2016
DOI: 10.1080/17538947.2016.1208686
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Multi-year MODIS active fire type classification over the Brazilian Tropical Moist Forest Biome

Abstract: The Brazilian Tropical Moist Forest Biome (BTMFB) spans almost 4 million km 2 and is subject to extensive annual fires that have been categorized into deforestation, maintenance, and forest fire types. Information on fire types is important as they have different atmospheric emissions and ecological impacts. A supervised classification methodology is presented to classify the fire type of MODerate resolution Imaging Spectroradiometer (MODIS) active fire detections using training data defined by consideration o… Show more

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Cited by 35 publications
(19 citation statements)
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References 128 publications
(171 reference statements)
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“…This variable is retrieved from the radiance at the 4-μm band of satellite sensors and represents the instantaneous radiative energy that is released from actively burning fires. FRP has been extensively used as a proxy of fire intensity to characterize fire types (Roy & Kumar, 2017;Wooster & Zhang, 2004), fire behaviors (Smith & Wooster, 2005), and fire regimes (Archibald et al, 2013), to predict fire danger (Freeborn et al, 2016), and to investigate interactions among biomass burning, land cover dynamics, and hydrological cycles (Ichoku et al, 2016). More importantly, FRP is related to the rate of biomass combustion (Kaufman et al, 1998;Wooster et al, 2003) and the rate of emissions (Ichoku & Kaufman, 2005), which have been subsequently applied to estimate trace gas and aerosol emissions (Kaiser et al, 2012;Kumar et al, 2011;Vermote et al, 2009;Zhang et al, 2012).…”
Section: Introductionmentioning
confidence: 99%
“…This variable is retrieved from the radiance at the 4-μm band of satellite sensors and represents the instantaneous radiative energy that is released from actively burning fires. FRP has been extensively used as a proxy of fire intensity to characterize fire types (Roy & Kumar, 2017;Wooster & Zhang, 2004), fire behaviors (Smith & Wooster, 2005), and fire regimes (Archibald et al, 2013), to predict fire danger (Freeborn et al, 2016), and to investigate interactions among biomass burning, land cover dynamics, and hydrological cycles (Ichoku et al, 2016). More importantly, FRP is related to the rate of biomass combustion (Kaufman et al, 1998;Wooster et al, 2003) and the rate of emissions (Ichoku & Kaufman, 2005), which have been subsequently applied to estimate trace gas and aerosol emissions (Kaiser et al, 2012;Kumar et al, 2011;Vermote et al, 2009;Zhang et al, 2012).…”
Section: Introductionmentioning
confidence: 99%
“…Fires in the region can be broadly classified as maintenance, deforestation and forest fires with different temporal patterns related to climate conditions, but in some cases they are related to the ignition cause; i.e. maintenance fires in Brazil are lit every 2-4 years (Roy and Kumar, 2017) Fire occurrence in the tropics has a particular pattern: in Latin America it has been established that north of the equator the fire season is between December and February while in the south it is between May and July (Chuvieco et al, 2008). However, unusual fire events have been occurring more frequently and more intensely in the Amazon Basin and are associated with extreme climatic events such as the El Niño Southern Oscillation (ENSO) (Aragão et al, 2007;Ray et al, 2005) or the warm tropical North Atlantic Oscillation (NAO) (Marengo et al, 2008a;Phillips et al, 2009) as well as to the occurrence of extreme drought years (Asner and Alencar, 2010;Brown et al, 2006;Lewis et al, 2011;Malhi et al, 2009;Marengo et al, 2008b).…”
Section: Introductionmentioning
confidence: 99%
“…Fire dynamics is strongly influenced by climate, and indeed the dry season (∼ July-September) in the southern Amazonia corresponded to a wet season in northern Amazonia, and this is well established. For example, 2004For example, /2005For example, , 2006For example, /2007For example, and 2009For example, /2010 were El Niño years, affecting the dry season in the Northern Hemisphere, while increased Atlantic sea surface temperatures (SST) in the Atlantic Ocean were responsible for the 2005 and 2010 droughts during the dry season in the Southern Hemisphere (Phillips et al, 2009;Saatchi et al, 2013).…”
Section: Discussionmentioning
confidence: 99%