How the extreme 2019-2020 Australian wildfires affected global circulation and adjustments

• Main Authors: Senf, Fabian, Heinold, Bernd, Kubin, Anne, Müller, Jason, Schrödner, Roland, Tegen, Ina
• Format: Article in Journal/Newspaper
• Language: English
• Published: Katlenburg-Lindau : EGU 2023
• Subjects: ddc:550; Australia; aerosol; atmospheric circulation; carbon dioxide; climate effect; climate modeling; longwave radiation; meridional circulation; radiative forcing; Southern Hemisphere; stratosphere; troposphere; wildfire; Southern Ocean
• Online Access: https://oa.tib.eu/renate/handle/123456789/14690; https://doi.org/10.34657/13712

Wildfires are a significant source of absorbing aerosols in the atmosphere. Extreme fires in particular, such as those during the 2019-2020 Australian wildfire season (Black Summer fires), can have considerable large-scale effects. In this context, the climate impact of extreme wildfires unfolds not only because of the emitted carbon dioxide but also due to smoke aerosol released up to an altitude of 17ĝ€¯km. The overall aerosol effects depend on a variety of factors, such as the amount emitted, the injection height, and the composition of the burned material, and is therefore subject to considerable uncertainty. In the present study, we address the global impact caused by the exceptionally strong and high-reaching smoke emissions from the Australian wildfires using simulations with a global aerosol-climate model. We show that the absorption of solar radiation by the black carbon contained in the emitted smoke led to a shortwave radiative forcing of more than +5ĝ€¯Wm-2 in the southern mid-latitudes of the lower stratosphere. Subsequent adjustment processes in the stratosphere slowed down the diabatically driven meridional circulation, thus redistributing the heating perturbation on a global scale. As a result of these stratospheric adjustments, a positive temperature perturbation developed in both hemispheres, leading to additional longwave radiation emitted back to space. According to the model results, this adjustment occurred in the stratosphere within the first 2 months after the event. At the top of the atmosphere (TOA), the net effective radiative forcing (ERF) averaged over the Southern Hemisphere was initially dominated by the instantaneous positive radiative forcing of about +0.5ĝ€¯Wm-2, for which the positive sign resulted mainly from the presence of clouds above the Southern Ocean. The longwave adjustments led to a compensation of the initially net positive TOA ERF, which is seen in the Southern Hemisphere, the tropics, and the northern mid-latitudes. The simulated changes in the lower stratosphere ...