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The paleoclimate context and future trajectory of extreme summer hydroclimate in eastern Australia


Cook, BI and Palmer, JG and Cook, ER and Turney, CSM and Allen, K and Fenwick, P and O'Donnell, A and Lough, JM and Grierson, PF and Ho, M and Baker, PJ, The paleoclimate context and future trajectory of extreme summer hydroclimate in eastern Australia, Journal of Geophysical Research, 121, (21) pp. 12,820-12,838. ISSN 0148-0227 (2016) [Refereed Article]


Copyright Statement

Copyright 2016 This article is a US Government work and is in the public domain in the USA

DOI: doi:10.1002/2016JD024892


Eastern Australia recently experienced an intense drought (Millennium Drought, 2003-2009) and record-breaking rainfall and flooding (austral summer 2010-2011). There is some limited evidence for a climate change contribution to these events, but such analyses are hampered by the paucity of information on long-term natural variability. Analyzing a new reconstruction of summer (December-January-February) Palmer Drought Severity Index (the Australia-New Zealand Drought Atlas; ANZDA, 1500-2012 Common Era), we find moisture deficits during the Millennium Drought fall within the range of the last 500 years of natural hydroclimate variability. This variability includes periods of multidecadal drought in the 1500s more persistent than any event in the historical record. However, the severity of the Millennium Drought, which was caused by autumn (March-April-May) precipitation declines, may be underestimated in the ANZDA because the reconstruction is biased toward summer and antecedent spring (September-October-November) precipitation. The pluvial in 2011, however, which was characterized by extreme summer rainfall faithfully captured by the ANZDA, is likely the wettest year in the reconstruction for Coastal Queensland. Climate projections (Representative Concentration Pathways (RCP) 8.5 scenario) suggest that eastern Australia will experience long-term drying during the 21st century. While the contribution of anthropogenic forcing to recent extremes remains an open question, these projections indicate an amplified risk of multiyear drought anomalies matching or exceeding the intensity of the Millennium Drought.

Item Details

Item Type:Refereed Article
Research Division:Earth Sciences
Research Group:Physical geography and environmental geoscience
Research Field:Palaeoclimatology
Objective Division:Environmental Policy, Climate Change and Natural Hazards
Objective Group:Natural hazards
Objective Field:Climatological hazards (e.g. extreme temperatures, drought and wildfires)
UTAS Author:Allen, K (Dr Kathy Allen)
ID Code:142994
Year Published:2016
Web of Science® Times Cited:21
Deposited By:Geography and Spatial Science
Deposited On:2021-02-19
Last Modified:2021-11-16
Downloads:11 View Download Statistics

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