Abstract
Achieving climate targets requires mitigation against climate change, but also understanding of the response of land and ocean carbon systems. In this context, global soil carbon stocks and its response to environmental changes is key. In this presentation, the global soil carbon feedbacks to both changes in atmospheric CO2 and associated climate changes for Earth system models (ESMs) in CMIP6 are quantified. A standard approach is used to calculate the carbon cycle feedbacks, which are defined as soil specific carbon-concentration (βs) and carbon-climate (γs) feedback parameters. Amongst CMIP6 ESMs, it is shown that the sensitivity to CO2 is found to dominate global soil carbon changes at least up to a doubling of atmospheric CO2. However, the sensitivity of soil carbon to climate change is found to become an increasingly important source of uncertainty under higher atmospheric CO2 concentrations.
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