@Article{FassoniAndradePaiRudBarNov:2020:CaStAm,
author = "Fassoni Andrade, Alice C{\'e}sar and Paiva, Rodrigo Cauduro Dias
de and Rudorff, Conrado de Moraes and Barbosa, Cl{\'a}udio
Clemente Faria and Novo, Evlyn M{\'a}rcia Le{\~a}o de Moraes",
affiliation = "{Universidade Federal do Rio Grande do Sul (UFRGS)} and
{Universidade Federal do Rio Grande do Sul (UFRGS)} and {Centro
Nacional de Monitoramento e Alertas de Desastres Naturais
(CEMADEN)} and {Instituto Nacional de Pesquisas Espaciais (INPE)}
and {Instituto Nacional de Pesquisas Espaciais (INPE)}",
title = "High-resolution mapping of floodplain topography from space: A
case study in the Amazon",
journal = "Remote Sensing of Environment",
year = "2020",
volume = "251",
pages = "e112065",
month = "Dec.",
keywords = "Flood frequency, Water level, Topography, Digital elevation model,
MERIT, SRTM, Amazon, Lakes, Floodplain, Geomorphology changes,
Storage volume, Altimetry, ICESat, Landsat, Global surface water,
Google earth engine.",
abstract = "Terrain elevation is essential for land management, navigation,
and earth science applications. Remote sensing advancements have
led to an increase in the availability of a range of digital
elevation models with global to quasi-global land coverage.
However, the generation of these models in water bodies requires
specialized approaches, such as the delimitation of the shorelines
(isobaths) of lakes over time. Therefore, the processing costs are
high in complex areas with many lakes. Currently, there is no
systematic topographic mapping of lakes and channels in large and
complex floodplains using remote sensing data. We present here the
first high-resolution topographic mapping (30 m) of the
non-forested portion of the middle-lower Amazon floodplain using a
new method based on in-situ Amazon river water levels and a
flood-frequency map derived from the Landsat Global Surface Water
Dataset. Validation using locally derived bathymetry showed a root
mean square error (RMSE) of 0.89 m for floodplain elevation and a
good representation of spatial patterns with Pearson's correlation
coefficient of 0.77. Our approach for improving topographic
representation in open water areas is an alternative to SRTM3 DEM
or MERIT DEM, which represents these areas as a flat surface. We
also generated the Amazon River bathymetry using nautical charts
from the Brazilian Navy (average RMSE of 7.5 m and bias of 5 m),
and floodplain depths maps corresponding to the high- and
low-water periods of the river flood wave. The results show that
the storage volume in the open-water floodplain varies 104.3 km3
on average each year (from 11.9 km3 in low-water to 116.2 km3 in
high-water). The method can be applied to any temporarily flooded
area to provide the often missing underwater digital topographic
data required for hydrological, ecological, and geomorphological
studies. The data set developed in this study can be found at
https://doi-org.ez61.periodicos.capes.gov.br/10.17632/vn599y9szb.1.",
doi = "10.1016/j.rse.2020.112065",
url = "http://dx.doi.org/10.1016/j.rse.2020.112065",
issn = "0034-4257",
language = "en",
targetfile = "andrade_high.pdf",
urlaccessdate = "27 abr. 2024"
}