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A derivation error that affects carbon balance models exists in the current implementation of the modified Arrhenius
Bridget K Murphy1,2, Joseph R Stinziano3
1Department of Biology, University of Toronto Mississauga, Mississauga, ON, L5L 1C6, Canada.
The New Phytologist
|August 18, 2020
Summary
A crucial term was missing in the modified Arrhenius equation used for modeling temperature responses in plants. Correcting this error significantly impacts predictions of daily carbon gain and global carbon fluxes.
Area of Science:
- Plant physiology
- Biogeochemical cycles
- Climate modeling
Background:
- Accurate modeling of biological temperature responses is essential for predicting global carbon fluxes.
- Current large-scale models use a modified Arrhenius equation to represent temperature responses of photosynthetic capacity.
Purpose of the Study:
- To rederive the modified Arrhenius equation and identify any discrepancies.
- To assess the impact of a previously overlooked term on temperature response parameters and carbon gain predictions.
Main Methods:
- Re-derivation of the modified Arrhenius equation from its 1942 source publication.
- Comparison of fitted temperature response parameters using the correct and erroneous derivations.
- Scaling the impact of derived parameter differences on whole-plant carbon balance.
Main Results:
- A critical term was found to be missing from the modified Arrhenius equation after 2002.
- While most parameters showed minimal changes, activation energy was substantially affected.
- The corrected equation led to a significant deviation of approximately 18% day⁻¹ in modeled daily carbon gain.
Conclusions:
- The error in the modified Arrhenius equation derivation has impacted the accuracy of carbon flux predictions in Earth System Models.
- Over 40% of current Earth System Models may contain this erroneous derivation, affecting large-scale predictions.
- Correction of the derivation error is recommended for future modeling efforts to improve the accuracy of global carbon flux predictions.
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