{"refrec":{"BRefID":231284,"RR":"<b>Mohtadi, M.; Oppo, D.W.; Steinke, S.; Stuut, J.B.W.; De Pol-Holz, R.; Hebbeln, D.; Lückge, A.; Stuut, J.B.W.; De-Pol-Holz, R.</b> (2011). Glacial to Holocene swings of the Australian-Indonesian monsoon. <i>Nature Geoscience 4(8)</i>: 540-544. <a href=\"http://dx.doi.org/10.1038/NGEO1209\" target=\"_blank\">dx.doi.org/10.1038/NGEO1209</a>","BEntID":222996,"PublicFlag":1,"CheckedFlag":1,"wosflag":1,"vabbflag":1,"RefStringPartII":". <i>Nature Geoscience 4(8)</i>: 540-544. <a href=\"https://dx.doi.org/10.1038/NGEO1209\" target=\"_blank\">https://dx.doi.org/10.1038/NGEO1209</a>","DocTypID":8,"DocType":"Journal article","MarineFlag":0,"FreshFlag":0,"BrackishFlag":0,"TerrestrialFlag":0,"Authorstring":"Mohtadi, M.; Oppo, D.W.; Steinke, S.; Stuut, J.B.W.; De Pol-Holz, R.; Hebbeln, D.; Lückge, A.; Stuut, J.B.W.; De-Pol-Holz, R.","OrigTitleTranslFlag":0,"Authorstringtrunc":"Mohtadi, M. <i>et al.</i>","Englishabstract":"The Australian-Indonesian monsoon is an important component of the climate system in the tropical Indo-Pacific region(1). However, its past variability, relation with northern and southern high-latitude climate and connection to the other Asian monsoon systems are poorly understood. Here we present high-resolution records of monsoon-controlled austral winter upwelling during the past 22,000 years, based on planktic foraminiferal oxygen isotopes and faunal composition in a sedimentary archive collected offshore southern Java. We show that glacial-interglacial variations in the Australian-Indonesian winter monsoon were in phase with the Indian summer monsoon system, consistent with their modern linkage through cross-equatorial surface winds. Likewise, millennial-scale variability of upwelling shares similar sign and timing with upwelling variability in the Arabian Sea. On the basis of element composition and grain-size distribution as precipitation-sensitive proxies in the same archive, we infer that (austral) summer monsoon rainfall was highest during the Bolling-Allerod period and the past 2,500 years. Our results indicate drier conditions during Heinrich Stadial 1 due to a southward shift of summer rainfall and a relatively weak Hadley cell south of the Equator. We suggest that the Australian-Indonesian summer and winter monsoon variability were closely linked to summer insolation and abrupt climate changes in the northern hemisphere.","AbstractOtherLang":null,"BibLvlCode":"AS","StandardTitle":"Glacial to Holocene swings of the Australian-Indonesian monsoon","OrigTitleLangCode":"en","OrigTitleLangCodeExtended":"eng","OrigTitleLangID":15,"DateLastModified":{"date":"2024-12-10 01:33:17.368041","timezone_type":1,"timezone":"+01:00"},"UserAccessRight":null,"UserAccID":null,"AuthorKeywords":null,"OtherDescriptors":null,"Notes":null,"AnaPub":2011,"MonPub":null,"DateUpdate":"2014-06-03","DateCreate":"2013-12-01","SecASFANote":null,"ConfID":null,"PeerRev":1,"VlizCoreFlag":1,"WoScode":"WOS:000293277100016","VABBcode":null,"OpenAcc":0,"DOI":"10.1038/NGEO1209"},"refs":null,"anarec":{"AnaID":231284,"PubliDate":2011,"Pagination":"540-544","XtraPublOfAnaID":null,"ISBN":null,"Volume":"4","Issue":"8","BRefMon":null,"BRefMonRR":null,"BRefXtra":null,"BRefXtraRR":null,"SerBRefID":123796,"SerRR":"Nature Geoscience. 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