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Assessing the feasibility of a global model for multi-temporal burned area mapping using SPOT-VEGETATION data
Authors:J. M. N. Silva  J. F. C. L. Cadima  J. M. C. Pereira  J.-M. Grégoire
Affiliation:1. Department of Forestry , Instituto Superior de Agronomia , Lisboa, 1349-017, Portugal Phone: +351 21 3653387 +351 21 3645000 E-mail: joaosilva@isa.utl.pt;2. Department of Mathematics , Instituto Superior de Agronomia , Lisboa, 1349-017, Portugal Phone: +351 21 3653317 +351 21 3630723 E-mail: jcadima@isa.utl.pt;3. Department of Forestry , Instituto Superior de Agronomia , Lisboa, 1349-017, Portugal Phone: +351 21 3653387 +351 21 3645000 E-mail: jmcpereira@isa.utl.pt;4. Joint Research Centre of the European Commission , Institute for Environment and Sustainability , I-21020, Ispra, TP 440 , VA, Italy Phone: +39 0332 789215 +39 0332 789073 E-mail: jean-marie.gregoire@jrc.it
Abstract:The possibility of using the Syst@me Probatoire de l'Observation de la Terre (SPOT)-VEGETATION (VGT) data for global burned area mapping with a single algorithm was investigated. Using VGT images from south-eastern Africa, the Iberian Peninsula and south-eastern Siberia/north-eastern China, we analysed the variability of the spectral signature of burned areas and its relationship with land cover, and performed the selection of the best variables for burned area mapping. The results show that in grasslands and croplands, near-infrared (NIR) and short-wave infrared (SWIR) reflectance always decreases as a result of fire. In forests and woodlands, there may occur a simultaneous decrease of SWIR and NIR or an increase of SWIR and a decrease of NIR. Burning of green vegetation (high values of the Normalized Difference Vegetation Index (NDVI)) tends to result in an increase of the SWIR. The best variables for burned area mapping are different in each region. Only the NIR allows a good discrimination of burned areas in all study areas. We derived a logistic regression model for multi-temporal burned area mapping in tropical, temperate and boreal regions, which handles the spectral variability of burned areas dependent on the type of vegetation. The results underline the feasibility of a single model for global burned area mapping.
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