Abstract

The impact of wildfire on catchment water yield remains uncertain, with case studies reporting a range of observed response paths. Additionally, the impacts of fire and climate variability are often intertwined, making them difficult to evaluate separately. This study assesses how wildfire and climate influence streamflow in forested catchments. We focused on selected forested catchments in eastern Australia that have experienced both sustained drought and large fire events, but otherwise have experienced little hydrological modification. We compared the relationship between streamflow and rainfall before and after the severe fire events in the 2019/2020 season and over a longer multi-year period. We obtained historical data for streamflow, rainfall, and wildfire extent, timing, and severity for each catchment. The study found a consistent increase in streamflow with given rainfall after the 2019/2020 fire event. However, the timing of the fire aligned with the end of a prolonged major drought that affected the region. Dry conditions decrease runoff while fire increases it, which makes it difficult to attribute the flow increase to fire alone. We also assessed the relative importance of multiple potential drivers (climatic and fire-related) of changes in streamflow over a longer, multi-year historical period. We found that the impacts of historical wildfires on streamflow are generally smaller than the impacts of hydro-climatic factors such as catchment storage, which has a relative importance for the streamflow over 3 times greater than that of the fire-related factors. Our results imply that historical changes in flow in the study region are more heavily affected by climate variability than by fires at the catchment scale. They emphasize the importance for water resources management of considering regional drivers such as changing climatic conditions over wildfire, which often affects only parts of individual catchments.

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