Seasonal variation in net ecosystem CO2 exchange of a Brazilian seasonally dry tropical forest

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作者
Keila R. Mendes
Suany Campos
Lindenberg L. da Silva
Pedro R. Mutti
Rosaria R. Ferreira
Salomão S. Medeiros
Aldrin M. Perez-Marin
Thiago V. Marques
Tarsila M. Ramos
Mariana M. de Lima Vieira
Cristiano P. Oliveira
Weber A. Gonçalves
Gabriel B. Costa
Antonio C. D. Antonino
Rômulo S. C. Menezes
Bergson G. Bezerra
Cláudio M. Santos e Silva
机构
[1] Climate Sciences Post-graduate Program,Meteorology Post
[2] Federal University of Rio Grande do Norte,graduate Program
[3] Federal University of Campina Grande,National Institute of Semi
[4] Rua Aprígio Veloso,Arid
[5] 882,Department of Atmospheric and Climate Sciences
[6] Zip Code 58429-900,Institute of Biodiversity and Forests
[7] Universitário,undefined
[8] Av. Francisco Lopes de Almeida,undefined
[9] s/n,undefined
[10] Zip Code 58434-700,undefined
[11] Serrotão,undefined
[12] Federal University of Rio Grande do Norte,undefined
[13] Av. Senador Salgado Filho,undefined
[14] 3000,undefined
[15] Federal University of Western Pará,undefined
[16] UFOPA,undefined
[17] Federal University of Pernambuco,undefined
[18] Department of Nuclear Energy,undefined
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摘要
Forest ecosystems sequester large amounts of atmospheric CO2, and the contribution from seasonally dry tropical forests is not negligible. Thus, the objective of this study was to quantify and evaluate the seasonal and annual patterns of CO2 exchanges in the Caatinga biome, as well as to evaluate the ecosystem condition as carbon sink or source during years. In addition, we analyzed the climatic factors that control the seasonal variability of gross primary production (GPP), ecosystem respiration (Reco) and net ecosystem CO2 exchange (NEE). Results showed that the dynamics of the components of the CO2 fluxes varied depending on the magnitude and distribution of rainfall and, as a consequence, on the variability of the vegetation state. Annual cumulative NEE was significantly higher (p < 0.01) in 2014 (−169.0 g C m−2) when compared to 2015 (−145.0 g C m−2) and annual NEP/GPP ratio was 0.41 in 2014 and 0.43 in 2015. Global radiation, air and soil temperature were the main factors associated with the diurnal variability of carbon fluxes. Even during the dry season, the NEE was at equilibrium and the Caatinga acted as an atmospheric carbon sink during the years 2014 and 2015.
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