Articles | Volume 12, issue 1
https://doi.org/10.5194/bg-12-147-2015
© Author(s) 2015. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
https://doi.org/10.5194/bg-12-147-2015
© Author(s) 2015. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
The effects of river inflow and retention time on the spatial heterogeneity of chlorophyll and water–air CO2 fluxes in a tropical hydropower reservoir
Earth System Science Center, National Institute for Space Research, São José dos Campos, 12227–010, São Paulo, Brazil
M. C. S. Soares
Laboratory of Aquatic Ecology, Federal University of Juiz de Fora, Juiz de Fora, 36036–900, Minas Gerais, Brazil
A. T. Assireu
Institute of Natural Resources, Federal University of Itajubá, Itajubá, 37500–903, Minas Gerais, Brazil
M. P. Curtarelli
Remote Sense Division, National Institute for Space Research, São José dos Campos, 12227–010, São Paulo, Brazil
F. Roland
Laboratory of Aquatic Ecology, Federal University of Juiz de Fora, Juiz de Fora, 36036–900, Minas Gerais, Brazil
G. Abril
Laboratoire Environnements et Paléoenvironnements Océaniques et Continentaux (EPOC), CNRS, Université Bordeaux 1, Avenue des Facultés, 33405 Talence, France
J. L. Stech
Remote Sense Division, National Institute for Space Research, São José dos Campos, 12227–010, São Paulo, Brazil
P. C. Alvalá
Earth System Science Center, National Institute for Space Research, São José dos Campos, 12227–010, São Paulo, Brazil
J. P. Ometto
Earth System Science Center, National Institute for Space Research, São José dos Campos, 12227–010, São Paulo, Brazil
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- Air–water CO2 and CH4 fluxes along a river–reservoir continuum: Case study in the Pengxi River, a tributary of the Yangtze River in the Three Gorges Reservoir, China Y. Huang et al. 10.1007/s10661-017-5926-2
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- Patterns and drivers of CH4 concentration and diffusive flux from a temperate river–reservoir system in North China F. Yang et al. 10.1016/j.jes.2021.12.004
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Latest update: 13 Dec 2024
Short summary
CO2 fluxes in Funil Reservoir (FR) is driven by primary production and river inflow dynamics. Our findings suggest that the lack of spatial data in reservoir C budget calculations can affect regional and global estimates. Our results support the idea that the FR is a dynamic system where the hydrodynamics represented by changes in the river inflow and retention time are potentially a more important force driving both the Chl and pCO2 spatial variability than the in-system ecological factors.
CO2 fluxes in Funil Reservoir (FR) is driven by primary production and river inflow dynamics....
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