MORPHOMETRIC OF THE COLORADO RIVER HIGH BASIN, ARGENTINA

The Grande and Barrancas Rivers watersheds conform the upper basin of the Colorado River. They provide discharge from snow precipitated in the high mountain peaks. Morphometric and functional characteristics analysis of a basin is elementary in hydrology and modeling approach. The aim of this work w...

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Main Authors: Carolina Manuela Aumassanne, Fernanda Julia Gaspari, Maria Eugenia Bege, Paolo Daniel Sartor, Patricio Oricchio, Carlos Marcelo Di Bella
Format: Article
Language:English
Published: Departamento de Geografía, Facultad de Humanidades, Universidad Nacional del Comahue 2018-09-01
Series:Boletín Geográfico
Subjects:
Online Access:http://revele.uncoma.edu.ar/htdoc/revele/index.php/geografia/article/view/2056
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spelling doaj-a49c6ca311004dc383d023e9a8ecc7682020-11-25T03:02:19ZengDepartamento de Geografía, Facultad de Humanidades, Universidad Nacional del ComahueBoletín Geográfico0326-17352313-903X2018-09-0114013171960MORPHOMETRIC OF THE COLORADO RIVER HIGH BASIN, ARGENTINACarolina Manuela Aumassanne0Fernanda Julia GaspariMaria Eugenia BegePaolo Daniel SartorPatricio OricchioCarlos Marcelo Di BellaBiblioteca Central UNCoThe Grande and Barrancas Rivers watersheds conform the upper basin of the Colorado River. They provide discharge from snow precipitated in the high mountain peaks. Morphometric and functional characteristics analysis of a basin is elementary in hydrology and modeling approach. The aim of this work was to analyze and interpret the morphometric parameters and derived indices of the upper basin of the Colorado River, Argentina. Parameters quantification and analysis were based on a digital elevation model and Geographic Information Systems. Length of the Grande River is three times greater than Barrancas River ones, with a drainage area that follows the same relationship. Gravelius coefficients evidenced similarities in watershed shapes, both rectangled-oblongued. Both watersheds have a half of their area between 1500 and 2500 m.a.s.l., with predominant slopes between 0 and 15o. In both cases, 54% of slopes are orientated to south direction, meaning predominantly shady. Barrancas River has a greater difference between the source and the mouth, having a smaller drained area. Results from this study offers an important source of base information to further research and modeling spatio-temporal dynamics of flow of River basin.http://revele.uncoma.edu.ar/htdoc/revele/index.php/geografia/article/view/2056río granderío barrancassrtm
collection DOAJ
language English
format Article
sources DOAJ
author Carolina Manuela Aumassanne
Fernanda Julia Gaspari
Maria Eugenia Bege
Paolo Daniel Sartor
Patricio Oricchio
Carlos Marcelo Di Bella
spellingShingle Carolina Manuela Aumassanne
Fernanda Julia Gaspari
Maria Eugenia Bege
Paolo Daniel Sartor
Patricio Oricchio
Carlos Marcelo Di Bella
MORPHOMETRIC OF THE COLORADO RIVER HIGH BASIN, ARGENTINA
Boletín Geográfico
río grande
río barrancas
srtm
author_facet Carolina Manuela Aumassanne
Fernanda Julia Gaspari
Maria Eugenia Bege
Paolo Daniel Sartor
Patricio Oricchio
Carlos Marcelo Di Bella
author_sort Carolina Manuela Aumassanne
title MORPHOMETRIC OF THE COLORADO RIVER HIGH BASIN, ARGENTINA
title_short MORPHOMETRIC OF THE COLORADO RIVER HIGH BASIN, ARGENTINA
title_full MORPHOMETRIC OF THE COLORADO RIVER HIGH BASIN, ARGENTINA
title_fullStr MORPHOMETRIC OF THE COLORADO RIVER HIGH BASIN, ARGENTINA
title_full_unstemmed MORPHOMETRIC OF THE COLORADO RIVER HIGH BASIN, ARGENTINA
title_sort morphometric of the colorado river high basin, argentina
publisher Departamento de Geografía, Facultad de Humanidades, Universidad Nacional del Comahue
series Boletín Geográfico
issn 0326-1735
2313-903X
publishDate 2018-09-01
description The Grande and Barrancas Rivers watersheds conform the upper basin of the Colorado River. They provide discharge from snow precipitated in the high mountain peaks. Morphometric and functional characteristics analysis of a basin is elementary in hydrology and modeling approach. The aim of this work was to analyze and interpret the morphometric parameters and derived indices of the upper basin of the Colorado River, Argentina. Parameters quantification and analysis were based on a digital elevation model and Geographic Information Systems. Length of the Grande River is three times greater than Barrancas River ones, with a drainage area that follows the same relationship. Gravelius coefficients evidenced similarities in watershed shapes, both rectangled-oblongued. Both watersheds have a half of their area between 1500 and 2500 m.a.s.l., with predominant slopes between 0 and 15o. In both cases, 54% of slopes are orientated to south direction, meaning predominantly shady. Barrancas River has a greater difference between the source and the mouth, having a smaller drained area. Results from this study offers an important source of base information to further research and modeling spatio-temporal dynamics of flow of River basin.
topic río grande
río barrancas
srtm
url http://revele.uncoma.edu.ar/htdoc/revele/index.php/geografia/article/view/2056
work_keys_str_mv AT carolinamanuelaaumassanne morphometricofthecoloradoriverhighbasinargentina
AT fernandajuliagaspari morphometricofthecoloradoriverhighbasinargentina
AT mariaeugeniabege morphometricofthecoloradoriverhighbasinargentina
AT paolodanielsartor morphometricofthecoloradoriverhighbasinargentina
AT patriciooricchio morphometricofthecoloradoriverhighbasinargentina
AT carlosmarcelodibella morphometricofthecoloradoriverhighbasinargentina
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