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

Terengganu 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 a...

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Main Authors: Ahmad S.A., Samad D.H., Yusof N.M., Sidek L.M., Basri H., Omar S.M.A., Ahmad F., Muda Z.C., Hafez Ahmed M.A.
Other Authors: 58679834900
Format: Book chapter
Published: Springer Science and Business Media Deutschland GmbH 2024
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Institution: Universiti Tenaga Nasional
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spelling my.uniten.dspace-343502024-10-14T11:19:13Z Debris Flow Induced by Heavy Rainfall in Hulu Terengganu: Hydrological and Geological Analysis Ahmad S.A. Samad D.H. Yusof N.M. Sidek L.M. Basri H. Omar S.M.A. Ahmad F. Muda Z.C. Hafez Ahmed M.A. 58679834900 58905464500 58905461900 35070506500 57065823300 57964112400 57188874669 55812444000 58905811200 Debris flow Geology Heavy rainfall Hydrology Hydropower Terengganu 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. Final 2024-10-14T03:19:13Z 2024-10-14T03:19:13Z 2023 Book chapter 10.1007/978-981-99-3708-0_65 2-s2.0-85185921093 https://www.scopus.com/inward/record.uri?eid=2-s2.0-85185921093&doi=10.1007%2f978-981-99-3708-0_65&partnerID=40&md5=d99fbe4cf9b5bceb743f3643d7c8d8e6 https://irepository.uniten.edu.my/handle/123456789/34350 Part F2265 927 948 Springer Science and Business Media Deutschland GmbH Scopus
institution Universiti Tenaga Nasional
building UNITEN Library
collection Institutional Repository
continent Asia
country Malaysia
content_provider Universiti Tenaga Nasional
content_source UNITEN Institutional Repository
url_provider http://dspace.uniten.edu.my/
topic Debris flow
Geology
Heavy rainfall
Hydrology
Hydropower
spellingShingle Debris flow
Geology
Heavy rainfall
Hydrology
Hydropower
Ahmad S.A.
Samad D.H.
Yusof N.M.
Sidek L.M.
Basri H.
Omar S.M.A.
Ahmad F.
Muda Z.C.
Hafez Ahmed M.A.
Debris Flow Induced by Heavy Rainfall in Hulu Terengganu: Hydrological and Geological Analysis
description Terengganu 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.
author2 58679834900
author_facet 58679834900
Ahmad S.A.
Samad D.H.
Yusof N.M.
Sidek L.M.
Basri H.
Omar S.M.A.
Ahmad F.
Muda Z.C.
Hafez Ahmed M.A.
format Book chapter
author Ahmad S.A.
Samad D.H.
Yusof N.M.
Sidek L.M.
Basri H.
Omar S.M.A.
Ahmad F.
Muda Z.C.
Hafez Ahmed M.A.
author_sort Ahmad S.A.
title Debris Flow Induced by Heavy Rainfall in Hulu Terengganu: Hydrological and Geological Analysis
title_short Debris Flow Induced by Heavy Rainfall in Hulu Terengganu: Hydrological and Geological Analysis
title_full Debris Flow Induced by Heavy Rainfall in Hulu Terengganu: Hydrological and Geological Analysis
title_fullStr Debris Flow Induced by Heavy Rainfall in Hulu Terengganu: Hydrological and Geological Analysis
title_full_unstemmed Debris Flow Induced by Heavy Rainfall in Hulu Terengganu: Hydrological and Geological Analysis
title_sort debris flow induced by heavy rainfall in hulu terengganu: hydrological and geological analysis
publisher Springer Science and Business Media Deutschland GmbH
publishDate 2024
_version_ 1814061176229724160