Western Pacific hydroclimate linked to global climate variability over the past two millennia.
Identifieur interne : 001392 ( PubMed/Checkpoint ); précédent : 001391; suivant : 001393Western Pacific hydroclimate linked to global climate variability over the past two millennia.
Auteurs : Michael L. Griffiths [États-Unis] ; Alena K. Kimbrough [Australie] ; Michael K. Gagan [Australie] ; Russell N. Drysdale [Australie] ; Julia E. Cole [États-Unis] ; Kathleen R. Johnson [États-Unis] ; Jian-Xin Zhao [Australie] ; Benjamin I. Cook [États-Unis] ; John C. Hellstrom [Australie] ; Wahyoe S. Hantoro [Indonésie]Source :
- Nature communications [ 2041-1723 ] ; 2016.
Abstract
Interdecadal modes of tropical Pacific ocean-atmosphere circulation have a strong influence on global temperature, yet the extent to which these phenomena influence global climate on multicentury timescales is still poorly known. Here we present a 2,000-year, multiproxy reconstruction of western Pacific hydroclimate from two speleothem records for southeastern Indonesia. The composite record shows pronounced shifts in monsoon rainfall that are antiphased with precipitation records for East Asia and the central-eastern equatorial Pacific. These meridional and zonal patterns are best explained by a poleward expansion of the Australasian Intertropical Convergence Zone and weakening of the Pacific Walker circulation (PWC) between ∼1000 and 1500 CE Conversely, an equatorward contraction of the Intertropical Convergence Zone and strengthened PWC occurred between ∼1500 and 1900 CE. Our findings, together with climate model simulations, highlight the likelihood that century-scale variations in tropical Pacific climate modes can significantly modulate radiatively forced shifts in global temperature.
DOI: 10.1038/ncomms11719
PubMed: 27271972
Affiliations:
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Hellstrom</name><affiliation wicri:level="4"><nlm:affiliation>School of Earth Sciences, The University of Melbourne, Parkville, Victoria 3010, Australia.</nlm:affiliation><country xml:lang="fr">Australie</country><wicri:regionArea>School of Earth Sciences, The University of Melbourne, Parkville, Victoria 3010</wicri:regionArea><orgName type="university">Université de Melbourne</orgName><placeName><settlement type="city">Melbourne</settlement><region type="état">Victoria (État)</region></placeName></affiliation></author><author><name sortKey="Hantoro, Wahyoe S" sort="Hantoro, Wahyoe S" uniqKey="Hantoro W" first="Wahyoe S" last="Hantoro">Wahyoe S. Hantoro</name><affiliation wicri:level="1"><nlm:affiliation>Research Center for Geotechnology, Indonesian Institute of Sciences, Bandung 40135, Indonesia.</nlm:affiliation><country xml:lang="fr">Indonésie</country><wicri:regionArea>Research Center for Geotechnology, Indonesian Institute of Sciences, Bandung 40135</wicri:regionArea><wicri:noRegion>Bandung 40135</wicri:noRegion></affiliation></author></analytic><series><title level="j">Nature communications</title><idno type="eISSN">2041-1723</idno><imprint><date when="2016" type="published">2016</date></imprint></series></biblStruct></sourceDesc></fileDesc><profileDesc><textClass></textClass></profileDesc></teiHeader><front><div type="abstract" xml:lang="en">Interdecadal modes of tropical Pacific ocean-atmosphere circulation have a strong influence on global temperature, yet the extent to which these phenomena influence global climate on multicentury timescales is still poorly known. Here we present a 2,000-year, multiproxy reconstruction of western Pacific hydroclimate from two speleothem records for southeastern Indonesia. The composite record shows pronounced shifts in monsoon rainfall that are antiphased with precipitation records for East Asia and the central-eastern equatorial Pacific. These meridional and zonal patterns are best explained by a poleward expansion of the Australasian Intertropical Convergence Zone and weakening of the Pacific Walker circulation (PWC) between ∼1000 and 1500 CE Conversely, an equatorward contraction of the Intertropical Convergence Zone and strengthened PWC occurred between ∼1500 and 1900 CE. Our findings, together with climate model simulations, highlight the likelihood that century-scale variations in tropical Pacific climate modes can significantly modulate radiatively forced shifts in global temperature.</div></front></TEI><pubmed><MedlineCitation Status="In-Data-Review" Owner="NLM"><PMID Version="1">27271972</PMID><DateCreated><Year>2016</Year><Month>06</Month><Day>09</Day></DateCreated><DateRevised><Year>2017</Year><Month>02</Month><Day>20</Day></DateRevised><Article PubModel="Electronic"><Journal><ISSN IssnType="Electronic">2041-1723</ISSN><JournalIssue CitedMedium="Internet"><Volume>7</Volume><PubDate><Year>2016</Year><Month>Jun</Month><Day>08</Day></PubDate></JournalIssue><Title>Nature communications</Title><ISOAbbreviation>Nat Commun</ISOAbbreviation></Journal><ArticleTitle>Western Pacific hydroclimate linked to global climate variability over the past two millennia.