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Direct radiative forcing of biomass burning aerosols from the extensive Australian wildfires in 2019–2020

Bibliographic Data

ID15546387
AuthorsDong Yeong Chang (0000-0003-2614-0397, Seoul National University), Jongmin Yoon (National Institute of Environmental Research, corresponding author), Jos Lelieveld (0000-0001-6307-3846, Cyprus Institute), Seon Ki Park (0000-0002-8538-911X, Ewha Womans University), Seong Soo Yum (0000-0002-0879-1615, Yonsei University), Jhoon Kim (0000-0002-1508-9218, Yonsei University), Sujong Jeong (0000-0003-4586-4534, Seoul National University)
Year2021
Volume16
Issue4
Pages044041-044041
Publication date2021-03-09
Open AccessYes
TypeARTICLE
VenueEnvironmental Research Letters (JOURNAL)
Journal identifiersISSN: 1748-9326 • E-ISSN: 1748-9326
PublisherIOP Publishing (PUBLISHER • GB)
DOI10.1088/1748-9326/abecfe
OpenAlexW3134579764
LanguageEN
Citations received1
References cited39

In 2019, an unusually strong positive Indian Ocean Dipole spawned hot and dry weather in southeastern Australia, which promoted devastating wildfires in the period from September 2019 to February 2020. The fires produced large plumes of biomass burning aerosols that prevented sunlight from reaching the Earth’s surface, and in this way elicited regional radiative cooling. We estimated the direct aerosol radiative forcing (ARF) resulting from these wildfires, based on Moderate Resolution Imaging Spectroradiometer space-based data and an empirical relationship from AErosol RObotic NETwork ground-based data collected in biomass-burning regions. The wildfire-derived air pollution was associated with an aerosol optical thickness of >0.3 in Victoria and a strongly negative ARF of between −14.8 and −17.7 W m −2 , which decreased the surface air temperature by about 3.7 °C–4.4 °C. This is of the same order of magnitude as the radiative cooling from volcanic eruptions. Although the atmospheric lifetime of biomass-burning aerosols is relatively short (about a week), the Australian wildfire pollution plumes extended across the Pacific Ocean to South America. Since climate change is expected to lead to more frequent and increasingly intense fires in many regions worldwide, the consequent biomass burning aerosols may become a significant radiative forcing factor, which will need to be accounted for in climate model projections for the future

Aerosol · Atmospheric sciences · Biomass burning · Climate change · Climate model · Climatology · Forcing (mathematics · Geography · Meteorology · Moderate-resolution imaging spectroradiometer · Radiative forcing · Radiative transfer · Satellite · Atmospheric aerosols and clouds · Atmospheric and Environmental Gas Dynamics · Atmospheric chemistry and aerosols · Environmental Science · Geology · Oceanography

  • Responses of wildfire-induced global black carbon pollution and radiative forcing to climate change

    Open Access•Xinrui Liu, Jianmin Ma et al.•Environmental Research Letters•2023

  • Analysis of daily, monthly, and annual burned area using the fourth‐generation global fire emissions database (GFED4)

    Open Access•Louis Giglio, James T Randerson et al.•Journal of Geophysical Research:…•2013

  • Fire in the Earth System

    Open Access•David M J S Bowman, Jennifer K Balch et al.•Science•2009

  • Climate-induced variations in global wildfire danger from 1979 to 2013

    Open Access•W Matt Jolly, Mark A Cochrane et al.•Nature Communications•2015

Citations per year0.33
Citation span2023 - 2023 (1)
Highly citedNo

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