Publication:
Debris Flow Induced by Heavy Rainfall in Hulu Terengganu: Hydrological and Geological Analysis

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dc.citedby0
dc.contributor.authorAhmad S.A.en_US
dc.contributor.authorSamad D.H.en_US
dc.contributor.authorYusof N.M.en_US
dc.contributor.authorSidek L.M.en_US
dc.contributor.authorBasri H.en_US
dc.contributor.authorOmar S.M.A.en_US
dc.contributor.authorAhmad F.en_US
dc.contributor.authorMuda Z.C.en_US
dc.contributor.authorHafez Ahmed M.A.en_US
dc.contributor.authorid58679834900en_US
dc.contributor.authorid58905464500en_US
dc.contributor.authorid58905461900en_US
dc.contributor.authorid35070506500en_US
dc.contributor.authorid57065823300en_US
dc.contributor.authorid57964112400en_US
dc.contributor.authorid57188874669en_US
dc.contributor.authorid55812444000en_US
dc.contributor.authorid58905811200en_US
dc.date.accessioned2024-10-14T03:19:13Z
dc.date.available2024-10-14T03:19:13Z
dc.date.issued2023
dc.description.abstractTerengganu is one of the states in Malaysia that will be the most affected by the northeast monsoon which usually happens early in November and lasts until March every year. Continuous heavy rainfall may cause various natural disasters including debris flow. Due to the features of sudden outbursts and high energy density, debris flow has caused a significant number of deaths in several geohazard incidents in Malaysia. In contrast to other types of landslides, almost all debris flows begin on natural topography. The majority of the incident was caused by rain. Intense and severe rainfall raises the water content and pore water pressure inside the remaining soil, potentially causing landslides. Based on a recent event on February 27, 2022, this study will examine the hydrological analysis including rainfall time series and rainfall distribution by using rainfall data from February 23, 2022, until March 1, 2022, along with geological analysis of the upper part of Hulu Terengganu. As a result, heavy and sustained rainfall has proved to become the primary cause of debris flow. � The Author(s), under exclusive license to Springer Nature Singapore Pte Ltd. 2023.en_US
dc.description.natureFinalen_US
dc.identifier.doi10.1007/978-981-99-3708-0_65
dc.identifier.epage948
dc.identifier.scopus2-s2.0-85185921093
dc.identifier.spage927
dc.identifier.urihttps://www.scopus.com/inward/record.uri?eid=2-s2.0-85185921093&doi=10.1007%2f978-981-99-3708-0_65&partnerID=40&md5=d99fbe4cf9b5bceb743f3643d7c8d8e6
dc.identifier.urihttps://irepository.uniten.edu.my/handle/123456789/34350
dc.identifier.volumePart F2265
dc.pagecount21
dc.publisherSpringer Science and Business Media Deutschland GmbHen_US
dc.sourceScopus
dc.sourcetitleWater Resources Development and Management
dc.subjectDebris flow
dc.subjectGeology
dc.subjectHeavy rainfall
dc.subjectHydrology
dc.subjectHydropower
dc.titleDebris Flow Induced by Heavy Rainfall in Hulu Terengganu: Hydrological and Geological Analysisen_US
dc.typeBook chapteren_US
dspace.entity.typePublication
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