The importance of antecedent vegetation and drought conditions as global drivers of burnt areaThe importance of antecedent vegetation and drought conditions as global drivers of burnt area Peer-Reviewed Journal Publication Δημοσίευση σε Περιοδικό με Κριτές 2023-01-102021enThis article is part of the special issue “The role of fire in the Earth system: understanding interactions with the land, atmosphere, and society (ESD/ACP/BG/GMD/NHESS inter-journal SI)”. It is a result of the EGU General Assembly 2020, 3–8 May 2020The seasonal and longer-term dynamics of fuel accumulation affect fire seasonality and the occurrence of extreme wildfires. Failure to account for their influence may help to explain why state-of-the-art fire models do not simulate the length and timing of the fire season or interannual variability in burnt area well. We investigated the impact of accounting for different timescales of fuel production and accumulation on burnt area using a suite of random forest regression models that included the immediate impact of climate, vegetation, and human influences in a given month and tested the impact of various combinations of antecedent conditions in four productivity-related vegetation indices and in antecedent moisture conditions. Analyses were conducted for the period from 2010 to 2015 inclusive. Inclusion of antecedent vegetation conditions representing fuel build-up led to an improvement of the global, climatological out-of-sample R2 from 0.579 to 0.701, but the inclusion of antecedent vegetation conditions on timescales ≥ 1 year had no impact on simulated burnt area. Current moisture levels were the dominant influence on fuel drying. Additionally, antecedent moisture levels were important for fuel build-up. The models also enabled the visualisation of interactions between variables, such as the importance of antecedent productivity coupled with instantaneous drying. The length of the period which needs to be considered varies across biomes; fuel-limited regions are sensitive to antecedent conditions that determine fuel build-up over longer time periods (∼ 4 months), while moisture-limited regions are more sensitive to current conditions that regulate fuel drying.http://creativecommons.org/licenses/by/4.0/Biogeosciences18123861–3879Kuhn-Régnier_et_al_Biogeosciences_18(12)_2021.pdfChania [Greece]Library of TUC2023-01-10application/pdf3.9 MBfree Kuhn-Régnie Alexander Voulgarakis Apostolos Βουλγαρακης Αποστολος Nowack Peer Forkel Matthias Prentice, I. Colin, 1952- Harrison Sandy Copernicus Publications Fire Wildfire Soil moisture Climate change