4.6 Review

Matrix Approach to Land Carbon Cycle Modeling

Journal

Publisher

AMER GEOPHYSICAL UNION
DOI: 10.1029/2022MS003008

Keywords

biogeochemistry; carbon cycle; dynamical equation; terrestrial ecosystems; uncertainty analysis

Funding

  1. US National Science Foundation [DEB 1655499, DEB 2017884]
  2. US Department of Energy [DE-SC0020227]
  3. Oak Ridge National Laboratory (ORNL) [4000158404, 4000161830]
  4. German Research Foundation [SI 1953/2-1]
  5. U.S. Department of Energy (DOE) [DE-SC0020227] Funding Source: U.S. Department of Energy (DOE)

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Land ecosystems play an important role in mitigating climate change by absorbing approximately 30% of anthropogenic carbon emissions. However, the uncertainty in estimating the amount and distribution of carbon uptake across different ecosystems or biomes hinders a comprehensive understanding of the mechanisms and drivers of land carbon uptake, as well as predictions of future land carbon sink. In order to advance land carbon cycle modeling, researchers have developed a matrix approach that organizes carbon balance equations into a single matrix equation, allowing for a theoretical framework to understand the behavior of the land carbon cycle. This matrix approach offers computational efficiency, helping to address key issues in modeling and improve predictions using increasingly available data.
Land ecosystems contribute to climate change mitigation by taking up approximately 30% of anthropogenically emitted carbon. However, estimates of the amount and distribution of carbon uptake across the world's ecosystems or biomes display great uncertainty. The latter hinders a full understanding of the mechanisms and drivers of land carbon uptake, and predictions of the future fate of the land carbon sink. The latter is needed as evidence to inform climate mitigation strategies such as afforestation schemes. To advance land carbon cycle modeling, we have developed a matrix approach. Land carbon cycle models use carbon balance equations to represent carbon exchanges among pools. Our approach organizes this set of equations into a single matrix equation without altering any processes of the original model. The matrix equation enables the development of a theoretical framework for understanding the general, transient behavior of the land carbon cycle. While carbon input and residence time are used to quantify carbon storage capacity at steady state, a third quantity, carbon storage potential, integrates fluxes with time to define dynamic disequilibrium of the carbon cycle under global change. The matrix approach can help address critical contemporary issues in modeling, including pinpointing sources of model uncertainty and accelerating spin-up of land carbon cycle models by tens of times. The accelerated spin-up liberates models from the computational burden that hinders comprehensive parameter sensitivity analysis and assimilation of observational data to improve model accuracy. Such computational efficiency offered by the matrix approach enables substantial improvement of model predictions using ever-increasing data availability. Overall, the matrix approach offers a step change forward for understanding and modeling the land carbon cycle.

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