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Global burned area and biomass burning emissions from small fires

Authors :
Randerson, J. T
Randerson, J. T
Chen, Y.
van der Werf, G. R
Rogers, B. M
Morton, D. C
Randerson, J. T
Randerson, J. T
Chen, Y.
van der Werf, G. R
Rogers, B. M
Morton, D. C
Source :
Journal of Geophysical Research; vol 117, iss G4; 0148-0227
Publication Year :
2012

Abstract

In several biomes, including croplands, wooded savannas, and tropical forests, many small fires occur each year that are well below the detection limit of the current generation of global burned area products derived from moderate resolution surface reflectance imagery. Although these fires often generate thermal anomalies that can be detected by satellites, their contributions to burned area and carbon fluxes have not been systematically quantified across different regions and continents. Here we developed a preliminary method for combining 1-km thermal anomalies (active fires) and 500 m burned area observations from the Moderate Resolution Imaging Spectroradiometer (MODIS) to estimate the influence of these fires. In our approach, we calculated the number of active fires inside and outside of 500 m burn scars derived from reflectance data. We estimated small fire burned area by computing the difference normalized burn ratio (dNBR) for these two sets of active fires and then combining these observations with other information. In a final step, we used the Global Fire Emissions Database version 3 (GFED3) biogeochemical model to estimate the impact of these fires on biomass burning emissions. We found that the spatial distribution of active fires and 500 m burned areas were in close agreement in ecosystems that experience large fires, including savannas across southern Africa and Australia and boreal forests in North America and Eurasia. In other areas, however, we observed many active fires outside of burned area perimeters. Fire radiative power was lower for this class of active fires. Small fires substantially increased burned area in several continental-scale regions, including Equatorial Asia (157%), Central America (143%), and Southeast Asia (90%) during 2001–2010. Globally, accounting for small fires increased total burned area by approximately by 35%, from 345 Mha/yr to 464 Mha/yr. A formal quantification of uncertainties was not possible, but sensitivity ana

Details

Database :
OAIster
Journal :
Journal of Geophysical Research; vol 117, iss G4; 0148-0227
Notes :
application/pdf, Journal of Geophysical Research vol 117, iss G4 0148-0227
Publication Type :
Electronic Resource
Accession number :
edsoai.on1287542182
Document Type :
Electronic Resource