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dc.contributor.authorWei, Hsiao-Pingen_US
dc.contributor.authorSu, Yuan-Fongen_US
dc.contributor.authorCheng, Chao-Tzuenen_US
dc.contributor.authorYeh, Keh-Chiaen_US
dc.date.accessioned2020-10-05T01:59:51Z-
dc.date.available2020-10-05T01:59:51Z-
dc.date.issued2020-06-01en_US
dc.identifier.urihttp://dx.doi.org/10.3390/su12114511en_US
dc.identifier.urihttp://hdl.handle.net/11536/154982-
dc.description.abstractWith the growing concern about the failure risk of river embankments in a rapidly changing climate, this study aims to quantify the overtopping probability of river embankment in Kao-Ping River basin in southern Taiwan. A water level simulation model is calibrated and validated with historical typhoon events and the calibrated model is further used to assess overtopping risk in the future under a climate change scenario. A dynamic downscaled projection dataset, provided by Meteorological Research Institute (MRI) has been further downscaled to 5-km grids and bias-corrected with a quantile mapping method, is used to simulate the water level of Kao-Ping River in the future. Our results highlighted that the overtopping risk of Kao-Ping River increased by a factor of 5.7 similar to 8.0 by the end of the 21st century.en_US
dc.language.isoen_USen_US
dc.subjectclimate changeen_US
dc.subjectovertopping risken_US
dc.subjectleveeen_US
dc.titleLevee Overtopping Risk Assessment under Climate Change Scenario in Kao-Ping River, Taiwanen_US
dc.typeArticleen_US
dc.identifier.doi10.3390/su12114511en_US
dc.identifier.journalSUSTAINABILITYen_US
dc.citation.volume12en_US
dc.citation.issue11en_US
dc.citation.spage0en_US
dc.citation.epage0en_US
dc.contributor.department土木工程學系zh_TW
dc.contributor.departmentDepartment of Civil Engineeringen_US
dc.identifier.wosnumberWOS:000543391800174en_US
dc.citation.woscount0en_US
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