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dc.contributor.authorDenniston, Rhawn F.  Concept link
dc.contributor.authorVillarini, Gabriele  Concept link
dc.contributor.authorGonzales, Angelique N.  Concept link
dc.contributor.authorWyrwoll, Karl-Heinz  Concept link
dc.contributor.authorPolyak, Victor J.  Concept link
dc.contributor.authorUmmenhofer, Caroline C.  Concept link
dc.contributor.authorLachniet, Matthew S.  Concept link
dc.contributor.authorWanamaker, Alan D.  Concept link
dc.contributor.authorHumphreys, William F.  Concept link
dc.contributor.authorWoods, David  Concept link
dc.contributor.authorCugley, John  Concept link
dc.date.accessioned2015-04-15T18:48:46Z
dc.date.available2015-09-30T08:42:20Z
dc.date.issued2015-03
dc.identifier.urihttps://hdl.handle.net/1912/7224
dc.descriptionAuthor Posting. © The Author(s), 2015]. This is the author's version of the work. It is posted here by permission of National Academy of Sciences for personal use, not for redistribution. The definitive version was published in Proceedings of the National Academy of Sciences of the United States of America 112 (2015): 4576–4581, doi: 10.1073/pnas.1422270112.en_US
dc.description.abstractAssessing temporal variability in extreme rainfall events prior to the historical era is complicated by the sparsity of long-term ‘direct’ storm proxies. Here we present a 2200-yr-long, accurate and precisely dated record of cave flooding events from the northwest Australian tropics that we interpret, based on an integrated analysis of meteorological data and sediment layers within stalagmites, as representing a proxy for extreme rainfall events derived primarily from tropical cyclones (TCs) and secondarily from the regional summer monsoon. This time series reveals substantial multi-centennial variability in extreme rainfall, with elevated occurrence rates characterizing the twentieth century, the period 850-1450 CE, and 50-400 CE; reduced activity marks 1450-1650 CE and 500-850 CE. These trends are similar to reconstructed numbers of TCs in the North Atlantic and Caribbean basins, and form temporal and spatial patterns best explained by secular changes in the dominant mode of the El Niño-Southern Oscillation (ENSO), the primary driver of modern TC variability. We thus attribute long-term shifts in cyclogenesis in both the central Australian and North Atlantic sectors over the past two millennia to entrenched El Niño or La Niña states of the tropical Pacific. The influence of ENSO on monsoon precipitation in this region of northwest Australia is muted, but ENSO-driven changes to the monsoon may have complemented changes to TC activity.en_US
dc.description.sponsorshipFunding was provided by the Paleo Perspectives on Climate Change (P2C2) program of the United States National Science Foundation (NSF) through grant AGS-1103413, a seed grant from the Center for Global and Regional Environmental Research, and Cornell College (all to R.D.), the Kimberley Foundation Australia (to K-H.W.), and Penzance and John P. Chase Memorial Endowed Funds at WHOI (to C.U.).en_US
dc.format.mimetypeapplication/pdf
dc.language.isoen_USen_US
dc.relation.urihttps://doi.org/10.1073/pnas.1422270112
dc.subjectSpeleothemen_US
dc.subjectTropical cycloneen_US
dc.subjectMonsoonen_US
dc.subjectEl Niño/Southern Oscillationen_US
dc.subjectAustraliaen_US
dc.titleExtreme rainfall activity in the Australian tropics reflects changes in the El Niño/Southern Oscillation over the last two millenniaen_US
dc.typePreprinten_US
dc.description.embargo2015-09-30en_US


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