Articles | Volume 12, issue 1
https://doi.org/10.5194/bg-12-147-2015
https://doi.org/10.5194/bg-12-147-2015
Research article
 | 
09 Jan 2015
Research article |  | 09 Jan 2015

The effects of river inflow and retention time on the spatial heterogeneity of chlorophyll and water–air CO2 fluxes in a tropical hydropower reservoir

F. S. Pacheco, M. C. S. Soares, A. T. Assireu, M. P. Curtarelli, F. Roland, G. Abril, J. L. Stech, P. C. Alvalá, and J. P. Ometto

Download

Interactive discussion

Status: closed
Status: closed
AC: Author comment | RC: Referee comment | SC: Short comment | EC: Editor comment
Printer-friendly Version - Printer-friendly version Supplement - Supplement

Peer-review completion

AR: Author's response | RR: Referee report | ED: Editor decision
AR by F. S. Pacheco on behalf of the Authors (14 Oct 2014)  Author's response    Manuscript
ED: Referee Nomination & Report Request started (27 Oct 2014) by Tom J. Battin
RR by Anonymous Referee #1 (03 Nov 2014)
RR by Anonymous Referee #2 (13 Nov 2014)
ED: Publish subject to technical corrections (01 Dec 2014) by Tom J. Battin
AR by F. S. Pacheco on behalf of the Authors (13 Dec 2014)  Author's response    Manuscript
Download
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.
Altmetrics
Final-revised paper
Preprint