Understanding the Temporal Dynamics of Carbon Emission from Fires in the Amazon-Cerrado Transition Zone

Autores/as

  • Henrique Luis Godinho Cassol Remote Sensing Division, National Institute for Space Research (INPE), São José dos Campos, Brazil
  • Lucas Domingues Gatti Earth System Science Center (CCST), National Institute for Space Research (INPE), São José dos Campos, SP, Brazil
  • Luana Santamaria Basso Earth System Science Center (CCST), National Institute for Space Research (INPE), São José dos Campos, SP, Brazil
  • Luciana Vanni Gatti Earth System Science Center (CCST), National Institute for Space Research (INPE), São José dos Campos, SP, Brazil
  • Luciano Marani Earth System Science Center (CCST), National Institute for Space Research (INPE), São José dos Campos, SP, Brazil
  • Graciela Pinelli Tejada Earth System Science Center (CCST), National Institute for Space Research (INPE), São José dos Campos, SP, Brazil
  • Egidio Arai Remote Sensing Division, National Institute for Space Research (INPE), São José dos Campos, Brazil
  • John B Miller Global Monitoring Division, Earth System Research Laboratory, National Oceanic and Atmospheric Administration (NOAA), Boulder, Colorado 80305, USA.Global Monitoring Division, Earth System Research Laboratory, National Oceanic and Atmospheric Administration (NOAA), Boulder, Colorado 80305, USA.
  • Liana O Anderson National Center for Monitoring and Early Warning of Natural Disasters - CEMADEN, São José dos Campos, SP, Brazil
  • Luiz Eduardo Oliveira Cruz Aragão Remote Sensing Division, National Institute for Space Research (INPE), São José dos Campos, Brazil

DOI:

https://doi.org/10.37002/biodiversidadebrasileira.v9i1.1273

Palabras clave:

Climate change, fire emission, Amazon, Hysplit, rainforest, Cerrado

Resumen

Carbon emissions from fires (C fire) account for one-tenth of the global annual C
emissions. Fires are the main source of emissions from land-use change. Recently, Werf et al.
2017, showed an 11% increase in global fire emissions during the 1997-2016 period. Savannas
and Tropical Forests have shared almost the same fire-derived C emission values in the South
America (Werf et al. 2017). Therefore, for this study we focused our analysis on a site
representing the transition zone between Amazonia and Cerrado, located in Alta Floresta (ALF)
in Mato Grosso State, Brazil. To understand the temporal dynamics of fire-derived C emission,
we correlated fire counts (FC) within the influence area with fire-derived C emission directly
measured in the atmosphere as CO concentration. CO and CO2 were collected monthly for 7
years from 2010 onwards using an aircraft flying up to 4.5 km altitude, totaling 153 vertical profiles.
FC was extracted from influence areas weighted by the density of backward trajectories
calculated quarterly. Trajectories starting from the flight location within a cell of one degree
resolution were obtained using the Hysplit model at different heights. The average annual C
emission from fire was 0.10 ± 0.04 Pg.C.yr-1, which represents about 10% of the Amazon fire
emissions (Aragão et al. 2018). The highest daily value of fire emission was observed in 2010
(drought year) and 2017 (0.47-0.51 gC.m².day-1), although the years of 2011, 2016, and 2017
were the largest contributor to the total emission flux. This occurred because the influence area
that belongs to the Amazon was lower in those years. Inter annually there is a typical behavior of
the backward trajectories in ALF site whose 1st and 4th quarters have 80% of the air-streams
coming from the Amazon, while during the 2nd and 3rd quarters this contribution is about 45%.
However, emissions from fire and FC are higher in the 3rd quarter, outside the Amazon. The
correlation between FC and fire emission was positively significant (ρ = 0.88, α = 0.05, p<0.001),
meaning that an increase of 1,000 FC per quarter causes an increase of 0.074 gC.m².day-1 or, on
average, an emission of 0.16 Pg.C.yr-1

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Publicado

2019-05-15