@InProceedings{GattiMBDCMCSATAAVGPNC:2019:AmCaBa,
author = "Gatti, Luciana Vanni and Miller, John B. and Basso, Luana
Santamaria and Domingues, Lucas Gatti and Cassol, Henrique Luis
Godinho and Marani, Luciano and Correira, Caio Silvestre de
Carvalho and Sanchez, Alber and Arai, Eg{\'{\i}}dio and Tejada,
Graciela and Arag{\~a}o, Luiz Eduardo Oliveira e Cruz de and
Anderson, Liana O. and Von Randow, Celso and Gloor, Manuel and
Peters, Wouter and Neves, Raiane Aparecida Lopes and Crispim,
Stephane Palma",
affiliation = "{Instituto Nacional de Pesquisas Espaciais (INPE)} and {NOAA/ESRL
Global Monitoring Division} and {Instituto Nacional de Pesquisas
Espaciais (INPE)} and {Instituto Nacional de Pesquisas Espaciais
(INPE)} and {Instituto Nacional de Pesquisas Espaciais (INPE)} and
{Instituto Nacional de Pesquisas Espaciais (INPE)} and {Instituto
Nacional de Pesquisas Energ{\'e}ticas (IPEN)} and {Instituto
Nacional de Pesquisas Espaciais (INPE)} and {Instituto Nacional de
Pesquisas Espaciais (INPE)} and {Instituto Nacional de Pesquisas
Espaciais (INPE)} and {Instituto Nacional de Pesquisas Espaciais
(INPE)} and {Centro Nacional de Monitoramento e Alertas de
Desastres Naturais (CEMADEN)} and {Instituto Nacional de Pesquisas
Espaciais (INPE)} and {University of Leeds} and {Wageningen
University} and {Instituto Nacional de Pesquisas Espaciais (INPE)}
and {Instituto Nacional de Pesquisas Espaciais (INPE)}",
title = "Amazon Carbon Balance and its Sensitivity to climate and
human-driven changes",
year = "2019",
organization = "AGU Fall Meeting",
abstract = "The Amazon accounts for 50% of Earths tropical rainforests hosting
the largest live carbon pools in vegetation and soils (~200 PgC).
The net carbon exchange between tropical land and the atmosphere
is critically important, because the stability of carbon in
forests and soils can be disrupted on short time-scales. The main
processes releasing C to the atmosphere are deforestation, fires
and changes in growing conditions due to increased temperatures
and droughts. Such changes may thus cause feedbacks on global
climate. In the last 40 years, the Amazon mean temperature has
increased by 1.1șC. Annual mean precipitation has also decreased
by 51 mm during this same 40 year period. The precipitation
reduction occurred mainly in the dry season, and the dry season
has lengthened, exacerbating vegetation water stress with
consequences for carbon balance. To better understand its C
budget, starting in 2010 we established a regionally
representative greenhouse gas monitoring program across Amazonia.
The program aims to quantify gas concentrations (CO2, CH4, N2O,
CO, and SF6) based on extensive collection of air from light
aircraft vertical profiles. The atmosphere is profiled from the
ground up to 4.5 km height at four sites along the main air-stream
over the Amazon Basin on a twice-monthly basis. Here we will
report what these new data tell us about the carbon balance and
its controls from 2010-2017. During this period we performed 513
vertical profiles over four strategic regions that represent
fluxes over much of Amazonia. The observed variability of carbon
fluxes during these 8 years is correlated with climate-related
(temperature, precipitation, soil water storage from GRACE
satellite) and anthropogenic (fire counts) variables. The
correlations were performed inside the upwind area for each
profiling site. During our study period, the Amazon was a
consistent source of 0.4 ± 0.2 PgC/year on average, extrapolating
to the entire Amazon Basin area of 7.2 million km2. Fire emission
is the main source of carbon to the atmosphere, which is not
compensated by the C removal from old-growth Amazon forest.
Moreover, the drought years of 2010, 2015 and 2016 are playing an
outsized role in the eight-year mean. Removing those years from
the mean, the net source is reduced from 0.4 ± 0.2 PgC/year to 0.2
± 0.2 PgC/year.",
conference-location = "San Francisco, CA",
conference-year = "09-13 dec.",
language = "en",
targetfile = "gatti_amazon.pdf",
urlaccessdate = "01 maio 2024"
}