@InProceedings{OliveiraFlBrHaEcQu:2017:AsMoHi,
author = "Oliveira, Guilherme Garcia de and Flores, Ta{\'{\i}}sa and
Bresolin Junior, Nestor Antonio and Haetinger, Claus and Eckhardt,
Rafael Rodrigo and Quevedo, Renata Pacheco",
title = "Associa{\c{c}}{\~a}o entre modelos hidrol{\'o}gicos e
geotecnologias para identifica{\c{c}}{\~a}o de {\'a}reas
suscet{\'{\i}}veis a inunda{\c{c}}{\~o}es e enxurradas em
locais com baixa disponibilidade de dados altim{\'e}tricos e
hidrol{\'o}gicos",
booktitle = "Anais...",
year = "2017",
editor = "Gherardi, Douglas Francisco Marcolino and Arag{\~a}o, Luiz
Eduardo Oliveira e Cruz de",
pages = "1210--1217",
organization = "Simp{\'o}sio Brasileiro de Sensoriamento Remoto, 18. (SBSR)",
publisher = "Instituto Nacional de Pesquisas Espaciais (INPE)",
address = "S{\~a}o Jos{\'e} dos Campos",
abstract = "Natural disasters very often have caused deep impacts on human
society. It is estimated that in the last decade about 1.5 billion
people around the globe were affected by hydrometeorological
events. In order to prevent natural disasters to reach careless
and susceptible areas, several methodologies have been presented
to identity the vulnerability. The identification of susceptible
areas to floods in the Forqueta River Basin has been conducted by
the utilization of a modelling method that integrates the
hydrological simulation and the use of geotechnologies. The
definition of extreme rainfall in return periods (RP) of 10, 30
and 100 years was carried out by using an
intensity-duration-frequency equation. Shuttle Radar Topography
Mission data were used to the delimitation of the basins and
rivers. The Soil Conservation Service method was used for the
transformation of rain runoff, while the spread of river flood
wave was conducted by Muskingum-Cunge model. The extreme
precipitation scenario for a period of 25 hours ranged from 123mm
(RP10) to 179mm (RP100). Hydrological simulation revealed that the
maximum flow rates can exceed 8,000m3.s-1 at the Forqueta river
outfall, with wet area section larger than 5,000m2 and waters
rising more than 10m on the average. About 2% of the basin showed
some degree of susceptibility (RP100), adding up to 53km2 of
wetlands. The approach has shown consistent results concerning to
flows and flood levels. One may conclude that the same data set
could be applied to other fields of study, for regional
hydrological characterization of susceptibility to disasters.",
conference-location = "Santos",
conference-year = "28-31 maio 2017",
isbn = "978-85-17-00088-1",
label = "59231",
language = "pt",
organisation = "Instituto Nacional de Pesquisas Espaciais (INPE)",
ibi = "8JMKD3MGP6W34M/3PS4GB9",
url = "http://urlib.net/ibi/8JMKD3MGP6W34M/3PS4GB9",
targetfile = "59231.pdf",
type = "Hidrologia",
urlaccessdate = "27 abr. 2024"
}