Please use this identifier to cite or link to this item: https://hdl.handle.net/10316/4002
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dc.contributor.authorLima, João L. M. P. de-
dc.contributor.authorSingh, Vijay P.-
dc.contributor.authorLima, M. Isabel P. de-
dc.date.accessioned2008-09-01T09:47:17Z-
dc.date.available2008-09-01T09:47:17Z-
dc.date.issued2003en_US
dc.identifier.citationCATENA. 52:1 (2003) 39-56en_US
dc.identifier.urihttps://hdl.handle.net/10316/4002-
dc.description.abstractAlthough the problem of storm movement affecting flows (shape of the hydrograph and peak discharges) has been recognised for a long time, most overland flow and water erosion studies do not take into account the effect on the runoff response caused by the movement of the storm across the catchment. Ignoring of the storm movement can result in considerable over- and underestimation of runoff volumes and peaks, and associated soil loss by sheet erosion.en_US
dc.description.urihttp://www.sciencedirect.com/science/article/B6VCG-477FTX5-2/1/e8eff27149827ca222d052137819ed4aen_US
dc.format.mimetypeaplication/PDFen
dc.language.isoengeng
dc.rightsopenAccesseng
dc.subjectSoil erosionen_US
dc.subjectStorm movementen_US
dc.subjectRainfall simulationen_US
dc.subjectOverland flowen_US
dc.titleThe influence of storm movement on water erosion: storm direction and velocity effectsen_US
dc.typearticleen_US
dc.identifier.doi10.1016/S0341-8162(02)00149-2-
uc.controloAutoridadeSim-
item.openairetypearticle-
item.cerifentitytypePublications-
item.languageiso639-1en-
item.fulltextCom Texto completo-
item.grantfulltextopen-
item.openairecristypehttp://purl.org/coar/resource_type/c_18cf-
crisitem.author.researchunitMARE - Marine and Environmental Sciences Centre-
crisitem.author.researchunitMARE - Marine and Environmental Sciences Centre-
crisitem.author.orcid0000-0002-0135-2249-
crisitem.author.orcid0000-0002-5134-4175-
Appears in Collections:FCTUC Eng.Civil - Artigos em Revistas Internacionais
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