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Australia’s Tinderbox Drought: An extreme natural event likely worsened by human-caused climate change

Devanand, Anjana1; Falster, Georgina2; Gillett, Zoe1; Hobeichi, Sanaa1; Holgate, Chiara2; Jin, Chenhui3; Mu, Mengyuan1; Parker, Tess3; Rifai, Sami1; Rome, Kathleen1; Stojanovic, Milica4; Vogel, Elisabeth1; Abram, Nerilie2; Abramowitz, Gab1; Coats, Sloan5; Evans, Jason1; Gallant, Allie3; Pitman, Andy1; Power, Scott6; Rauniyar, Surendra7; Taschetto, Andréa1; Ukkola, Anna1

Published Feb 15, 2024 on Dryad. https://doi.org/10.5061/dryad.12jm63z4q

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Feb 15, 2024 version files 28.54 GB

Abstract

We examine the characteristics and causes of southeast Australia’s Tinderbox Drought (2017–2019) that preceded the Black Summer fire disaster. The Tinderbox Drought was characterised by cool season rainfall deficits of around –50% in three consecutive years, which was exceptionally unlikely in the context of natural variability alone. The precipitation deficits were initiated and sustained by an anomalous atmospheric circulation that diverted oceanic moisture away from the region, despite traditional indicators of drought risk in southeast Australia generally being in neutral states. Moisture deficits were intensified by unusually high temperatures, high vapour pressure deficits and sustained reductions in terrestrial water availability. Anthropogenic forcing intensified the rainfall deficits of the Tinderbox Drought by around 18% with an interquartile range of 34.9% to –13.3% highlighting the considerable uncertainty in attributing droughts of this kind to human activity. Skillful predictability of this drought was possible by incorporating multiple remote and local predictors through machine learning, providing prospects for improving forecasting of multi-year droughts.