@Article{MacielNoCaBaFlLo:2019:MuAp,
author = "Maciel, Daniel Andrade and Novo, Evlyn M{\'a}rcia Le{\~a}o de
Moraes and Carvalho, Lino Augusto Sander de and Barbosa,
Cl{\'a}udio Clemente Faria and Flores J{\'u}nior, Rog{\'e}rio
and Lobo, Felipe de Lucia",
affiliation = "{Instituto Nacional de Pesquisas Espaciais (INPE)} and {Instituto
Nacional de Pesquisas Espaciais (INPE)} and {Universidade Federal
do Rio de Janeiro (UFRJ)} and {Instituto Nacional de Pesquisas
Espaciais (INPE)} and {Instituto Nacional de Pesquisas Espaciais
(INPE)} and {Instituto Nacional de Pesquisas Espaciais (INPE)}",
title = "Retrieving total and inorganic suspended sediments in Amazon
floodplain lakes: a multisensor approach",
journal = "Remote Sensing",
year = "2019",
volume = "11",
number = "15",
pages = "e1744",
month = "Aug.",
keywords = "suspended sediments, Amazon Floodplains, Optically Complex Waters,
Monte Carlo Simulation, inorganic sediments.",
abstract = "Remote sensing imagery are fundamental to increasing the knowledge
about sediment dynamics in the middle-lower Amazon floodplains.
Moreover, they can help to understand both how climate change and
how land use and land cover changes impact the sediment exchange
between the Amazon River and floodplain lakes in this important
and complex ecosystem. This study investigates the suitability of
Landsat-8 and Sentinel-2 spectral characteristics in retrieving
total (TSS) and inorganic (TSI) suspended sediments on a set of
Amazon floodplain lakes in the middle-lower Amazon basin using in
situ Remote Sensing Reflectance (Rrs) measurements to simulate
Landsat 8/OLI (Operational Land Imager) and Sentinel 2/MSI
(Multispectral Instrument) bands and to calibrate/validate several
TSS and TSI empirical algorithms. The calibration was based on the
Monte Carlo Simulation carried out for the following datasets: (1)
All-Dataset, consisting of all the data acquired during four field
campaigns at five lakes spread over the lower Amazon floodplain (n
= 94); (2) Campaign-Dataset including samples acquired in a
specific hydrograph phase (season) in all lakes. As sample size
varied from one season to the other, n varied from 18 to 31; (3)
Lake-Dataset including samples acquired in all seasons at a given
lake with n also varying from 17 to 67 for each lake. The
calibrated models were, then, applied to OLI and MSI scenes
acquired in August 2017. The performance of three atmospheric
correction algorithms was also assessed for both OLI (6S, ACOLITE,
and L8SR) and MSI (6S, ACOLITE, and Sen2Cor) images. The impact of
glint correction on atmosphere-corrected image performance was
assessed against in situ glint-corrected Rrs measurements. After
glint correction, the L8SR and 6S atmospheric correction performed
better with the OLI and MSI sensors, respectively (Mean Absolute
Percentage Error (MAPE) = 16.68% and 14.38%) considering the
entire set of bands. However, for a given single band, different
methods have different performances. The validated TSI and TSS
satellite estimates showed that both in situ TSI and TSS
algorithms provided reliable estimates, having the best results
for the green OLI band (561 nm) and MSI red-edge band (705 nm)
(MAPE < 21%). Moreover, the findings indicate that the OLI and MSI
models provided similar errors, which support the use of both
sensors as a virtual constellation for the TSS and TSI estimate
over an Amazon floodplain. These results demonstrate the
applicability of the calibration/validation techniques developed
for the empirical modeling of suspended sediments in lower Amazon
floodplain lakes using medium-resolution sensors.",
doi = "10.3390/rs11151744",
url = "http://dx.doi.org/10.3390/rs11151744",
issn = "2072-4292",
language = "en",
targetfile = "remotesensing-11-01744.pdf",
urlaccessdate = "21 maio 2024"
}