Abstract

The Black Summer fire season of 2019–2020 in southeastern Australia contributed to an intense ‘super outbreak’ of fire-induced and smoke-infused thunderstorms, known as pyrocumulonimbus (pyroCb). More than half of the 38 observed pyroCbs injected smoke particles directly into the stratosphere, producing two of the three largest smoke plumes observed at such altitudes to date. Over the course of 3 months, these plumes encircled a large swath of the Southern Hemisphere while continuing to rise, in a manner consistent with existing nuclear winter theory. We connect cause and effect of this event by quantifying the fire characteristics, fuel consumption, and meteorology contributing to the pyroCb spatiotemporal evolution. Emphasis is placed on the unusually long duration of sustained pyroCb activity and anomalous persistence during nighttime hours. The ensuing stratospheric smoke plumes are compared with plumes injected by significant volcanic eruptions over the last decade. As the second record-setting stratospheric pyroCb event in the last 4 years, the Australian super outbreak offers new clues on the potential scale and intensity of this increasingly extreme fire-weather phenomenon in a warming climate.

Highlights

  • An intense, multi-day outbreak of fire-induced and smoke-infused thunderstorms occurred during 29–31 December 2019 and 04 January 2020 in southeastern Australia

  • This study provides a quantitative analysis of the intense fire and pyroCb activity observed during the Australian New Year Super Outbreak (ANYSO) in southeastern Australia, revealing that 13 blow-up fires contributed to 38 distinct, ice-capped convective columns, defined as pyroCb pulses

  • Two distinct phases of ANYSO pyroCb activity resulted in two of the three largest smoke particle injections into the lower stratosphere observed through March 2021, rivaling or exceeding the stratospheric impact from all volcanic eruptions observed during 2012–2020

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Summary

Introduction

Multi-day outbreak of fire-induced and smoke-infused thunderstorms (known as pyrocumulonimbus or pyroCb) occurred during 29–31 December 2019 and 04 January 2020 in southeastern Australia. This Australian New Year Super Outbreak (ANYSO) of pyroCb activity resulted in roughly 1.0 Tg of cumulative smoke particle mass being injected into the lower stratosphere[1], consistent in magnitude with the initial ash and sulfate plume of a moderate volcanic eruption[2]. ANYSO occurred within three years of the Pacific Northwest Event (PNE) in western North America (12 August 2017), which served as the previous benchmark for an extreme, lower-stratospheric pyroCb smoke mass injection (albeit three times smaller). When compared with typical convective storms, pyroCbs are characterized by relatively smaller cloud droplet and ice particle size distributions, caused by an overabundance of smoke particles that dominate nucleation, condensation, and freezing processes[11]

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