Show simple item record

dc.contributor.authorYan, Hong  Concept link
dc.contributor.authorSun, Liguang  Concept link
dc.contributor.authorOppo, Delia W.  Concept link
dc.contributor.authorWang, Yuhong  Concept link
dc.contributor.authorLiu, Zhonghui  Concept link
dc.contributor.authorXie, Zhouqing  Concept link
dc.contributor.authorLiu, Xiaodong  Concept link
dc.contributor.authorCheng, Wenhan  Concept link
dc.date.accessioned2011-05-17T14:06:33Z
dc.date.available2011-05-17T14:06:33Z
dc.date.issued2011-04-26
dc.identifier.citationNature Communications 2 (2011): 293en_US
dc.identifier.urihttps://hdl.handle.net/1912/4610
dc.description© Macmillan Publishers Limited, 2011. This article is distributed under the terms of the Creative Commons Attribution License. The definitive version was published in Nature Communications 2 (2011): 293, doi:10.1038/ncomms1297.en_US
dc.description.abstractThe relative importance of north–south migrations of the intertropical convergence zone (ITCZ) versus El Niño-Southern Oscillation and its associated Pacific Walker Circulation (PWC) variability for past hydrological change in the western tropical Pacific is unclear. Here we show that north–south ITCZ migration was not the only mechanism of tropical Pacific hydrologic variability during the last millennium, and that PWC variability profoundly influenced tropical Pacific hydrology. We present hydrological reconstructions from Cattle Pond, Dongdao Island of the South China Sea, where multi-decadal rainfall and downcore grain size variations are correlated to the Southern Oscillation Index during the instrumental era. Our downcore grain size reconstructions indicate that this site received less precipitation during relatively warm periods, AD 1000–1400 and AD 1850–2000, compared with the cool period (AD 1400–1850). Including our new reconstructions in a synthesis of tropical Pacific records results in a spatial pattern of hydrologic variability that implicates the PWC.en_US
dc.description.sponsorshipThis work was supported by the Natural Science Foundation of China (NSFC) (40730107) and the Major State Basic Research Development Program of China (973 Program) (No.2010CB428902). DWO acknowledges support from the US NSF.en_US
dc.format.mimetypeapplication/pdf
dc.language.isoen_USen_US
dc.publisherNature Publishing Groupen_US
dc.relation.urihttps://doi.org/10.1038/ncomms1297
dc.rightsAttribution-NonCommercial-ShareAlike 3.0 Unported*
dc.rights.urihttp://creativecommons.org/licenses/by-nc-sa/3.0/*
dc.titleSouth China Sea hydrological changes and Pacific Walker Circulation variations over the last millenniumen_US
dc.typeArticleen_US
dc.identifier.doi10.1038/ncomms1297


Files in this item

Thumbnail
Thumbnail
Thumbnail

This item appears in the following Collection(s)

Show simple item record

Attribution-NonCommercial-ShareAlike 3.0 Unported
Except where otherwise noted, this item's license is described as Attribution-NonCommercial-ShareAlike 3.0 Unported