Results: Cross-landscape fuel moisture was highly variable and spanned known fuel moisture thresholds, demonstrating spatial variability in the potential for wildfire spread in live Calluna and smouldering combustion in the soil organic layer. Spatial differences were particularly important during the peak spring fire season when live canopy fuel moisture was lowest and least variable. Landscape and micrometeorological factors explained up to 72% of spatial fuel moisture variation. Landscape factors were predominantly more important beyond modifying microclimate. Landscape–fuel moisture relationships showed differences by layer and season, highlighting the criticality of fuel phenology in assessing landscape fuel moisture variations in temperate environments.
Conclusions: Understanding the mechanisms driving fuel moisture variability opens opportunities to develop locally robust fuel models for input into wildfire danger rating systems, adding versatility to wildfire danger assessments as a management tool.
Copyright
PyroLife abstracts are protected by copyright. Copyright grants its holder the exclusive right of reproducing the text, translating it, and distributing/communicating it to the public, among others. An abstract published online is therefore not free of rights and nobody can publish or copy it (the text) without the rightholder’s consent. Contact the author here: k.e.little@bham.ac.uk