EGU26-21635, updated on 14 Mar 2026
https://doi.org/10.5194/egusphere-egu26-21635
EGU General Assembly 2026
© Author(s) 2026. This work is distributed under
the Creative Commons Attribution 4.0 License.
Oral | Tuesday, 05 May, 14:20–14:30 (CEST)
 
Room N2
The multi-decadal hazard cascade of a tropical mountain wildfire
Martha Day1, William Veness1, Anthony Ross1, Yazidhi Bamutaze2, Jiayuan Han1, Douglas Mulangwa3,4, Andrew Mwesigwa4, Emmanuel Ntale5, Callist Tindimugaya5, Brian Guma5, Elisabeth Stephens6,7, and Wouter Buytaert1
Martha Day et al.
  • 1Imperial College London, Civil and Environmental Engineering, London, United Kingdom of Great Britain – England, Scotland, Wales (martha.day18@imperial.ac.uk)
  • 2Department of Geography, Geo-Informatics and Climatic Sciences, Makerere University, Kampala, Uganda
  • 3Department of Meteorology, University of Reading, Reading, RG6 6BB, UK
  • 4Ministry of Water and Environment, Kampala, Uganda
  • 5Uganda Red Cross Society, Kampala, Uganda
  • 6Department of Meteorology, University of Reading, Reading, RG6 6BB, UK
  • 7Red Cross Red Crescent Climate Centre, The Hague, The Netherlands

Climate change is driving wildfires to higher elevations, yet the hazard cascades that follow the burning of pristine tropical mountain ecosystems remain largely unexplored. We present an integrated multi-hazard risk assessment methodology combining quantitative remote sensing with qualitative humanitarian and community data, addressing the challenge of characterising cascading hazards in data-scarce mountain environments. Here, we apply this approach to analyse the long-term cascade following a February 2012 wildfire that burned 31 km² of forest and wetland in Uganda's Rwenzori Mountains National Park. We document ten major floods since 2012, including two debris floods in 2013 and 2020 that affected 200,000 people requiring large-scale humanitarian responses. Post-fire increases in erosion and mass movement have widened the River Nyamwamba sevenfold since 2012, breaching copper-cobalt mine tailings and mobilising an estimated 744,000 tonnes of waste into the river resulting in widespread pollution of the river and floodplains. Slow vegetation recovery at high altitudes and positive feedbacks between hazards have prolonged this high-risk state, demonstrating how hazard interactions compound to sustain elevated risk beyond typical post-fire recovery periods.

This study demonstrates how the characterisation of multi-hazard cascades and their interactions enable identification of management entry points in resource-constrained settings. However, challenges remain in multi-hazard risk management across spatial and temporal scales; montane environments globally, especially those without a history of fire, suffer from inadequate monitoring infrastructure and limited understanding of post-fire hazard interactions. The intensity and persistence of the Rwenzori hazard cascade highlights how wildfires in mature, fire-sensitive mountain ecosystems can impose long-lasting risks on downstream communities. We recommend that post-fire risk assessments be triggered at lower thresholds of burn area and severity when fires occur in fire-sensitive mountain ecosystems, and that investment in long-term monitoring be prioritized to capture the full temporal evolution of hazard cascades.

How to cite: Day, M., Veness, W., Ross, A., Bamutaze, Y., Han, J., Mulangwa, D., Mwesigwa, A., Ntale, E., Tindimugaya, C., Guma, B., Stephens, E., and Buytaert, W.: The multi-decadal hazard cascade of a tropical mountain wildfire, EGU General Assembly 2026, Vienna, Austria, 3–8 May 2026, EGU26-21635, https://doi.org/10.5194/egusphere-egu26-21635, 2026.