Show simple item record

dc.contributor.authorDenniston, Rhawn  Concept link
dc.contributor.authorUmmenhofer, Caroline C.  Concept link
dc.contributor.authorWanamaker, Alan D.  Concept link
dc.contributor.authorLachniet, Matthew S.  Concept link
dc.contributor.authorVillarini, Gabriele  Concept link
dc.contributor.authorAsmerom, Yemane  Concept link
dc.contributor.authorPolyak, Victor J.  Concept link
dc.contributor.authorPassaro, Kristian J.  Concept link
dc.contributor.authorCugley, John  Concept link
dc.contributor.authorWoods, David  Concept link
dc.contributor.authorHumphreys, William F.  Concept link
dc.date.accessioned2016-10-11T18:52:16Z
dc.date.available2016-10-11T18:52:16Z
dc.date.issued2016-09-29
dc.identifier.citationScientific Reports 6 (2016): 34485en_US
dc.identifier.urihttps://hdl.handle.net/1912/8444
dc.description© The Author(s), 2016. This article is distributed under the terms of the Creative Commons Attribution License. The definitive version was published in Scientific Reports 6 (2016): 34485, doi:10.1038/srep34485.en_US
dc.description.abstractThe seasonal north-south migration of the intertropical convergence zone (ITCZ) defines the tropical rain belt (TRB), a region of enormous terrestrial and marine biodiversity and home to 40% of people on Earth. The TRB is dynamic and has been shown to shift south as a coherent system during periods of Northern Hemisphere cooling. However, recent studies of Indo-Pacific hydroclimate suggest that during the Little Ice Age (LIA; AD 1400–1850), the TRB in this region contracted rather than being displaced uniformly southward. This behaviour is not well understood, particularly during climatic fluctuations less pronounced than those of the LIA, the largest centennial-scale cool period of the last millennium. Here we show that the Indo-Pacific TRB expanded and contracted numerous times over multi-decadal to centennial scales during the last 3,000 yr. By integrating precisely-dated stalagmite records of tropical hydroclimate from southern China with a newly enhanced stalagmite time series from northern Australia, our study reveals a previously unidentified coherence between the austral and boreal summer monsoon. State-of-the-art climate model simulations of the last millennium suggest these are linked to changes in the structure of the regional manifestation of the atmosphere’s meridional circulation.en_US
dc.description.sponsorshipFunded by grants from the US National Science Foundation (NSF) Paleo Perspectives on Climate Change (P2C2) program (AGS-1103413), the Center for Global and Regional Environmental Research, and Cornell College (to R.F.D.); and the NSF P2C2 program (AGS-1203704 and AGS-1602455) and the Penzance and John P. Chase Memorial Endowed Funds at WHOI (to C.C.U.).en_US
dc.language.isoen_USen_US
dc.publisherNature Publishing Groupen_US
dc.relation.urihttps://doi.org/10.1038/srep34485
dc.rightsAttribution 4.0 International*
dc.rights.urihttp://creativecommons.org/licenses/by/4.0/*
dc.titleExpansion and contraction of the Indo-Pacific tropical rain belt over the last three millenniaen_US
dc.typeArticleen_US
dc.identifier.doi10.1038/srep34485


Files in this item

Thumbnail
Thumbnail
Thumbnail
Thumbnail

This item appears in the following Collection(s)

Show simple item record

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