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dc.contributor.authorHassan Abdalla, Elhadi Mohsen
dc.contributor.authorAlfredsen, Knut
dc.contributor.authorMuthanna, Tone Merete
dc.date.accessioned2022-04-22T11:37:57Z
dc.date.available2022-04-22T11:37:57Z
dc.date.created2022-02-07T10:53:06Z
dc.date.issued2022
dc.identifier.issn0022-1694
dc.identifier.urihttps://hdl.handle.net/11250/2992277
dc.description.abstractConceptual rainfall-runoff models (CRRMs) can be used as a design tool for green roofs due to their simplicity and acceptable accuracy. This study showed how the uncertainty of CRRM parameters could be reduced by changing the calibration practice, which can enhance the interpretation and identifiability of CRRM parameters. A CRRM was developed and tested on a dataset of 14 extensive green roofs located in four Norwegian cities with different climatic conditions. Two calibration schemes were compared: a common scheme using runoff data as a basis for calibration (single-objective), and a scheme combining runoff and soil moisture data for the calibration (multi-objective scheme). The results confirmed the ability of the CRRM to simulate runoff from extensive green roofs across multiple climatic zones and different roof configurations (Kling Gupta Efficiency > 0.75). The multi-objective calibration scheme was found to reduce the uncertainty of the CRRM parameters, especially the storage parameters, enhancing the physical interpretation of parameter values. The study attempted to give guidelines to estimate parameters of the CRRM which can be used by practitioners for new roof configurations under different climatic conditions.en_US
dc.language.isoengen_US
dc.publisherElsevieren_US
dc.rightsNavngivelse 4.0 Internasjonal*
dc.rights.urihttp://creativecommons.org/licenses/by/4.0/deed.no*
dc.titleTowards improving the calibration practice of conceptual hydrological models of extensive green roofsen_US
dc.typePeer revieweden_US
dc.typeJournal articleen_US
dc.description.versionpublishedVersionen_US
dc.source.volume607en_US
dc.source.journalJournal of Hydrologyen_US
dc.identifier.doi10.1016/j.jhydrol.2022.127548
dc.identifier.cristin1998454
dc.relation.projectNorges forskningsråd: 237859en_US
cristin.ispublishedtrue
cristin.fulltextoriginal
cristin.qualitycode2


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