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Interactions between rainfall, deforestation and fires during recent years in the Brazilian Amazonia

Understanding the interplay between climate and land-use dynamics is a fundamental concern for assessing the vulnerability of Amazonia to climate change. In this study, we analyse satellite-derived monthly and annual time series of rainfall, fires and deforestation to explicitly quantify the seasona...

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Autores principales: Aragão, Luiz Eduardo O.C, Malhi, Yadvinder, Barbier, Nicolas, Lima, Andre, Shimabukuro, Yosio, Anderson, Liana, Saatchi, Sassan
Formato: Texto
Lenguaje:English
Publicado: The Royal Society 2008
Materias:
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC2373892/
https://www.ncbi.nlm.nih.gov/pubmed/18267907
http://dx.doi.org/10.1098/rstb.2007.0026
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author Aragão, Luiz Eduardo O.C
Malhi, Yadvinder
Barbier, Nicolas
Lima, Andre
Shimabukuro, Yosio
Anderson, Liana
Saatchi, Sassan
author_facet Aragão, Luiz Eduardo O.C
Malhi, Yadvinder
Barbier, Nicolas
Lima, Andre
Shimabukuro, Yosio
Anderson, Liana
Saatchi, Sassan
author_sort Aragão, Luiz Eduardo O.C
collection PubMed
description Understanding the interplay between climate and land-use dynamics is a fundamental concern for assessing the vulnerability of Amazonia to climate change. In this study, we analyse satellite-derived monthly and annual time series of rainfall, fires and deforestation to explicitly quantify the seasonal patterns and relationships between these three variables, with a particular focus on the Amazonian drought of 2005. Our results demonstrate a marked seasonality with one peak per year for all variables analysed, except deforestation. For the annual cycle, we found correlations above 90% with a time lag between variables. Deforestation and fires reach the highest values three and six months, respectively, after the peak of the rainy season. The cumulative number of hot pixels was linearly related to the size of the area deforested annually from 1998 to 2004 (r(2)=0.84, p=0.004). During the 2005 drought, the number of hot pixels increased 43% in relation to the expected value for a similar deforested area (approx. 19 000 km(2)). We demonstrated that anthropogenic forcing, such as land-use change, is decisive in determining the seasonality and annual patterns of fire occurrence. Moreover, droughts can significantly increase the number of fires in the region even with decreased deforestation rates. We may expect that the ongoing deforestation, currently based on slash and burn procedures, and the use of fires for land management in Amazonia will intensify the impact of droughts associated with natural climate variability or human-induced climate change and, therefore, a large area of forest edge will be under increased risk of fires.
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spelling pubmed-23738922008-05-09 Interactions between rainfall, deforestation and fires during recent years in the Brazilian Amazonia Aragão, Luiz Eduardo O.C Malhi, Yadvinder Barbier, Nicolas Lima, Andre Shimabukuro, Yosio Anderson, Liana Saatchi, Sassan Philos Trans R Soc Lond B Biol Sci Research Article Understanding the interplay between climate and land-use dynamics is a fundamental concern for assessing the vulnerability of Amazonia to climate change. In this study, we analyse satellite-derived monthly and annual time series of rainfall, fires and deforestation to explicitly quantify the seasonal patterns and relationships between these three variables, with a particular focus on the Amazonian drought of 2005. Our results demonstrate a marked seasonality with one peak per year for all variables analysed, except deforestation. For the annual cycle, we found correlations above 90% with a time lag between variables. Deforestation and fires reach the highest values three and six months, respectively, after the peak of the rainy season. The cumulative number of hot pixels was linearly related to the size of the area deforested annually from 1998 to 2004 (r(2)=0.84, p=0.004). During the 2005 drought, the number of hot pixels increased 43% in relation to the expected value for a similar deforested area (approx. 19 000 km(2)). We demonstrated that anthropogenic forcing, such as land-use change, is decisive in determining the seasonality and annual patterns of fire occurrence. Moreover, droughts can significantly increase the number of fires in the region even with decreased deforestation rates. We may expect that the ongoing deforestation, currently based on slash and burn procedures, and the use of fires for land management in Amazonia will intensify the impact of droughts associated with natural climate variability or human-induced climate change and, therefore, a large area of forest edge will be under increased risk of fires. The Royal Society 2008-02-11 2008-05-27 /pmc/articles/PMC2373892/ /pubmed/18267907 http://dx.doi.org/10.1098/rstb.2007.0026 Text en Copyright © 2008 The Royal Society http://creativecommons.org/licenses/by/2.5/ This is an open-access article distributed under the terms of the Creative Commons Attribution License, which permits unrestricted use, distribution, and reproduction in any medium, provided the original work is properly cited.
spellingShingle Research Article
Aragão, Luiz Eduardo O.C
Malhi, Yadvinder
Barbier, Nicolas
Lima, Andre
Shimabukuro, Yosio
Anderson, Liana
Saatchi, Sassan
Interactions between rainfall, deforestation and fires during recent years in the Brazilian Amazonia
title Interactions between rainfall, deforestation and fires during recent years in the Brazilian Amazonia
title_full Interactions between rainfall, deforestation and fires during recent years in the Brazilian Amazonia
title_fullStr Interactions between rainfall, deforestation and fires during recent years in the Brazilian Amazonia
title_full_unstemmed Interactions between rainfall, deforestation and fires during recent years in the Brazilian Amazonia
title_short Interactions between rainfall, deforestation and fires during recent years in the Brazilian Amazonia
title_sort interactions between rainfall, deforestation and fires during recent years in the brazilian amazonia
topic Research Article
url https://www.ncbi.nlm.nih.gov/pmc/articles/PMC2373892/
https://www.ncbi.nlm.nih.gov/pubmed/18267907
http://dx.doi.org/10.1098/rstb.2007.0026
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