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dc.contributor.authorGebregiorgis, Daniel  Concept link
dc.contributor.authorHathorne, Ed C.  Concept link
dc.contributor.authorGiosan, Liviu  Concept link
dc.contributor.authorClemens, Steven C.  Concept link
dc.contributor.authorNürnberg, Dirk  Concept link
dc.contributor.authorFrank, Martin  Concept link
dc.date.accessioned2018-11-13T18:48:07Z
dc.date.available2018-11-13T18:48:07Z
dc.date.issued2018-11-08
dc.identifier.citationNature Communications 9 (2018): 4702en_US
dc.identifier.urihttps://hdl.handle.net/1912/10706
dc.description© The Author(s), 2018. This article is distributed under the terms of the Creative Commons Attribution License. The definitive version was published in Nature Communications 9 (2018): 4702, doi:10.1038/s41467-018-07076-2.en_US
dc.description.abstractThe orbital-scale timing of South Asian monsoon (SAM) precipitation is poorly understood. Here we present new SST and seawater δ18O (δ18Osw) records from the Bay of Bengal, the core convective region of the South Asian monsoon, over the past 1 million years. Our records reveal that SAM precipitation peaked in the precession band ~9 kyrs after Northern Hemisphere summer insolation maxima, in phase with records of SAM winds in the Arabian Sea and eastern Indian Ocean. Precession-band variance, however, accounts for ~30% of the total variance of SAM precipitation while it was either absent or dominant in records of the East Asian monsoon (EAM). This and the observation that SAM precipitation was phase locked with obliquity minima and was sensitive to Southern Hemisphere warming provides clear evidence that SAM and EAM precipitation responded differently to orbital forcing and highlights the importance of internal processes forcing monsoon variability.en_US
dc.description.sponsorshipThis study was partly funded by the German Science Foundation, DFG, IODP Priority Program (grant HA 5751/3-1).en_US
dc.language.isoen_USen_US
dc.publisherNature Publishing Groupen_US
dc.relation.urihttps://doi.org/10.1038/s41467-018-07076-2
dc.rightsAttribution 4.0 International*
dc.rights.urihttp://creativecommons.org/licenses/by/4.0/*
dc.titleSouthern Hemisphere forcing of South Asian monsoon precipitation over the past ~1 million yearsen_US
dc.typeArticleen_US
dc.identifier.doi10.1038/s41467-018-07076-2


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Attribution 4.0 International
Except where otherwise noted, this item's license is described as Attribution 4.0 International