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dc.contributorDepartment of Civil and Environmental Engineeringen_US
dc.creatorWang, WCen_US
dc.creatorZhao, YWen_US
dc.creatorChau, KWen_US
dc.creatorXu, DMen_US
dc.creatorLiu, CJen_US
dc.date.accessioned2021-09-09T03:39:47Z-
dc.date.available2021-09-09T03:39:47Z-
dc.identifier.issn1464-7141en_US
dc.identifier.urihttp://hdl.handle.net/10397/91110-
dc.language.isoenen_US
dc.publisherInternational Water Association Publishingen_US
dc.rights© 2021 The Authorsen_US
dc.rightsThis is an Open Access article distributed under the terms of the Creative Commons Attribution Licence (CC BY 4.0), which permits copying, adaptation and redistribution, provided the original work is properly cited (http://creativecommons.org/licenses/by/4.0/).en_US
dc.rightsThe following publication Wang, W. C., Zhao, Y. W., Chau, K. W., Xu, D. M., & Liu, C. J. (2021). Improved flood forecasting using geomorphic unit hydrograph based on spatially distributed velocity field. Journal of Hydroinformatics, 23(4), 724-739 is available at https://doi.org/10.2166/hydro.2021.135.en_US
dc.subjectDistributed hydrological modelen_US
dc.subjectFlood forecastingen_US
dc.subjectGeomorphic unit hydrographen_US
dc.subjectHydrodynamic energyen_US
dc.subjectSpatially distributed velocity fielden_US
dc.titleImproved flood forecasting using geomorphic unit hydrograph based on spatially distributed velocity fielden_US
dc.typeJournal/Magazine Articleen_US
dc.identifier.spage724en_US
dc.identifier.epage739en_US
dc.identifier.volume23en_US
dc.identifier.issue4en_US
dc.identifier.doi10.2166/hydro.2021.135en_US
dcterms.abstractThis paper presents an energy model for determining the overland flow velocity in order to improve the low accuracy problem in flow concentration simulation. It furnishes a novel idea for studying flow concentration in ungauged basins. The model can be widely applied in analysis of spatial velocity field, extraction of instantaneous geomorphic unit hydrograph and development of distributed hydrological model. A distributed flood-forecasting model is constructed for Lianyuan Basin in Hunan Province of China. In the proposed method, gravitational potential energy is transformed into kinetic energy via an analysis of energy distribution of water particles in the basin. Based on the kinetic energy equation, the overland flow velocity simulating the geomorphic unit hydrograph is computed. Rainfall-runoff simulation is then performed by integrating with runoff yield and concentration model. Results indicate that the model based on energy conversion leads to more accurate results.en_US
dcterms.abstractThe model has the following advantages: firstly, the spatial distribution of the velocity field is appropriate; secondly, the model has only one parameter, which is easily determined; and finally, flow velocity results can be used for the computation of river network flow concentration.en_US
dcterms.accessRightsopen accessen_US
dcterms.bibliographicCitationJournal of hydroinformatics, 1 July 2021, v. 23, no. 4, 724-739en_US
dcterms.isPartOfJournal of hydroinformaticsen_US
dcterms.issued2021-07-01-
dc.identifier.isiWOS:000646254700001-
dc.description.validate202109 bchyen_US
dc.description.oaVersion of Recorden_US
dc.identifier.FolderNumberOA_Scopus/WOS-
dc.description.pubStatusPublisheden_US
dc.description.TAIWAP (2023) -“Subscribe to Open” since 2021en_US
dc.description.oaCategoryTAen_US
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