Un procedimiento para la delineación de cuencas hídricas en arcview y arcinfo
PDF

Palabras clave

Cuencas hídricas
Arcview
Arcinfo

Cómo citar

Un procedimiento para la delineación de cuencas hídricas en arcview y arcinfo. (2001). Ingenieria Y Universidad, 5(1-2), 35-46. https://revistas.javeriana.edu.co/index.php/iyu/article/view/33994
Almetrics
 
Dimensions
 
Google Scholar
 
Search GoogleScholar

Resumen

Different software for Geographic Informatiori Systems (GIS), such as ArcView and ArcInfo, are available nowadays. They provide tools not only for watershed and stream network delineation, but also for the automatic calculation of their physical and geometric properties based on topographic surfaces called Digital Evaluation Models (DEM).In this context, this paper presents the basics of DEM's, explains the conceptual framework of watershed delineation, and illustrates the methodology to be followed through the application of basic commands of ArcView and ArcInfo to a geographic area

PDF

CENTER FOR RESEARCH IN WATER RESOURCES (CRWR).Gis Hydro Series Cd's 97, 98,99 Y2000. University ofTexas, Austin. 1997, 1998, 1999, 2000.

MAlDMENT, D., DJOKIC, D. Hydrologic and Hydraulic Modeling Support with Geoqraphic Informatiori Systems. Redlands: ESRI Press, 2000.

O'CALLAGHAN, J. F. y MARK, D. M. "The Extraction of Drainage Networks from Digital Elevation Data". Computer Vision, Graphics and Image Processing. 1984.

OLIVERA F., Reed, S. y MAIDMENDT. ,"HEC-PrePro v. 2.0 An ArcView Pre-Processor for HEC's Hydrologic Modeling System". En: Proceedings of the ESRI Intemational User Conference 1998, Environmental Systems Researchlnstitute, 1998.

SMITH, P. y MAIDMENT, D. Hydrologic Data Development System. Masters Thesis, Department of Civil Engineering, University of Texas, Austin. 1995.

United States Geoqraphic Survey (USGS). MDE de la Región de Colombia. En: http://edcdaac.usgs.gov/gtopo30/w100n40.html. Marzo 2001.

Creative Commons License

Esta obra está bajo una licencia internacional Creative Commons Atribución 4.0.