{"refrec":{"BRefID":334029,"RR":"<b>He, C.; Liu, Z.; Otto-Bliesner, B.L.; Brady, E.C.; Zhu, C.; Tomas, R.; Clark, P.U.; Zhu, J.; Jahn, A.; Gu, S.; Zhang, J.; Nusbaumer, J.; Noone, D.; Cheng, H.; Wang, Y.; Yan, M.; Bao, Y.</b> (2021). Hydroclimate footprint of pan-Asian monsoon water isotope during the last deglaciation. <i>Science Advances 7(4)</i>: eabe2611. <a href=\"https://dx.doi.org/10.1126/sciadv.abe2611\" target=\"_blank\">https://dx.doi.org/10.1126/sciadv.abe2611</a>","BEntID":330584,"PublicFlag":1,"CheckedFlag":0,"wosflag":1,"vabbflag":0,"RefStringPartII":". <i>Science Advances 7(4)</i>: eabe2611. <a href=\"https://dx.doi.org/10.1126/sciadv.abe2611\" target=\"_blank\">https://dx.doi.org/10.1126/sciadv.abe2611</a>","DocTypID":8,"DocType":"Journal article","MarineFlag":0,"FreshFlag":0,"BrackishFlag":0,"TerrestrialFlag":0,"Authorstring":"He, C.; Liu, Z.; Otto-Bliesner, B.L.; Brady, E.C.; Zhu, C.; Tomas, R.; Clark, P.U.; Zhu, J.; Jahn, A.; Gu, S.; Zhang, J.; Nusbaumer, J.; Noone, D.; Cheng, H.; Wang, Y.; Yan, M.; Bao, Y.","OrigTitleTranslFlag":0,"Authorstringtrunc":"He, C. <i>et al.</i>","Englishabstract":"Oxygen isotope speleothem records exhibit coherent variability over the pan-Asian summer monsoon (AM) region. The hydroclimatic representation of these oxygen isotope records for the AM, however, has remained poorly understood. Here, combining an isotope-enabled Earth system model in transient experiments with proxy records, we show that the widespread AM δ<sup>18</sup>O<sub>c</sub> signal during the last deglaciation (20 to 11 thousand years ago) is accompanied by a continental-scale, coherent hydroclimate footprint, with spatially opposite signs in rainfall. This footprint is generated as a dynamically coherent response of the AM system primarily to meltwater forcing and secondarily to insolation forcing and is further reinforced by atmospheric teleconnection. Hence, widespread δ<sup>18</sup>O<sub>p</sub> depletion in the AM region is accompanied by a northward migration of the westerly jet and enhanced southwesterly monsoon wind, as well as increased rainfall from South Asia (India) to northern China but decreased rainfall in southeast China.","AbstractOtherLang":null,"BibLvlCode":"AS","StandardTitle":"Hydroclimate footprint of pan-Asian monsoon water isotope during the last deglaciation","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":2021,"MonPub":null,"DateUpdate":"2021-02-18","DateCreate":"2021-02-18","SecASFANote":null,"ConfID":null,"PeerRev":1,"VlizCoreFlag":1,"WoScode":"WOS:000610099000034","VABBcode":null,"OpenAcc":1,"DOI":"10.1126/sciadv.abe2611"},"refs":null,"anarec":{"AnaID":334029,"PubliDate":2021,"Pagination":"eabe2611","XtraPublOfAnaID":null,"ISBN":null,"Volume":"7","Issue":"4","BRefMon":null,"BRefMonRR":null,"BRefXtra":null,"BRefXtraRR":null,"SerBRefID":248966,"SerRR":"Science Advances. 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