The whole-soil carbon flux in response to warming
Lawrence Berkeley National Laboratory · University of California, Berkeley
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Abstract
Production from all soil depths increased with 4°C warming; annual soil respiration increased by 34 to 37%. All depths responded to warming with similar temperature sensitivities, driven by decomposition of decadal-aged carbon. Whole-soil warming reveals a larger soil respiration response than many in situ experiments (most of which only warm the surface soil) and models.
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4Topics & keywords
Topics
Keywords
- Carbon flux
- Environmental science
- Flux (metallurgy)
- Soil carbon
- Global warming
- Carbon fibers
- Atmospheric sciences
- Climate change
UN Sustainable Development Goals
- Climate action
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