Precipitation–fire functional interactions control biomass stocks and carbon exchanges across the world's largest savanna

Abstract. Southern African woodlands (SAW) are the world's largest savanna, covering ∼ 3 M km2, but their carbon balance and its interactions with climate and disturbance are poorly understood. Here we address three issues that hinder regional efforts to address international climate agreements: producing a state-of-the-art C budget of the SAW region; diagnosing C cycle functional variation and interactions with climate and fire across SAW; and evaluating SAW C cycle representation in land surface models (LSMs). Using 1506 independent 0.5° pixel model calibrations, each constrained with local Earth observation time series of woody carbon stocks (Cwood) and leaf area, we produce a regional SAW C analysis (2006–2017). The regional net biome production is neutral, i.e. −0.08 Mg C ha−1 yr−1 (95 % uncertainty interval −1.67/1.66), with fire emissions contributing ∼ 0.88 Mg C ha−1 yr−1 (95 % uncertainty interval 0.36–2.51). Fire-related mortality driving fluxes from the total Cwood to dead organic matter likely exceeds both fire-related emissions from Cwood into the atmosphere and non-fire Cwood mortality. The emergent spatial variation in biogenic fluxes and C pools is strongly correlated with mean annual precipitation and burned area. However, there are multiple, potentially confounding, causal pathways through which variation in environmental drivers impacts the spatial distribution of C stocks and fluxes, which is mediated by spatial variations in functional parameters like allocation, wood lifespan, and fire resilience. More Cwood in wetter areas is caused by positive precipitation effects on net primary production and on parameters for wood lifespan but is damped by a negative effect with rising precipitation increasing fire-related mortality. Compared to this analysis, LSMs showed marked differences in spatial distributions and magnitudes of C stocks and fire emissions. The current generation of LSMs represents savanna as a single plant functional type, missing important spatial functional variations identified here. Patterns of biomass and C cycling across the region are the outcome of climate controls on production and vegetation–fire interactions which determine residence times, which is linked to spatial variations in key ecosystem functional characteristics.

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Publication Details

Journal
Biogeosciences
Published
2025-03-27
DOI
https://doi.org/10.5194/bg-22-1597-2025
Citations
5
Primary Topic
Fire effects on ecosystems
Type
article
Field-Weighted Citation Impact
5.53

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article

Precipitation–fire functional interactions control biomass stocks and carbon exchanges across the world's largest savanna

Aude Valade, Iain M. McNicol, Mathew Williams, Carla Roesch et al.
5 citations
Biogeosciences
Fire effects on ecosystems
5.53
article

Precipitation–fire functional interactions control biomass stocks and carbon exchanges across the world's largest savanna

Aude Valade, Iain M. McNicol, Mathew Williams, Carla Roesch, David T. Milodowski, Michael O’Sullivan, Stephen A. Sitch, Kyle Graham Dexter, Gabriele C. Hegerl, Casey M. Ryan, T. Luke Smallman
article en
5 citations

Abstract

Abstract. Southern African woodlands (SAW) are the world's largest savanna, covering ∼ 3 M km2, but their carbon balance and its interactions with climate and disturbance are poorly understood. Here we address three issues that hinder regional efforts to address international climate agreements: producing a state-of-the-art C budget of the SAW region; diagnosing C cycle functional variation and interactions with climate and fire across SAW; and evaluating SAW C cycle representation in land surface models (LSMs). Using 1506 independent 0.5° pixel model calibrations, each constrained with local Earth observation time series of woody carbon stocks (Cwood) and leaf area, we produce a regional SAW C analysis (2006–2017). The regional net biome production is neutral, i.e. −0.08 Mg C ha−1 yr−1 (95 % uncertainty interval −1.67/1.66), with fire emissions contributing ∼ 0.88 Mg C ha−1 yr−1 (95 % uncertainty interval 0.36–2.51). Fire-related mortality driving fluxes from the total Cwood to dead organic matter likely exceeds both fire-related emissions from Cwood into the atmosphere and non-fire Cwood mortality. The emergent spatial variation in biogenic fluxes and C pools is strongly correlated with mean annual precipitation and burned area. However, there are multiple, potentially confounding, causal pathways through which variation in environmental drivers impacts the spatial distribution of C stocks and fluxes, which is mediated by spatial variations in functional parameters like allocation, wood lifespan, and fire resilience. More Cwood in wetter areas is caused by positive precipitation effects on net primary production and on parameters for wood lifespan but is damped by a negative effect with rising precipitation increasing fire-related mortality. Compared to this analysis, LSMs showed marked differences in spatial distributions and magnitudes of C stocks and fire emissions. The current generation of LSMs represents savanna as a single plant functional type, missing important spatial functional variations identified here. Patterns of biomass and C cycling across the region are the outcome of climate controls on production and vegetation–fire interactions which determine residence times, which is linked to spatial variations in key ecosystem functional characteristics.

BiogeosciencesVol. 22(6)
University of Exeter (GB), Ecologie fonctionnelle & biogéochimie des sols & des agro-systèmes (FR), National Centre for Earth Observation (GB), University of Edinburgh (GB)
UK Research and Innovation, Sight Research UK, European Commission, Natural Environment Research Council, Japan Aerospace Exploration Agency, National Centre for Earth Observation
Openalex Percentile: Top 5%
Fire effects on ecosystems
5.53
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