Author
Listed:
- Luciana V. Gatti
(National Institute for Space Research (INPE)
Nuclear and Energy Research Institute (IPEN))
- Luana S. Basso
(National Institute for Space Research (INPE))
- John B. Miller
(Global Monitoring Laboratory, National Oceanic and Atmospheric Administration (NOAA))
- Manuel Gloor
(University of Leeds)
- Lucas Gatti Domingues
(National Institute for Space Research (INPE)
Nuclear and Energy Research Institute (IPEN)
GNS Science)
- Henrique L. G. Cassol
(National Institute for Space Research (INPE))
- Graciela Tejada
(National Institute for Space Research (INPE))
- Luiz E. O. C. Aragão
(National Institute for Space Research (INPE)
University of Exeter)
- Carlos Nobre
(University of São Paulo (USP))
- Wouter Peters
(Wageningen University
University of Groningen)
- Luciano Marani
(National Institute for Space Research (INPE))
- Egidio Arai
(National Institute for Space Research (INPE))
- Alber H. Sanches
(National Institute for Space Research (INPE))
- Sergio M. Corrêa
(National Institute for Space Research (INPE)
Rio de Janeiro State University (UERJ))
- Liana Anderson
(National Center for Monitoring and Early Warning of Natural Disasters (CEMADEN))
- Celso Randow
(National Institute for Space Research (INPE))
- Caio S. C. Correia
(National Institute for Space Research (INPE)
Nuclear and Energy Research Institute (IPEN))
- Stephane P. Crispim
(National Institute for Space Research (INPE))
- Raiane A. L. Neves
(National Institute for Space Research (INPE))
Abstract
Amazonia hosts the Earth’s largest tropical forests and has been shown to be an important carbon sink over recent decades1–3. This carbon sink seems to be in decline, however, as a result of factors such as deforestation and climate change1–3. Here we investigate Amazonia’s carbon budget and the main drivers responsible for its change into a carbon source. We performed 590 aircraft vertical profiling measurements of lower-tropospheric concentrations of carbon dioxide and carbon monoxide at four sites in Amazonia from 2010 to 20184. We find that total carbon emissions are greater in eastern Amazonia than in the western part, mostly as a result of spatial differences in carbon-monoxide-derived fire emissions. Southeastern Amazonia, in particular, acts as a net carbon source (total carbon flux minus fire emissions) to the atmosphere. Over the past 40 years, eastern Amazonia has been subjected to more deforestation, warming and moisture stress than the western part, especially during the dry season, with the southeast experiencing the strongest trends5–9. We explore the effect of climate change and deforestation trends on carbon emissions at our study sites, and find that the intensification of the dry season and an increase in deforestation seem to promote ecosystem stress, increase in fire occurrence, and higher carbon emissions in the eastern Amazon. This is in line with recent studies that indicate an increase in tree mortality and a reduction in photosynthesis as a result of climatic changes across Amazonia1,10.
Suggested Citation
Luciana V. Gatti & Luana S. Basso & John B. Miller & Manuel Gloor & Lucas Gatti Domingues & Henrique L. G. Cassol & Graciela Tejada & Luiz E. O. C. Aragão & Carlos Nobre & Wouter Peters & Luciano Mara, 2021.
"Amazonia as a carbon source linked to deforestation and climate change,"
Nature, Nature, vol. 595(7867), pages 388-393, July.
Handle:
RePEc:nat:nature:v:595:y:2021:i:7867:d:10.1038_s41586-021-03629-6
DOI: 10.1038/s41586-021-03629-6
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