Please use this identifier to cite or link to this item: https://apo.ansto.gov.au/dspace/handle/10238/11010
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dc.contributor.authorBarr, C-
dc.contributor.authorTibby, J-
dc.contributor.authorLeng, MJ-
dc.contributor.authorTyler, JJ-
dc.contributor.authorHenderson, ACG-
dc.contributor.authorOverpeck, JT-
dc.contributor.authorSimpson, GL-
dc.contributor.authorCole, JE-
dc.contributor.authorPhipps, SJ-
dc.contributor.authorMarshall, JC-
dc.contributor.authorMcGregor, GB-
dc.contributor.authorHua, Q-
dc.contributor.authorMcRobie, FH-
dc.date.accessioned2021-06-30T23:07:05Z-
dc.date.available2021-06-30T23:07:05Z-
dc.date.issued2019-02-07-
dc.identifier.citationBarr, C., Tibby, J., Leng, M. J., Tyler, J. J., Henderson, A. C. G., Overpeck, J. T., Simpson, G. L., Cole, J. E., Phipps, S. J., Marshall, J. C., McGregor, G. B., Hua, Q. & McRobie, F. H. (2019). Holocene El Niño–Southern Oscillation variability reflected in subtropical Australian precipitation. Scientific Reports, 9(1), 1-9. doi:10.1038/s41598-019-38626-3en_US
dc.identifier.issn2045-2322-
dc.identifier.urihttps://doi.org/10.1038/s41598-019-38626-3en_US
dc.identifier.urihttps://apo.ansto.gov.au/dspace/handle/10238/11010-
dc.descriptionOpen Access: This article is licensed under a Creative Commons Attribution 4.0 International License. This article was updated by the Authors in 2021.en_US
dc.description.abstractThe La Niña and El Niño phases of the El Niño-Southern Oscillation (ENSO) have major impacts on regional rainfall patterns around the globe, with substantial environmental, societal and economic implications. Long-term perspectives on ENSO behaviour, under changing background conditions, are essential to anticipating how ENSO phases may respond under future climate scenarios. Here, we derive a 7700-year, quantitative precipitation record using carbon isotope ratios from a single species of leaf preserved in lake sediments from subtropical eastern Australia. We find a generally wet (more La Niña-like) mid-Holocene that shifted towards drier and more variable climates after 3200 cal. yr BP, primarily driven by increasing frequency and strength of the El Niño phase. Climate model simulations implicate a progressive orbitally-driven weakening of the Pacific Walker Circulation as contributing to this change. At centennial scales, high rainfall characterised the Little Ice Age (~1450–1850 CE) in subtropical eastern Australia, contrasting with oceanic proxies that suggest El Niño-like conditions prevail during this period. Our data provide a new western Pacific perspective on Holocene ENSO variability and highlight the need to address ENSO reconstruction with a geographically diverse network of sites to characterise how both ENSO, and its impacts, vary in a changing climate. © The Author(s) 2019, corrected publication 2021en_US
dc.language.isoenen_US
dc.publisherSpringer Natureen_US
dc.subjectQuaternary perioden_US
dc.subjectSouthern Oscillationen_US
dc.subjectRainen_US
dc.subjectLimnologyen_US
dc.subjectPaleoclimatologyen_US
dc.subjectAustraliaen_US
dc.titleHolocene El Niño–Southern Oscillation variability reflected in subtropical Australian precipitationen_US
dc.typeJournal Articleen_US
dc.date.statistics2021-06-30-
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