@InProceedings{LealPoCiYaSaBi:2017:ReGu,
author = "Leal, Philipe Riskalla and Pomp{\^e}o, Marcelo Luiz Martins and
Cintra, Jorge Pimentel and Yamamoto, Jorge Kazuo and Santos,
Rozely Ferreira dos and Bitencourt, Marisa Dantas",
affiliation = "{Instituto Nacional de Pesquisas Espaciais (INPE)}",
title = "Modelagem de relevo submerso atrav{\'e}s de geoprocessamento:
Reservat{\'o}rio Guarapiranga ? SP",
booktitle = "Anais...",
year = "2017",
editor = "Gherardi, Douglas Francisco Marcolino and Arag{\~a}o, Luiz
Eduardo Oliveira e Cruz de",
pages = "577--584",
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 = "This work aimed at a Fishfinder bathymetric data processing in GIS
(Geographic Information System) environment, in order to assess
lentic ecosystem morphometry. The Reservoir Guarapiranga has been
utilized as the model environment for data acquisition and results
interpretation. This reservoir is of major importance to the
S{\~a}o Paulo Metropolitan Region Brazil, responsible for 20% of
its water supply. It is considered a shallow reservoir, with
highly urbanized margins, and it is one of the eldest reservoirs
of the region (110 years). The bathymetric data has been assessed
during July 29 and 30 of 2015, relative to the water levels 735.11
and 735.10 meters respectively, through the GARMIN GPSmap (model
421S). The reservoirs margins have been assessed through visual
vectorization based on the water limits derived from the
ALOS-AVNIR images of 03/09/2010. 18.677 bathymetric points have
been assessed through the Fishfinder, and others 3488 points from
the margins visual vectorization. Our results are: a) the
bathymetric data interpolation processing which best represented
the underwater surface has been the Triangular Irregular Network
(TIN) with Delaunay triangulation; b) the reservoir depth varied
between zero e 17m; c) a useful volume of 160.09 hm3; d) a
projected area of 24.85 Km2 of free water surface (with no
macrophytes, exposed soils or islands); e) real surface area of
45.32 Km2 of free water surface, which is the reservoirs bed real
surface. Conclusions: a) the Fishfinder has properly served its
purposes, presenting easy handling and low cost; b) the reservoirs
morphometric structures perception became evident with the TIN
interpolation, denoting its dependency to the interpolator
applied; c) by comparing the reservoirs original volume with the
one found by this research, one may notice little difference; d)
the GIS tools have shown to be applicable to tridimensional
studies, which are of major importance for limnological studies.",
conference-location = "Santos",
conference-year = "28-31 maio 2017",
isbn = "978-85-17-00088-1",
label = "60194",
language = "pt",
organisation = "Instituto Nacional de Pesquisas Espaciais (INPE)",
ibi = "8JMKD3MGP6W34M/3PS44H6",
url = "http://urlib.net/ibi/8JMKD3MGP6W34M/3PS44H6",
targetfile = "60194.pdf",
type = "Recursos h{\'{\i}}dricos",
urlaccessdate = "27 abr. 2024"
}