Geomorphic and forest cover controls on flooding: central Nepal Himalaya

dc.citation.doi10.2307/3673948
dc.citation.epage264en_US
dc.citation.issn1994-7151en_US
dc.citation.issue3en_US
dc.citation.jtitleMountain Research and Developmenten_US
dc.citation.spage257en_US
dc.citation.volume16en_US
dc.contributor.authorMarston, Richard A.
dc.contributor.authorKleinman, Jack
dc.contributor.authorMiller, Maynard
dc.contributor.authoreidrmarstonen_US
dc.date.accessioned2010-01-19T19:14:00Z
dc.date.available2010-01-19T19:14:00Z
dc.date.issued1996-08-01
dc.date.published1996en_US
dc.description.abstractDevastating monsoon season floods in the central Nepal Himalaya have been difficult to predict with any precision, reliability, or accuracy. Deforestation is often blamed as the principal cause of flooding. This paper uses field data at 22 stream crossings, together with drainage basin morphometric data and forest cover data, to determine the dominant controls on bank-full discharge from monsoon storms. Results demonstrate that 82 percent of the variation in bank-full discharge can be explained as a function of drainage area alone; forest cover did not add explanatory power. Findings from this study can be used to guide planning for future projects that will be affected by flood hazards in the central Nepal Himalaya, including irrigation, hydropower, and footbridge construction.en_US
dc.identifier.urihttp://hdl.handle.net/2097/2392
dc.relation.urihttps://doi.org/10.2307/3673948en_US
dc.rightsThis Item is protected by copyright and/or related rights. You are free to use this Item in any way that is permitted by the copyright and related rights legislation that applies to your use. For other uses you need to obtain permission from the rights-holder(s).
dc.rights.urihttp://rightsstatements.org/vocab/InC/1.0/
dc.subjectDeforestationen_US
dc.subjectFloodsen_US
dc.subjectHimalayasen_US
dc.subjectNepalen_US
dc.titleGeomorphic and forest cover controls on flooding: central Nepal Himalayaen_US
dc.typeArticle (publisher version)en_US

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