hydroclimates. Since the current episode of global warming strongly affects latitudinal temperature gradients through Arctic amplification, our results can inform projections of likely inter-hemispheric precipitation changes in the future.en_GB
dc.language.isoengde
dc.rightsCC BY*
dc.rights.urihttps://creativecommons.org/licenses/by/4.0/*
dc.subject.ddc550 Geowissenschaftende_DE
dc.subject.ddc550 Earth sciencesen_GB
dc.titleInter-hemispheric synchroneity of Holocene precipitation anomalies controlled by Earth’s latitudinal insolation gradientsen_GB
dc.typeZeitschriftenaufsatzde
dc.identifier.doihttp://doi.org/10.25358/openscience-5758-
jgu.type.dinitypearticleen_GB
jgu.type.versionPublished versionde
jgu.type.resourceTextde
jgu.organisation.departmentFB 09 Chemie, Pharmazie u. Geowissensch.de
jgu.organisation.number7950-
jgu.organisation.nameJohannes Gutenberg-Universität Mainz-
jgu.rights.accessrightsopenAccess-
jgu.journal.titleNature communicationsde
jgu.journal.volume11de
jgu.pages.alternative5447de
jgu.publisher.year2020-
jgu.publisher.nameNature Publishing Group UKde
jgu.publisher.placeLondonde
jgu.publisher.urihttps://doi.org/10.1038/s41467-020-19021-3de
jgu.publisher.issn2041-1723de
jgu.organisation.placeMainz-
jgu.subject.ddccode550de
jgu.publisher.doi10.1038/s41467-020-19021-3
jgu.organisation.rorhttps://ror.org/023b0x485
Appears in collections:JGU-Publikationen

Files in This Item:
  File Description SizeFormat
Thumbnail
deiniger_michael-inter-hemisphe-20210419124942680.pdf2.1 MBAdobe PDFView/Open