2019
DOI: 10.3390/rs11091074
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Contrasting Post-Fire Dynamics between Africa and South America based on MODIS Observations

Abstract: Fire is an important driver of land cover change throughout the world, affecting processes such as deforestation, forest recovery and vegetation transition. Little attention has been given to the role of fire in shaping the temporal and spatial land cover changes among continents. This study has integrated two MODIS products (MCD64A1: Burned area and MCD12Q1: Land cover) over Africa and South America from 2001–2013 to explore the vegetation dynamics after fires. The results indicated that while Africa suffered… Show more

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Cited by 8 publications
(5 citation statements)
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“…This association may indicate that fires are agents of loss (i.e., humans use fire to deforest), a common cause drives more fires and deforestation (e.g., climate change makes wildfires more common and people opportunistically deforest the burnt area), or some combination of both. Previous studies of postfire vegetation dynamics have found most South American forests can be severely affected by single fires and therefore recover only very slowly, requiring up to two decades to grow back ( 35 ). While statistical analyses confirm persistence is frequent enough after a single fire (Fig.…”
Section: Discussionmentioning
confidence: 99%
“…This association may indicate that fires are agents of loss (i.e., humans use fire to deforest), a common cause drives more fires and deforestation (e.g., climate change makes wildfires more common and people opportunistically deforest the burnt area), or some combination of both. Previous studies of postfire vegetation dynamics have found most South American forests can be severely affected by single fires and therefore recover only very slowly, requiring up to two decades to grow back ( 35 ). While statistical analyses confirm persistence is frequent enough after a single fire (Fig.…”
Section: Discussionmentioning
confidence: 99%
“…It did not vary even in periods of extreme drought or periods of higher rainfall, thus attesting to human interference in the environment. According to the classification determined by Oliveira-Júnior et al [32], the SPI values in 2009, 2014, 2016, and 2017 were considered normal. For the positive SPI values, 2013 was a year of high rainfall, and 2019 was a year of severe rainfall.…”
Section: Discussionmentioning
confidence: 99%
“…Dynamic thresholds were then applied to guide the statistical characterization of burn-and non-burn-related changes. Finally, spatial and temporal active fire information was used to create regional probability density functions to classify each pixel as burned or unburned [32].…”
Section: Burned Area Analysismentioning
confidence: 99%
“…The algorithm identifies the date of burn for the 500 m grid cells within each individual MODIS tile. The date is encoded in a single data layer as the ordinal day of the calendar year during which the burn occurred, with values assigned to unburned land pixels and additional special values reserved for missing data and water grid cells [73,74].…”
Section: Burned Areasmentioning
confidence: 99%