EGU23-8967, updated on 26 Feb 2023
https://doi.org/10.5194/egusphere-egu23-8967
EGU General Assembly 2023
© Author(s) 2023. This work is distributed under
the Creative Commons Attribution 4.0 License.

Modelling pyro-convective activity and the meteorological conditions leading to mega-fires

Cátia Campos1,2, Flavio T. Couto1,2, Carolina Purificação1,2, Jean-Baptiste Filippi3, Roberta Baggio3, and Rui Salgado1,2
Cátia Campos et al.
  • 1University of Evora, Institute of Earth Sciences - University of Evora Pole, Évora, Portugal. (catiacampos1998@hotmail.com)
  • 2Earth Remote Sensing Laboratory (EaRS Lab), Universidade de Évora, Évora, Portugal.
  • 3Centre National de la Recherche Scientifique (CNRS), Sciences Pour l’Environnement – Unite ì Mixte de Recherche 6134, Università di Corsica, Campus Grossetti, Corte, France.

Mega-fires are wildfires that burn an area greater than 10.000 hectares. Despite being a minority in relation to the total number of fires, they are the one with the greatest negative impact on society and the environment. Associated with this wildfire type, the phenomenon of pyro-convection has been reported in several cases. Strong pyro-convective activity can lead to the formation of clouds within the smoke plume, also known as pyro-cumulus (PyroCu) or pyro-cumulonimbus (PyroCb). In 2017, Portugal recorded 11 mega-fires, of which 8 occurred on the 15th October. Since the photographic evidence of the formation of a PyroCu cloud, the chosen case study was the Quiaios mega-fire. The study aims to simulate the impact of a fire in the atmosphere, as well as the large-scale meteorological conditions that were affecting Portugal during the mega-fires. For this purpose, two numerical simulations were performed using the MesoNH atmospheric model: a coupled simulation with the ForeFire fire propagation model, with 3 nested domains with resolution of 2000m, 400m and 80m (300 by 300 grid points), and a large-scale non-coupled simulation, with a 15km resolution (300 by 250 grid points) to study the large-scale conditions. The coupled simulation allowed identifying the formation of a PyroCu cloud composed by different species of hydrometeors, namely graupel and rain droplets. The pyro-cloud developed inside the plume due the vertical transport of water vapor to higher levels. In the context of large scale, the simulation well represented the evolution of hurricane Ophelia, showing the change in wind direction from Southeast to Southwest in Portuguese territory, which created a favourable condition to the intensification of the active fires and the development of PyroCb clouds during the late afternoon. This study was funded by national funds through FCT-Foundation for Science and Technology, I.P. under the PyroC.pt project (Ref. PCIF/MPG/0175/2019).

 

How to cite: Campos, C., Couto, F. T., Purificação, C., Filippi, J.-B., Baggio, R., and Salgado, R.: Modelling pyro-convective activity and the meteorological conditions leading to mega-fires, EGU General Assembly 2023, Vienna, Austria, 24–28 Apr 2023, EGU23-8967, https://doi.org/10.5194/egusphere-egu23-8967, 2023.