Carbon Flux Models in a Zonally Dry Tropical Forest Area (Caatinga)
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Keywords

Remote sensing
Modeling
Semi-arid

How to Cite

SILVA, J. N. B. da; MIRANDA, R. de Q.; SOARES, G. A. S.; MOURA, M. S. B. de; GALVÍNCIO, J. D. Carbon Flux Models in a Zonally Dry Tropical Forest Area (Caatinga). Sociedade & Natureza, [S. l.], v. 36, n. 1, 2024. DOI: 10.14393/SN-v36-2024-72381. Disponível em: https://seer.ufu.br/index.php/sociedadenatureza/article/view/72381. Acesso em: 2 jan. 2025.

Abstract

Studies on energy exchange in ecosystems are critical for understanding carbon flows amid different vegetation patterns. In semi-arid areas, comprehending the variability in carbon absorption is essential for quantifying and anticipating the impacts of changes in the caatinga ecosystem. This study aims to calibrate and evaluate models for Gross Primary Production (GPP), Net Ecosystem Exchange (NEE), and Ecosystem Respiration (Reco) in the caatinga biome. NEE measurements were obtained and calculated at 30-minute intervals using EddyPro 3.6 software, from raw data measured at 10 Hz. GPP was estimated by partitioning NEE and Reco, all measured in micromoles of CO2 per square meter per second (μmol CO2 m⁻² s⁻¹) using the eddy covariance (EC) tower, installed in a legal reserve at Embrapa Semiárido, in Petrolina, Pernambuco, within a section of the caatinga canopy. Following the measurement of carbon fluxes and ecosystem respiration, field measurements were conducted using a portable FieldSpec HandHeld spectroradiometer to obtain the reflectance of the canopy around the turbulent eddy covariance tower. These measurements were carried out in 2015 in a preserved caatinga area. Multiple linear regression models were developed to estimate carbon fluxes from orbital images, enabling accurate estimation of GPP, NEE, and Reco, using the MODIS/Terra Daily Surface Reflectance product (MOD09GA). The primary results demonstrate the effectiveness of the developed models, particularly the GPP model, which exhibited the best statistical indices (R = 0.97; R² = 0.95; Root Mean Square Error = 0.20). Observations from the EC tower indicated that the models developed to estimate NEE, GPP, and Reco, using visible and near-infrared reflectance data, accurately represented the dry period and effectively captured the phenological aspects of the caatinga ecosystem.

https://doi.org/10.14393/SN-v36-2024-72381
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Copyright (c) 2023 Joélia Natália Bezerra Silva, Rodrigo de Queiroga Miranda, Gabriel Antonio Silva Soares, Magna Soelma Besera de Moura, Josiclêda Domiciano Galvíncio

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