Anders Ahlström
Senior lecturer
Soil carbon storage capacity of drylands under altered fire regimes
Author
Summary, in English
The determinants of fire-driven changes in soil organic carbon (SOC) across broad environmental gradients remains unclear, especially in global drylands. Here we combined datasets and field sampling of fire-manipulation experiments to evaluate where and why fire changes SOC and compared our statistical model to simulations from ecosystem models. Drier ecosystems experienced larger relative changes in SOC than humid ecosystems—in some cases exceeding losses from plant biomass pools—primarily explained by high fire-driven declines in tree biomass inputs in dry ecosystems. Many ecosystem models underestimated the SOC changes in drier ecosystems. Upscaling our statistical model predicted that soils in savannah–grassland regions may have gained 0.64 PgC due to net-declines in burned area over the past approximately two decades. Consequently, ongoing declines in fire frequencies have probably created an extensive carbon sink in the soils of global drylands that may have been underestimated by ecosystem models.
Department/s
- LU Profile Area: Nature-based future solutions
- Dept of Physical Geography and Ecosystem Science
- MERGE: ModElling the Regional and Global Earth system
- BECC: Biodiversity and Ecosystem services in a Changing Climate
- MECW: The Middle East in the Contemporary World
- LTH Profile Area: Aerosols
- eSSENCE: The e-Science Collaboration
- MERGE: ModElling the Regional and Global Earth System
Publishing year
2023-10
Language
English
Pages
1089-1094
Publication/Series
Nature Climate Change
Volume
13
Issue
10
Document type
Journal article
Publisher
Nature Publishing Group
Topic
- Physical Geography
- Climate Research
Status
Published
ISBN/ISSN/Other
- ISSN: 1758-678X