EGU25-5023, updated on 14 Mar 2025
https://doi.org/10.5194/egusphere-egu25-5023
EGU General Assembly 2025
© Author(s) 2025. This work is distributed under
the Creative Commons Attribution 4.0 License.
Oral | Wednesday, 30 Apr, 16:15–16:25 (CEST)
 
Room F2
Increasing aerosol emissions from boreal biomass burning exacerbate Arctic warming
Qirui Zhong1, Nick Schutgens2, Sander Veraverbeke2,3, Guido van der Werf4, and Shu Tao1
Qirui Zhong et al.
  • 1College of Urban and Environmental Sciences, Peking University, Beijing, China
  • 2Department of Earth Sciences, Vrije Universiteit, Amsterdam, The Netherlands
  • 3School of Environmental Sciences, University of East Anglia, Norwich, UK
  • 4Environmental Sciences Group, Wageningen University and Research, Wageningen, The Netherlands

The Northern Hemisphere boreal region is undergoing rapid warming, leading to an upsurge in biomass burning. Previous studies have primarily focused on greenhouse gas emissions from these fires, whereas the associated biomass burning aerosols (BBAs) have received less attention. Here we use satellite-constrained modelling to assess the radiative effect of aerosols from boreal fires on the climate in the Arctic region. We find a substantial increase in boreal BBA emissions associated with warming over the past two decades, causing pronounced positive radiative effects during Arctic summer mostly due to increased solar absorption. At a global warming level of 1 °C above current temperatures, boreal BBA emissions are projected to increase 6-fold, further warming the Arctic and potentially negating the benefits of ambitious anthropogenic black carbon mitigation. Given the high sensitivity of boreal and Arctic fires to climate change, our results underscore the increasingly relevant role of BBAs in Arctic climate.

How to cite: Zhong, Q., Schutgens, N., Veraverbeke, S., van der Werf, G., and Tao, S.: Increasing aerosol emissions from boreal biomass burning exacerbate Arctic warming, EGU General Assembly 2025, Vienna, Austria, 27 Apr–2 May 2025, EGU25-5023, https://doi.org/10.5194/egusphere-egu25-5023, 2025.