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A Look at Amazon Basin Seasonal Dynamics with the Biophysical ...

A Look at Amazon Basin Seasonal Dynamics with the Biophysical ...

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Detecting deforested areas from NDVI series in <strong>Amazon</strong>ia 1982-1999N. Dessay, H. Laurent, L. Machado, J. Ronchail, Y. ShimabukuroCTA /IAE/ ACACentro Técnico Aeroespacial /Instituto de Aeronáutica e Espaço/ Divisão de CiênciasAtmosféricas CEP 12228-904, São José dos Campos, SP, Brasil.andInstitut de Recherche pour le développement/Labor<strong>at</strong>oire d'Etude des Transferts enHydrologie et Environnement, Grenoble, Francendessay@iae.cta.br, hlaurent@iae.cta.br, machado@iae.cta.br,josyane@aneel.gov.br, yosio@ltid.inpe.brThe aim of this work is to localize forest areas th<strong>at</strong> evolved toward a deforest<strong>at</strong>ion or areforest<strong>at</strong>ion using <strong>the</strong> Normalized Difference Veget<strong>at</strong>ion Index (NDVI). We shall pay special<strong>at</strong>tention to 9 areas chosen among <strong>the</strong> LBA study areas. When <strong>the</strong> forest undergoes <strong>at</strong>ransform<strong>at</strong>ion such as deforest<strong>at</strong>ion, <strong>the</strong> NDVI presents a very sharp minimum during <strong>the</strong> dryseason, th<strong>at</strong> we shall use in this work. Firstly, we use <strong>the</strong> areas th<strong>at</strong> have remained steadyduring 18 years as a reference to calibr<strong>at</strong>e <strong>the</strong> NDVI d<strong>at</strong>aset over this period. Secondly, <strong>the</strong>regions of rain forest are geographically distinct because <strong>the</strong> dry season is not <strong>the</strong> same fromone region to <strong>the</strong> o<strong>the</strong>r. To take this into account, we define homogeneous areas using <strong>the</strong>IBGE (Instituto Brasileiro de Geografia e Est<strong>at</strong>ística) veget<strong>at</strong>ion classific<strong>at</strong>ion, <strong>the</strong>precipit<strong>at</strong>ion series th<strong>at</strong> are provided by <strong>the</strong> Agência Nacional de Energia Eléctrica (ANEEL)and <strong>the</strong> Instituto Nacional de Meteorologia (INMET) and <strong>the</strong> high level cloud cover availablefrom <strong>the</strong> Intern<strong>at</strong>ional S<strong>at</strong>ellite Cloud Clim<strong>at</strong>ology Project (ISCCP). Then we define referencedry season NDVI by averaging <strong>the</strong> NDVI minimum in different areas th<strong>at</strong> are known as nothaving suffered deforest<strong>at</strong>ion. Afterwards, we compare <strong>the</strong> d<strong>at</strong>e and amplitude of <strong>the</strong> NDVIminimum for 9 LBA target areas <strong>with</strong> th<strong>at</strong> of <strong>the</strong> nearest reference area. We observe in somecases large differences th<strong>at</strong> permit to analyze <strong>the</strong> deforest<strong>at</strong>ion or <strong>the</strong> reforest<strong>at</strong>ion. Thisapproach gives both a sp<strong>at</strong>ial and a temporal vision of <strong>the</strong> evolution of <strong>the</strong> forest.

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