Current and future patterns of fire-induced forest degradation in Amazonia
Amazon droughts directly increase forest flammability by reducing forest understory air and fuel moisture. Droughts also increase forest flammability indirectly by decreasing soil moisture, triggering leaf shedding, branch loss, and tree mortality—all of which contribute to increased fuel loads. The...
| Autores: | , , , , , |
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| Tipo de recurso: | artículo |
| Estado: | Versión publicada |
| Fecha de publicación: | 2017 |
| País: | Brasil |
| Institución: | Universidade Federal de Minas Gerais (UFMG) |
| Repositorio: | Repositório Institucional da UFMG |
| Idioma: | inglés |
| OAI Identifier: | oai:repositorio.ufmg.br:1843/52116 |
| Acceso en línea: | https://doi.org/10.1088/1748-9326/aa69ce http://hdl.handle.net/1843/52116 https://orcid.org/0000-0002-8560-0034 https://orcid.org/0000-0001-8952-7025 https://orcid.org/0000-0002-1287-2004 https://orcid.org/0000-0002-7703-946X https://orcid.org/0000-0002-7470-0697 |
| Access Level: | acceso abierto |
| Palabra clave: | Amazon Climate change Drought Fire intensity Fire severity CMIP5 Fire modeling Amazônia Mudanças climáticas Mudanças climáticas - Amazônia Secas Queimada |
| Sumario: | Amazon droughts directly increase forest flammability by reducing forest understory air and fuel moisture. Droughts also increase forest flammability indirectly by decreasing soil moisture, triggering leaf shedding, branch loss, and tree mortality—all of which contribute to increased fuel loads. These direct and indirect effects can cause widespread forest fires that reduce forest carbon stocks in the Amazon, with potentially important consequences for the global carbon cycle. These processes are expected to become more widespread, common, and intense as global climate changes, yet the mechanisms linking droughts, wildfires, and associated changes in carbon stocks remain poorly understood. Here, we expanded the capabilities of a dynamic forest carbon model to better represent (1) drought effects on carbon and fuel dynamics and (2) understory fire behavior and severity. We used the refined model to quantify changes in PanAmazon live carbon stocks as a function of the maximum climatological water deficit (MCWD) and fire intensity, under both historical and future climate conditions. We found that the 2005 and 2010 droughts increased potential fire intensity by 226 kW m1 and 494 kW m1 , respectively. These increases were due primarily to increased understory dryness (109 kW m1 in 2005; 124 kW m1 in 2010) and altered forest structure (117 kW m1 in 2005; 370 kW m1 in 2010) effects. Combined, these historic droughts drove total simulated reductions in live carbon stocks of 0.016 (2005) and 0.027 (2010) PgC across the Amazon Basin. Projected increases in future fire intensity increased simulated carbon losses by up to 90% per unit area burned, compared with modern climate. Increased air temperature was the primary driver of changes in simulated future fire intensity, while reduced precipitation was secondary, particularly in the eastern portion of the Basin. Our results show that fire-drought interactions strongly affect live carbon stocks and that future climate change, combined with the synergistic effects of drought on forest flammability, may strongly influence the stability of tropical forests in the future. |
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