Preprints
https://doi.org/10.5194/egusphere-2026-3167
https://doi.org/10.5194/egusphere-2026-3167
19 Jun 2026
 | 19 Jun 2026
Status: this preprint is open for discussion and under review for Biogeosciences (BG).

Quantifying canopy CO2 storage to improve long-term estimates of net ecosystem carbon exchange in the southern Amazon forest

Bárbara Antonucci, Raoni A. Santana, Nara L. R. Andrade, Eliane Gomes Alves, Santiago Botía, Carla M.A. Souza, Anne C. S. Mendonça, Shujiro Komiya, Denisi H. Hall, Natalia Restrepo-Coupe, Gabriel B. Costa, and Cléo Q. Dias-Júnior

Abstract. The Amazon rainforest plays a critical role in the global carbon cycle, yet large uncertainties remain regarding its net carbon balance. Accurate estimates of net ecosystem exchange (NEE) require accounting for the CO2 storage term, which is commonly derived from vertical CO2 profile measurements that are scarcely available at long-term flux tower sites. Here, we evaluated three approaches for estimating canopy CO2 storage at the Rebio Jaru forest site in Rondônia, Brazil: (1) a multi-point CO2 profile (MPP), (2) a single-point profile (SPP) based on a closed-path gas analyzer, and (3) a single-point eddy covariance approach (SPE) using CO2 measurements from an open-path gas analyzer. Although the methods operated simultaneously for less than two years, both simplified approaches showed strong agreement with the reference MPP method, with coefficients of determination of R2 = 0.87 for SPP and R2 = 0.79 for SPE, whereas neglecting the storage term resulted in poor agreement (R2 = 0.24). Using the SPE approach, we reconstructed a 13-year NEE time series that revealed pronounced interannual variability, with the forest generally acting as a carbon sink during La Niña conditions and shifting toward a carbon source during El Niño events and during consecutive years due to drought legacy effects. The seasonal cycle exhibited a marked carbon source peak during the transition from the dry to the wet season, likely associated with enhanced litter decomposition and increased soil respiration following the first rainfall events after prolonged dry periods. These results demonstrate that simplified single-point approaches can reliably reconstruct long-term NEE dynamics and substantially improve estimates of Amazonian carbon balance at sites where complete CO2 profile measurements are unavailable.

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Bárbara Antonucci, Raoni A. Santana, Nara L. R. Andrade, Eliane Gomes Alves, Santiago Botía, Carla M.A. Souza, Anne C. S. Mendonça, Shujiro Komiya, Denisi H. Hall, Natalia Restrepo-Coupe, Gabriel B. Costa, and Cléo Q. Dias-Júnior

Status: open (until 31 Jul 2026)

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Bárbara Antonucci, Raoni A. Santana, Nara L. R. Andrade, Eliane Gomes Alves, Santiago Botía, Carla M.A. Souza, Anne C. S. Mendonça, Shujiro Komiya, Denisi H. Hall, Natalia Restrepo-Coupe, Gabriel B. Costa, and Cléo Q. Dias-Júnior
Bárbara Antonucci, Raoni A. Santana, Nara L. R. Andrade, Eliane Gomes Alves, Santiago Botía, Carla M.A. Souza, Anne C. S. Mendonça, Shujiro Komiya, Denisi H. Hall, Natalia Restrepo-Coupe, Gabriel B. Costa, and Cléo Q. Dias-Júnior
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Short summary
The Amazon rainforest helps regulate the global climate by absorbing carbon from the atmosphere. We developed a simple method to improve long-term estimates of forest carbon exchange using measurements available at many monitoring sites. Applying this approach to a 13-year record from the southwestern Amazon showed that the forest absorbed carbon during wetter years but became a weaker carbon sink, or even a carbon source, during droughts and El Niño events.
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