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Reference spectra to classify Amazon water types
Authors:Felipe de Lucia Lobo  Evlyn Márcia Leão de Moraes Novo  Claudio Clemente Faria Barbosa  Lênio Soares Galvão
Affiliation:1. Divis?o de Sensoriamento Remoto, , Instituto Nacional de Pesquisas Espaciais (INPE) , S?o José dos Campos , SP , 12245-970 , Brazil lobo@dsr.inpe.br;3. Divis?o de Sensoriamento Remoto, , Instituto Nacional de Pesquisas Espaciais (INPE) , S?o José dos Campos , SP , 12245-970 , Brazil;4. Divis?o de Processamento de Imagens, , Instituto Nacional de Pesquisas Espaciais (INPE) , S?o José dos Campos , SP , 12245-970 , Brazil
Abstract:Reference spectra extracted from spectral libraries can distinguish different water types in images when associated with limnological information. In this study, we compiled available databases into a single spectral library, using field water reflectance spectra and limnological data collected by different researchers and campaigns in the Amazonian region. By using an iterative clustering procedure based on the combination of reflectance and optically active components (OACs), reference spectra representative of the major Amazonian water types were defined from this library. Differences between the resultant limnological classes were also evaluated by paired t-tests at significance level 0.05. Finally, reference spectra were tested for Spectral Angle Mapper (SAM) classification of waters in Hyperion/Earth Observing-One (EO-1) and Medium Resolution Imaging Spectrometer (MERIS)/Environment Satellite (Envisat) images acquired simultaneously as the field campaigns. Results showed highly variable concentrations of OACs due to the complexity of the Amazonian aquatic environments. Ten classes were defined to represent this complexity, broadly grouped into four limnological characteristics: clear waters with low concentrations of OACs (class 1); black waters rich in dissolved organic carbon (DOC) (class 2); waters with large concentrations of inorganic suspended solids (ISSs) (classes 3–7); and waters dominated by chlorophyll-a (chl-a) (classes 8–10). Using the ten reference spectra, SAM classification of the field water curves produced an overall accuracy of 86% with the highest values observed for classes 3, 4, 6 and 7 and the lowest accuracy for classes 1 and 2. The results of paired t-tests confirmed the class differences based on the concentrations of OACs. SAM classification of the Hyperion and MERIS images using ground truth information resulted in overall classification accuracies of 48% and 67%, respectively, with the highest errors associated with specific portions of the scenes that were not adequately represented in the spectral library.
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