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Bankfull discharge in mountain streams in the Cauca Region of Colombia

dc.contributor.authorArbeláez, Ana C., author
dc.contributor.authorGuevara, María Elvira, author
dc.contributor.authorPosada, Lillian, author
dc.contributor.authorGonzález, Luís Jorge, author
dc.contributor.authorGallardo, Carlos A., author
dc.contributor.authorColorado State University, publisher
dc.date.accessioned2020-02-04T20:45:34Z
dc.date.available2020-02-04T20:45:34Z
dc.date.issued2007
dc.description2007 annual AGU hydrology days was held at Colorado State University on March 19 - March 21, 2007.
dc.descriptionIncludes bibliographical references.
dc.description.abstractA flow considered effective or dominant in the process of stable channel forming, is the bankfull discharge associated to frequency between 1 and 2 years with an average of 1.5 year, according to Dunne and Leopold, 1978. Bankfull discharge or forming discharge is the flow which defines the morphological characteristics of the channel such as bars, meanders and curves. In this article, different approximations for channel forming discharge are explored from the morphological and statistical point of view, in order to establish the frequency of the forming discharge for some rivers in the Andes Region of the Department of Cauca, Colombia.
dc.format.mediumborn digital
dc.format.mediumproceedings (reports)
dc.identifier.urihttps://hdl.handle.net/10217/200685
dc.identifier.urihttp://dx.doi.org/10.25675/10217/200685
dc.languageEnglish
dc.language.isoeng
dc.publisherColorado State University. Libraries
dc.relation.ispartofHydrology Days
dc.rightsCopyright and other restrictions may apply. User is responsible for compliance with all applicable laws. For information about copyright law, please see https://libguides.colostate.edu/copyright.
dc.titleBankfull discharge in mountain streams in the Cauca Region of Colombia
dc.title.alternativeHydrology days 2007
dc.title.alternativeAGU hydrology days 2007
dc.typeText

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