Quantifying immediate carbon emissions from El Niño-mediated wildfires in humid tropical forests

Author:

Withey Kieran1ORCID,Berenguer Erika12ORCID,Palmeira Alessandro Ferraz3,Espírito-Santo Fernando D. B.4,Lennox Gareth D.1,Silva Camila V. J.1,Aragão Luiz E. O. C.56,Ferreira Joice7,França Filipe178,Malhi Yadvinder2,Rossi Liana Chesini9,Barlow Jos1

Affiliation:

1. Lancaster Environment Centre, Lancaster University, Lancaster LA1 4YQ, UK

2. Environmental Change Institute, University of Oxford, Oxford OX1 3QY, UK

3. Instituto de Ciências Biológicas, Universidade Federal do Pará, Rua Augusto Corrêa, 01, Campus Guamá, Belém, PA CEP: 66075-110, Brazil

4. Centre for Landscape and Climate Research (CLCR) and Leicester Institute of Space and Earth Observation (LISEO), School of Geography, Geology and Environment, University of Leicester, University Road, Leicester LE1 7RH, UK

5. Remote Sensing Division, National Institute for Space Research, Avenida dos Astronautas, 1.758, 12227-010 São José dos Campos, São Paulo, Brazil

6. College of Life and Environmental Sciences, University of Exeter, Exeter EX4 4RJ, UK

7. Embrapa Amazônia Oriental, Travessa Dr Enéas Pinheiro, s/n, CP 48, 66095-100 Belém, Pará, Brazil

8. Instituto Federal de Minas Gerais, Rodovia Bambuí/Medeiros, Km-05, 38900-000 Bambuí, Minas Gerais, Brazil

9. Departamento de Ecologia, Universidade Estadual Paulista, 13506-900 Rio Claro, São Paulo, Brazil

Abstract

Wildfires produce substantial CO 2 emissions in the humid tropics during El Niño-mediated extreme droughts, and these emissions are expected to increase in coming decades. Immediate carbon emissions from uncontrolled wildfires in human-modified tropical forests can be considerable owing to high necromass fuel loads. Yet, data on necromass combustion during wildfires are severely lacking. Here, we evaluated necromass carbon stocks before and after the 2015–2016 El Niño in Amazonian forests distributed along a gradient of prior human disturbance. We then used Landsat-derived burn scars to extrapolate regional immediate wildfire CO 2 emissions during the 2015–2016 El Niño. Before the El Niño, necromass stocks varied significantly with respect to prior disturbance and were largest in undisturbed primary forests (30.2 ± 2.1 Mg ha −1 , mean ± s.e.) and smallest in secondary forests (15.6 ± 3.0 Mg ha −1 ). However, neither prior disturbance nor our proxy of fire intensity (median char height) explained necromass losses due to wildfires. In our 6.5 million hectare (6.5 Mha) study region, almost 1 Mha of primary (disturbed and undisturbed) and 20 000 ha of secondary forest burned during the 2015–2016 El Niño. Covering less than 0.2% of Brazilian Amazonia, these wildfires resulted in expected immediate CO 2 emissions of approximately 30 Tg, three to four times greater than comparable estimates from global fire emissions databases. Uncontrolled understorey wildfires in humid tropical forests during extreme droughts are a large and poorly quantified source of CO 2 emissions. This article is part of a discussion meeting issue ‘The impact of the 2015/2016 El Niño on the terrestrial tropical carbon cycle: patterns, mechanisms and implications’.

Funder

Natural Environment Research Council

Conselho Nacional de Desenvolvimento Científico e Tecnológico

Empresa Brasileira de Pesquisa Agropecuária

Publisher

The Royal Society

Subject

General Agricultural and Biological Sciences,General Biochemistry, Genetics and Molecular Biology

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