Please use this identifier to cite or link to this item: https://repositorio.inpa.gov.br/handle/1/14713
Title: Variability of carbon and water fluxes following climate extremes over a tropical forest in southwestern amazonia
Authors: Zeri, Marcelo
Sá, Leonardo Deane Abreu
Manzi, Antônio Ocimar
Araú, Alessandro C.
Aguiar, Renata Gonçalves
Randow, Celso Von
Sampaio, Gilvan de Oliveira
Cardoso, Fernando Luiz
Nobre, Carlos Afonso
Keywords: Carbon
Rain
Water
Carbon
Carbon Dioxide
Soil
Water
Air Temperature
Albedo
Atmosphere
Carbon Balance
Carbon Cycle
Carbon Source
Climate Change
Drought
Ecosystem
Evapotranspiration
Flooding
Geographic Distribution
Geographic Names
Plant Water Use
Seasonal Variation
Southwestern Amazonia
Species Composition
Tropical Rain Forest
Vapor Pressure
Water Cycle
Water Vapor
Calibration
Chemistry
Climate Change
Forest
Regression Analysis
River
Season
Soil
Tropic Climate
Atmosphere
Calibration
Carbon
Carbon Dioxide
Climate Change
Droughts
Forests
Rain
Regression Analysis
Rivers
Seasons
Soil
Tropical Climate
Water
Issue Date: 2014
metadata.dc.publisher.journal: PLoS ONE
metadata.dc.relation.ispartof: Volume 9, Número 2
Abstract: The carbon and water cycles for a southwestern Amazonian forest site were investigated using the longest time series of fluxes of CO2 and water vapor ever reported for this site. The period from 2004 to 2010 included two severe droughts (2005 and 2010) and a flooding year (2009). The effects of such climate extremes were detected in annual sums of fluxes as well as in other components of the carbon and water cycles, such as gross primary production and water use efficiency. Gap-filling and flux-partitioning were applied in order to fill gaps due to missing data, and errors analysis made it possible to infer the uncertainty on the carbon balance. Overall, the site was found to have a net carbon uptake of ≈5 t C ha-1 year-1, but the effects of the drought of 2005 were still noticed in 2006, when the climate disturbance caused the site to become a net source of carbon to the atmosphere. Different regions of the Amazon forest might respond differently to climate extremes due to differences in dry season length, annual precipitation, species compositions, albedo and soil type. Longer time series of fluxes measured over several locations are required to better characterize the effects of climate anomalies on the carbon and water balances for the whole Amazon region. Such valuable datasets can also be used to calibrate biogeochemical models and infer on future scenarios of the Amazon forest carbon balance under the influence of climate change. © 2014 Zeri et al.
metadata.dc.identifier.doi: 10.1371/journal.pone.0088130
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