@Article{LibonatiCamaPerePere:2010:ReMiRe,
author = "Libonati, Renata and Camara, Carlos C. and Pereira, Jose Miguel
and Peres, Leonardo",
affiliation = "{Instituto Nacional de Pesquisas Espaciais (INPE)} and University
of Lisbon, IDL/CGUL, Lisbon, Portugal and School of Agronomy,
Technical University of Lisbon, Lisbon, Portugal and {Instituto
Nacional de Pesquisas Espaciais (INPE)}",
title = "Retrieving middle-infrared reflectance for burned area mapping in
tropical environments using MODIS",
journal = "Remote Sensing of Environment",
year = "2010",
volume = "114",
number = "4",
pages = "831--843",
month = "Apr.",
note = "{} and b School of Agronomy, Technical University of Lisbon,
Lisbon, Portugal and c Center for Weather Forecast and Climate
Studies, Brazilian National Institute for Space Research,
Cachoeira Paulista, Brazil",
keywords = "land surface, emissivity, radiation, aerosol.",
abstract = "The ephemeral character of the radiative signal together with the
presence of aerosols imposes severe limitations on the use of
classical approaches, e.g. based on red and near-infrared, to
discriminate between burned and unburned surfaces in tropical
environments. Surface reflectance in the middle-infrared (MIR) has
been used to circumvent these difficulties because the signal is
virtually unaffected by the presence of aerosols associated to
biomass burning. Retrieval of the MIR reflected component from the
total signal is, however, a difficult problem because of the
presence of a diversity of radiance sources, namely the surface
reflected solar irradiance and the surface emitted radiance that
may reach comparable magnitude during daytime. The method proposed
by Kaufman and Remer (1994) to retrieve surface MIR reflectance
presents the advantage of not requiring auxiliary datasets (e.g.
atmospheric profiles) nor major computational means (e.g. for
solving radiative transfer models). Nevertheless, the method was
specifically designed to retrieve MIR reflectance over dense dark
forests in the middle latitudes and, as shown in the present
study, severe problems may arise when applying it beyond the range
of validity, namely for burned area mapping in tropical
environments. The present study consists of an assessment of the
performance of the method for a wide range of atmospheric,
geometric and surface conditions and of the usefulness of
extracted surface reflectances for burned area discrimination.
Results show that, in the case of tropical environments, there is
a significant decrease in performance of the method for high
values of land surface temperature, especially when associated
with low sun elevation angles. Burned area discrimination is
virtually impaired in such conditions, which are often present
when using data from instruments on-board polar orbiters, namely
MODIS in Aqua and Terra, to map burned surfaces over the Amazon
forest and {"}cerrado{"} savanna regions. (C) 2009 Elsevier Inc.
All rights reserved.",
doi = "10.1016/j.rse.2009.11.018",
url = "http://dx.doi.org/10.1016/j.rse.2009.11.018",
issn = "0034-4257",
language = "en",
targetfile = "peres 2010.pdf",
urlaccessdate = "03 maio 2024"
}