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Diagnosing Linearity Along the Carbon Cascade in Terrestrial Biosphere Models and Observations
Huanyuan Zhang-Zheng1,2,3, Vivek K Arora4, Peter Anthoni5
1Environmental Change Institute, School of Geography and the Environment, University of Oxford, Oxford, UK.
Elevated carbon dioxide (eCO2) boosts photosynthesis, but its effect on net primary production (NPP) and vegetation carbon stocks (Cveg) varies. This study introduces a framework to analyze this carbon cascade, finding diverse model behaviors but an overall linear trend in the ensemble mean.
Area of Science:
- Earth System Science
- Ecology
- Climate Change Research
Background:
- Elevated carbon dioxide (eCO2) enhances photosynthesis (gross primary production, GPP), acting as a fertilizer for plants.
- The propagation of increased GPP through the carbon (C) cascade to net primary production (NPP) and vegetation C stocks (Cveg) under eCO2 is not well understood.
- Existing vegetation models may be overly sensitive to photosynthesis (source-driven) and neglect crucial sink-driven processes that influence C dynamics.
Purpose of the Study:
- To introduce and apply an analytical framework to diagnose the linearity (L) of changes in linked carbon fluxes and pools within the terrestrial carbon cycle.
- To assess how effectively increased GPP under eCO2 translates to NPP and Cveg across different plant compartments using a multi-model ensemble.
- To compare model-based linearity patterns with observation-based estimates of CO2 sensitivities.
Main Methods:
- Developed an analytical framework to calculate linearity (L) as the ratio of relative changes in linked carbon fluxes and pools.
- Applied this framework to 16 vegetation models from the TRENDY v11 ensemble.
- Analyzed observation-based estimates of CO2 sensitivities for comparison with model results.
Main Results:
- Found significant variations in linearity patterns (L) across models and geographical regions.
- Six models indicated increased vegetation carbon use efficiency (L_NPP:GPP > 1) in most grid cells, while only three showed the opposite.
- Model results for the linearity of Cveg to NPP (L_Cveg*:NPP) and root C to Cveg (L_Croot:Cveg) showed considerable spread, with some models aligning with field evidence and others diverging.
Conclusions:
- Individual models exhibit strong nonlinear behaviors in response to eCO2, leading to diverse patterns in the carbon cascade.
- Despite individual model variability, the ensemble mean suggests an overall linear behavior in terrestrial carbon cycle representations.
- Further research and improved model validation against observational data are needed to refine our understanding of carbon C cascade dynamics under eCO2.
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