Full text: Technical Commission VIII (B8)

International Archives of the Photogrammetry, Remote Sensing and Spatial Information Sciences, Volume XXXIX-B8, 2012 
XXII ISPRS Congress, 25 August — 01 September 2012, Melbourne, Australia 
GLOBAL BURNED AREA MAPPING FROM EUROPEAN SATELLITES: THE ESA 
FIRE CCI PROJECT 
E. Chuvieco®, Christopher Sandow?, K. P. Guenther', F. González-Alonso!, J.M. Pereira‘, O. Perez“, A.V. Bradley®, M. Schultz”, F. 
Mouillot' and P. Ciais! 
*Departamento de Geografía, Universidad de Alcalá. Colegios, 2. 28801 Alcalá de Henares, Spain. 
emilio.chuvieco@uah.es 
PGAF AG, Arnulfstr. 197, 80634 Munich, Germany. christopher.sandow@gaf.de 
German Aerospace Center (DLR), German Remote Sensing Data Center (DFD), 82234 Oberpfaffenhofen, Germany. 
Kurt.Guenther@dlr.de 
‘Centro de Investigacion Forestal (CIFOR). INIA. Crta. Km7 28040. Madrid. Spain. alonso@inia.es 
“Instituto Superior de Agronomia, Universidade Técnica de Lisboa, Tapada da Ajuda, 1349-017 Lisboa, Portugal. 
f{GMV AEROSPACE AND DEFENCE, S.A., Isaac Newton, 11, E-28760 Madrid (Spain). operez@gmv.com 
Department of Geography, University of Leicester, University Road LE1 7RH. UK. avb4@leicester.ac.uk 
"Forschungszentrum Juelich GmbH, 52425 Juelich, Germany. m.schultz@fz-juelich.de 
. TRD,1919 Route de Mend, 34293 Montpellier Cedex 5, France. mouillot@cefe.cnrs.fr 
JIPSL — LSCE,CEA CNRS UVSQ, 91191 Gif sur Yvette France. philippe.ciais@lsce.ipsi.fr 
KEY WORDS: Burned Area, Climate Change, MERIS, ATSR, VEGETATION, European Space Agency 
ABSTRACT: 
The European Space Agency (ESA) Climate Change Initiative (CCI) is part of the European contribution to the Global Climate 
Observing System (GCOS) program. Fire disturbance is one of the Essential Climate Variables (ECV) included in the ESA CCI 
program. It focus on mapping burned area (BA) using European sensors (ATSR, VEGETATION and MERIS data), and in 
comparing the performance of the results with other existing datasets. The project aims at developing and validating algorithms to 
produce consistent, stable, error-characterized global BA information. The project includes as well developing algorithms to generate 
georeferenced and calibrated reflectances of (A)ATSR, VEGETATION and MERIS data, identifying potential sources of confusion 
with burned areas (clouds, smoke, cloud shadows, water, snow, topographic shadows). The final product will be a merging of BA 
information derived from three different sensors . 
modelling communities. 
1. INTRODUCTION 
The European Space Agency (ESA) Climate Change Initiative 
(CCI) is part of the European contribution to the Global Climate 
Observing System (GCOS) program. In particular, the objective 
of this initiative is producing consistent and accurate time series 
of Essential Climate Variables (ECV), which can be used by 
climate, atmospheric and ecosystem scientists for their 
modeling efforts (Plummer, 2009). The CCI stresses the 
importance of improving scientific impact of data acquired by 
ESA sensors, while maintain close links with key science 
bodies and other agencies currently generating ECV data. The 
first call of the CCI program includes ten ECVs covering 
atmospheric products (ozone, greenhouse gasses, aerosols, 
clouds), oceanic variables (ocean colour, sea ice, height and 
temperature), and terrestrial (fire, glaciers, and land cover). 
Biomass burning is widely recognized as one of the critical 
factors affecting vegetation succession and carbon budgets 
worldwide (Chuvieco, 2008; Thonicke et al., 2010). At regional 
and local scale, fires have also important socio-economic 
implications, both affecting lives and structures (Chuvieco et 
al., 2010). 
At a global scale, the effects of fire on the atmospheric 
chemistry are one of the most complex factors to account for in 
the current emission models, although recent studies estimate 
that biomass burning is responsible for half (3-4 Pg C) of the 
CO2 released by fossil fuels consumption (Bowman et al., 
2009; van der Werf et al., 2010). The available estimations are 
based on bottom-up approaches, which try to account for the 
different factors of fire-related emissions. They require accurate 
mapping of pre-fire biomass, of burned areas and of the amount 
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The outputs will be adapted to the needs of the atmospheric and vegetation 
of biomass that has been actually consumed by the fire (Seiler 
and Crutzen, 1980). The generation of these variables still 
presents high uncertainty, and therefore the estimations have a 
wide range of variability (van der Werf et al., 2010). The actual 
area affected by fires worldwide is not yet accurately known. 
The most recent studies based on multitemporal series of 
MODIS data estimate that an average area of 3.5 million km2 is 
burned every year (Giglio et al., 2010; Tansey et al, 2008), 
mostly in the Tropical savannas, temperate grasslands and 
boreal forests. Other impacts of fire on the global climate are 
still poorly understood, such as the direct and indirect role of 
aerosols, their impact on land use change and surface albedo, 
the relation with tropospheric ozone and the deposition of black 
carbon on soils (Bowman et al., 2009). 
The fire cci project aims to improve mapping of burned areas 
(BA) and the use of BA information in global vegetation and 
atmospheric models. The BA maps will be generated from 
European sensors: (A)ATSR, VEGETATION and MERIS data, 
trying to meet the GCOS ECV requirements (Global Climate 
Observing System (GCOS), 2009), which require consistent, 
stable, error-characterized global satellite data products from 
multi-sensor data archives. A synthetic estimation based on the 
three sensors will be produced for the temporal series of 1995 to 
2009 for several study sites, as well as for five years of global 
coverage. The project will dedicate considerable effort to 
validate the products and interact with modellers. From a 
conceptual point of view, the project tries to answer the 
following scientific questions: What is the actual magnitude of 
fire impacts? How much area is burned annually worldwide?, 
What are the recent trends in fire activity? These questions are 
the basis for other aspects of global fire science, such as the 
 
	        
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