@Article{OvandoMarTomRodRan:2018:MuFlMa,
author = "Ovando, Alex Leyton and Martinez, Jean Michel and Tomasella,
Javier and Rodriguez, Daniel Andr{\'e}s and von Randow, Celso",
affiliation = "{Centro Nacional de Monitoramento e Alertas de Desastres Naturais
(CEMADEN)} and {Institut de Recherche pour le D{\'e}veloppement
(IRD)} and {Centro Nacional de Monitoramento e Alertas de
Desastres Naturais (CEMADEN)} and {Universidade Federal do Rio de
Janeiro (UFRJ)} and {Instituto Nacional de Pesquisas Espaciais
(INPE)}",
title = "Multi-temporal flood mapping and satellite altimetry used to
evaluate the flood dynamics of the Bolivian Amazon wetlands",
journal = "International Journal of Applied Earth Observation and
Geoinformation",
year = "2018",
volume = "69",
pages = "27--40",
abstract = "The Bolivian Amazon wetlands are extensive floodplains distributed
over the Mamore, Beni, Madre de Dios and Guapore Rivers. Located
within the upper Madeira River Basin, the wetlands play important
roles in regulating the biogeochemical processes and hydrological
cycle of the region. In addition, they have major ecological and
hydrological relevance for the entire Amazon Basin. These wetlands
are characterized by the occurrence of episodic floods that result
from contrasting hydro-meteorological processes in the Andean
Mountain region, the piedmont area and the Amazon lowlands. In
this study, we characterized the flood dynamics of the region
using multi-temporal flood mapping based on optical altimetry
(MODIS Moderate Resolution Imaging Spectroradiometer M*D09A1) and
satellite altimetry (ENVISAT RA-2 and SARAL AltiKa altimeters).
This study provides new insights regarding the frequency,
magnitude and spatial distribution of exogenous floods, which are
created by flood waves from the Andes; and endogenous floods,
which result from runoff originating in the lowlands. The maximum
extent of flooding during 20012014 was 43144\ km2 in the
Mamore Basin and 34852\ km2 in the Guapore Basin, and the
total surface water storage in these floodplains reached
94\ km3. The regionalization of flood regimes based on
water stage time series signatures allowed those regions that are
exposed to frequent floods, which are generally located along
rivers without a direct connection with the Andes, to be
distinguished from floodplains that are more dependent on flood
waves originating in the Andes and its piedmonts. This information
is of great importance for understanding the roles of these
wetlands in the provision of ecosystem services.",
doi = "10.1016/j.jag.2018.02.013",
url = "http://dx.doi.org/10.1016/j.jag.2018.02.013",
issn = "0303-2434",
label = "lattes: 0535860239259102 5 OvandoMarTomRodRan:2018:MuFlMa",
language = "en",
urlaccessdate = "30 abr. 2024"
}