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dc.contributor.authorTayfur, G
dc.date.accessioned2021-02-12T18:52:46Z
dc.date.available2021-02-12T18:52:46Z
dc.date.issued2003
dc.identifier.isbn1-4020-1398-1
dc.identifier.issn1568-1238
dc.identifier.urihttps://hdl.handle.net/11147/10774
dc.descriptionNATO Advanced Research Workshop on Integrated Technologies for Environmental Monitoring and Information Productionen_US
dc.description.abstractSt. Venant equations, which are used to model sheet flows, are point-scale, depth-averaged equations, requiring data on model parameters at a very fine scale. When data are available at the scale of a hillslope transect, the point equations need to be upscaled to conserve the mass and momentum at that scale, Hillslope-scale upscaled model must be developed if data are available at that scale. The performance of the three models applied to simulate flows from non-rilled surfaces revealed that the hillslope-scale upscaled model performs as good as the point-scale model though it uses far less data. The transectionally-upscaled model slightly underestimates the observed data.en_US
dc.description.sponsorshipNATO Sci Affairs Diven_US
dc.language.isoengen_US
dc.publisherSPRINGERen_US
dc.relation.ispartofseriesNATO Science Series IV Earth and Environmental Sciences
dc.rightsinfo:eu-repo/semantics/closedAccessen_US
dc.titleUpscaling surface flow equations depending upon data availability at different scalesen_US
dc.typeconferenceObjecten_US
dc.typeconferenceObjecten_US
dc.contributor.institutionauthorTayfur, G
dc.relation.journalIntegrated Technologies For Environmental Monitoring And Information Productionen_US
dc.contributor.departmentIzmir Isntitute of Technologyen_US
dc.identifier.volume23en_US
dc.identifier.startpage289en_US
dc.identifier.endpage300en_US
dc.identifier.wosWOS:000222998400022
dc.relation.publicationcategoryMakale - Uluslararası Hakemli Dergi - Kurum Öğretim Elemanıen_US


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