</ArticleTitle><Pagination><MedlinePgn>11719</MedlinePgn></Pagination><ELocationID EIdType="doi" ValidYN="Y">10.1038/ncomms11719</ELocationID><Abstract><AbstractText>Interdecadal modes of tropical Pacific ocean-atmosphere circulation have a strong influence on global temperature, yet the extent to which these phenomena influence global climate on multicentury timescales is still poorly known. Here we present a 2,000-year, multiproxy reconstruction of western Pacific hydroclimate from two speleothem records for southeastern Indonesia. The composite record shows pronounced shifts in monsoon rainfall that are antiphased with precipitation records for East Asia and the central-eastern equatorial Pacific. These meridional and zonal patterns are best explained by a poleward expansion of the Australasian Intertropical Convergence Zone and weakening of the Pacific Walker circulation (PWC) between ∼1000 and 1500 CE Conversely, an equatorward contraction of the Intertropical Convergence Zone and strengthened PWC occurred between ∼1500 and 1900 CE. Our findings, together with climate model simulations, highlight the likelihood that century-scale variations in tropical Pacific climate modes can significantly modulate radiatively forced shifts in global temperature.</AbstractText></Abstract><AuthorList CompleteYN="Y"><Author ValidYN="Y"><LastName>Griffiths</LastName><ForeName>Michael L</ForeName><Initials>ML</Initials><AffiliationInfo><Affiliation>Department of Environmental Science, William Paterson University, Wayne, New Jersey 07470, USA.</Affiliation></AffiliationInfo></Author><Author ValidYN="Y"><LastName>Kimbrough</LastName><ForeName>Alena K</ForeName><Initials>AK</Initials><AffiliationInfo><Affiliation>Research School of Earth Sciences, Australian National University, Canberra, Australian Capital Territory 0200, Australia.</Affiliation></AffiliationInfo></Author><Author ValidYN="Y"><LastName>Gagan</LastName><ForeName>Michael K</ForeName><Initials>MK</Initials><AffiliationInfo><Affiliation>Research School of Earth Sciences, Australian National University, Canberra, Australian Capital Territory 0200, Australia.</Affiliation></AffiliationInfo></Author><Author ValidYN="Y"><LastName>Drysdale</LastName><ForeName>Russell N</ForeName><Initials>RN</Initials><AffiliationInfo><Affiliation>School of Geography, University of Melbourne, Parkville, Victoria 3010, Australia.</Affiliation></AffiliationInfo><AffiliationInfo><Affiliation>EDYTEM, UMR CNRS 5204, Université de Savoie, 73376 Le Bourget du Lac, France.</Affiliation></AffiliationInfo></Author><Author ValidYN="Y"><LastName>Cole</LastName><ForeName>Julia E</ForeName><Initials>JE</Initials><AffiliationInfo><Affiliation>Department of Geosciences, University of Arizona, Tucson, Arizona 85721, USA.</Affiliation></AffiliationInfo><AffiliationInfo><Affiliation>Department of Atmospheric Sciences, University of Arizona, Tucson, Arizona 85721, USA.</Affiliation></AffiliationInfo></Author><Author ValidYN="Y"><LastName>Johnson</LastName><ForeName>Kathleen R</ForeName><Initials>KR</Initials><AffiliationInfo><Affiliation>Department of Earth System Science, University of California, Irvine, California 92697-3100, USA.</Affiliation></AffiliationInfo></Author><Author ValidYN="Y"><LastName>Zhao</LastName><ForeName>Jian-Xin</ForeName><Initials>JX</Initials><AffiliationInfo><Affiliation>School of Earth Sciences, University of Queensland, Brisbane, Queensland 4072, Australia.</Affiliation></AffiliationInfo></Author><Author ValidYN="Y"><LastName>Cook</LastName><ForeName>Benjamin I</ForeName><Initials>BI</Initials><AffiliationInfo><Affiliation>NASA Goddard Institute for Space Studies, New York, New York 10025, USA.</Affiliation></AffiliationInfo></Author><Author ValidYN="Y"><LastName>Hellstrom</LastName><ForeName>John C</ForeName><Initials>JC</Initials><Identifier Source="ORCID">http://orcid.org/0000-0001-9427-3525</Identifier><AffiliationInfo><Affiliation>School of Earth Sciences, The University of Melbourne, Parkville, Victoria 3010, Australia.</Affiliation></AffiliationInfo></Author><Author ValidYN="Y"><LastName>Hantoro</LastName><ForeName>Wahyoe S</ForeName><Initials>WS</Initials><AffiliationInfo><Affiliation>Research Center for Geotechnology, Indonesian Institute of Sciences, Bandung 40135, Indonesia.</Affiliation></AffiliationInfo></Author></AuthorList><Language>eng</Language><PublicationTypeList><PublicationType UI="D016428">Journal Article</PublicationType></PublicationTypeList><ArticleDate DateType="Electronic"><Year>2016</Year><Month>06</Month><Day>08</Day></ArticleDate></Article><MedlineJournalInfo><Country>England</Country><MedlineTA>Nat Commun</MedlineTA><NlmUniqueID>101528555</NlmUniqueID><ISSNLinking>2041-1723</ISSNLinking></MedlineJournalInfo><CitationSubset>IM</CitationSubset><CommentsCorrectionsList><CommentsCorrections RefType="Cites"><RefSource>Nat Commun. 2013;4:2908</RefSource><PMID Version="1">24309539</PMID></CommentsCorrections><CommentsCorrections RefType="Cites"><RefSource>Science. 2013 May 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Gagan</name><name sortKey="Hellstrom, John C" sort="Hellstrom, John C" uniqKey="Hellstrom J" first="John C" last="Hellstrom">John C. Hellstrom</name><name sortKey="Zhao, Jian Xin" sort="Zhao, Jian Xin" uniqKey="Zhao J" first="Jian-Xin" last="Zhao">Jian-Xin Zhao</name></country><country name="Indonésie"><noRegion><name sortKey="Hantoro, Wahyoe S" sort="Hantoro, Wahyoe S" uniqKey="Hantoro W" first="Wahyoe S" last="Hantoro">Wahyoe S. Hantoro</name></noRegion></country></tree></affiliations></record>Pour manipuler ce document sous Unix (Dilib)
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