Preprints
https://doi.org/10.5194/egusphere-2026-979
https://doi.org/10.5194/egusphere-2026-979
10 Apr 2026
 | 10 Apr 2026
Status: this preprint is open for discussion and under review for Atmospheric Chemistry and Physics (ACP).

Assessment of WRF-GHG model simulations during the CAFE-Brazil Campaign in Amazonia

Noelia R. Benavente, Santiago Botía, Luciana V. Rizzo, Angel Vara-Vela, Paulo Artaxo, Hella van Asperen, Felipe Santos da Silva, Flavio A. F. D'Oliveira, Horst Fischer, Michał Gałkowski, Theo Glauch, Alice Henkes, David Ho, Cléo Q. Dias-Júnior, Amauri C. P. Junior, Julia Marshall, Linda Ort, Ben-Hur M. Portella, and Luiz A. T. Machado

Abstract. The Amazon Basin plays an important role in the global climate and carbon budget, with natural emissions and removals of CO2 and CH4 prevailing in the wet season. Accurate modeling of the transport of greenhouse gases (GHG) is essential for understanding the contributions of sources, sinks, and atmospheric processes. High-resolution atmospheric models offer a compromise between computational cost and physical realism, capturing mesoscale processes that influence GHG transport in the Amazon. We evaluate the WRF-GHG model (Weather Research and Forecasting Model with GHG module) using CO2 and CH4 measurements from the Amazon Tall Tower Observatory (ATTO) and aircraft observations during the CAFE-Brazil campaign in January 2023. Simulations employed two domains centered at ATTO, with MapBiomas land cover data, region-specific parameters for CO2 biogenic emissions and removals, and multiple wetland CH4 emission configurations. Comparisons with ATTO indicate that the regionally adapted biogenic flux parameterizations improved the representation of CO2 and net ecosystem exchange (NEE). For CH4, CAMS Inversion-optimized flux product best reproduces observed concentrations, while the Kaplan diagnostic model and WetCHARTs inventories overestimate near-surface mole fractions. The model predicts diurnal CH4 fluctuations, controlled by boundary-layer dynamics and atmospheric transport, that were not observed at ATTO. Comparisons with CAFE-Brazil aircraft data indicated regional wetland sources and wind-driven transport driving the observed CH4 enhancements. These findings underscore the importance of improving the parameterization of biogenic fluxes to enhance the capability of models in complex tropical environments like the Amazon Basin and to accurately describe the complex circulation between rivers, upland areas, and floodplains.

Publisher's note: Copernicus Publications remains neutral with regard to jurisdictional claims made in the text, published maps, institutional affiliations, or any other geographical representation in this paper. While Copernicus Publications makes every effort to include appropriate place names, the final responsibility lies with the authors. Views expressed in the text are those of the authors and do not necessarily reflect the views of the publisher.
Share
Noelia R. Benavente, Santiago Botía, Luciana V. Rizzo, Angel Vara-Vela, Paulo Artaxo, Hella van Asperen, Felipe Santos da Silva, Flavio A. F. D'Oliveira, Horst Fischer, Michał Gałkowski, Theo Glauch, Alice Henkes, David Ho, Cléo Q. Dias-Júnior, Amauri C. P. Junior, Julia Marshall, Linda Ort, Ben-Hur M. Portella, and Luiz A. T. Machado

Status: open (until 22 May 2026)

Comment types: AC – author | RC – referee | CC – community | EC – editor | CEC – chief editor | : Report abuse
Noelia R. Benavente, Santiago Botía, Luciana V. Rizzo, Angel Vara-Vela, Paulo Artaxo, Hella van Asperen, Felipe Santos da Silva, Flavio A. F. D'Oliveira, Horst Fischer, Michał Gałkowski, Theo Glauch, Alice Henkes, David Ho, Cléo Q. Dias-Júnior, Amauri C. P. Junior, Julia Marshall, Linda Ort, Ben-Hur M. Portella, and Luiz A. T. Machado
Noelia R. Benavente, Santiago Botía, Luciana V. Rizzo, Angel Vara-Vela, Paulo Artaxo, Hella van Asperen, Felipe Santos da Silva, Flavio A. F. D'Oliveira, Horst Fischer, Michał Gałkowski, Theo Glauch, Alice Henkes, David Ho, Cléo Q. Dias-Júnior, Amauri C. P. Junior, Julia Marshall, Linda Ort, Ben-Hur M. Portella, and Luiz A. T. Machado
Metrics will be available soon.
Latest update: 11 Apr 2026
Download
Short summary
The Amazon Basin plays a vital role in regulating Earth's climate by absorbing and releasing carbon dioxide and methane. We studied how a high-resolution atmospheric transport model captures these gases, comparing it with measurements from towers and aircraft over the forest. Adjusting for forest carbon exchange improved carbon dioxide results, while methane levels were heavily dependent on emission estimates. Remaining errors were linked to winds and atmospheric mixing.
Share