Rainfall-induced landslides in Cameron Highland area, Malaysia
Cameron Highland is classified as one of the landslide-prone areas in Malaysia due to its hilly landform. It has been discovered that the landslides in Cameron Highland were mainly triggered by the intense rainfall since the area encountered high amount of rainfall throughout the year. This study...
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my.iium.irep.878492021-01-18T02:45:08Z http://irep.iium.edu.my/87849/ Rainfall-induced landslides in Cameron Highland area, Malaysia Abu Mansor Maturidi, Abdul Muaz Kasim, Norhidayu Abu Taib, Kamarudin Binti Wan Azahar, Wan Nur Aifa Md. Husain, Nadiah TD Environmental technology. Sanitary engineering Cameron Highland is classified as one of the landslide-prone areas in Malaysia due to its hilly landform. It has been discovered that the landslides in Cameron Highland were mainly triggered by the intense rainfall since the area encountered high amount of rainfall throughout the year. This study is carried out to evaluate the correlation between the rainfall intensity- duration (I-D) and the landslide occurrences in the Cameron Highland area. Twelve cases of landslides in the study area had been selected for conducting the analysis of rainfall intensity- duration (I-D) that triggers the landslides. The important variables from the analysis such as the maximum rainfall intensity (I) and the duration of rainfall series (D) have been applied to establish the empirical rainfall intensity-duration (I-D) threshold for Cameron Highland landslide areas. Based on the study, by utilising the logarithmic scale graph and applying a power-law model from the general equation of I= αD-β , the empirical I-D threshold for Cameron Highland landslide was determined as I = 29.088D-0.075 (I = rainfall intensity in mm/hr and D = duration in hour). The empirical (I-D) threshold can be a functional mechanism for the Early Warning System (EWS) once it is further developed, that enable the relevant authority to prepare mitigation measures such as evacuation, spreading information to the civilian in order to prevent major losses and casualties due to the landslide events IOP Publishing 2020-09-21 Conference or Workshop Item PeerReviewed application/pdf en http://irep.iium.edu.my/87849/1/87849_Rainfall-Induced%20Landslides%20in%20Cameron%20Highland%20Area.pdf application/pdf en http://irep.iium.edu.my/87849/2/87849_Rainfall-Induced%20Landslides%20in%20Cameron%20Highland%20Area%20SCOPUS.pdf Abu Mansor Maturidi, Abdul Muaz and Kasim, Norhidayu and Abu Taib, Kamarudin and Binti Wan Azahar, Wan Nur Aifa and Md. Husain, Nadiah (2020) Rainfall-induced landslides in Cameron Highland area, Malaysia. In: International Conference on Technology, Engineering and Sciences (ICTES) 2020, 17th-18th April 2020, Penang, Malaysia. https://iopscience.iop.org/article/10.1088/1757-899X/917/1/012019/pdf 10.1088/1757-899X/917/1/012019 |
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TD Environmental technology. Sanitary engineering Abu Mansor Maturidi, Abdul Muaz Kasim, Norhidayu Abu Taib, Kamarudin Binti Wan Azahar, Wan Nur Aifa Md. Husain, Nadiah Rainfall-induced landslides in Cameron Highland area, Malaysia |
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Cameron Highland is classified as one of the landslide-prone areas in Malaysia due
to its hilly landform. It has been discovered that the landslides in Cameron Highland were
mainly triggered by the intense rainfall since the area encountered high amount of rainfall
throughout the year. This study is carried out to evaluate the correlation between the rainfall
intensity- duration (I-D) and the landslide occurrences in the Cameron Highland area. Twelve
cases of landslides in the study area had been selected for conducting the analysis of rainfall
intensity- duration (I-D) that triggers the landslides. The important variables from the analysis
such as the maximum rainfall intensity (I) and the duration of rainfall series (D) have been
applied to establish the empirical rainfall intensity-duration (I-D) threshold for Cameron
Highland landslide areas. Based on the study, by utilising the logarithmic scale graph and
applying a power-law model from the general equation of I= αD-β
, the empirical I-D threshold
for Cameron Highland landslide was determined as I = 29.088D-0.075 (I = rainfall intensity in
mm/hr and D = duration in hour). The empirical (I-D) threshold can be a functional
mechanism for the Early Warning System (EWS) once it is further developed, that enable the
relevant authority to prepare mitigation measures such as evacuation, spreading information to
the civilian in order to prevent major losses and casualties due to the landslide events |
format |
Conference or Workshop Item |
author |
Abu Mansor Maturidi, Abdul Muaz Kasim, Norhidayu Abu Taib, Kamarudin Binti Wan Azahar, Wan Nur Aifa Md. Husain, Nadiah |
author_facet |
Abu Mansor Maturidi, Abdul Muaz Kasim, Norhidayu Abu Taib, Kamarudin Binti Wan Azahar, Wan Nur Aifa Md. Husain, Nadiah |
author_sort |
Abu Mansor Maturidi, Abdul Muaz |
title |
Rainfall-induced landslides in Cameron Highland area, Malaysia |
title_short |
Rainfall-induced landslides in Cameron Highland area, Malaysia |
title_full |
Rainfall-induced landslides in Cameron Highland area, Malaysia |
title_fullStr |
Rainfall-induced landslides in Cameron Highland area, Malaysia |
title_full_unstemmed |
Rainfall-induced landslides in Cameron Highland area, Malaysia |
title_sort |
rainfall-induced landslides in cameron highland area, malaysia |
publisher |
IOP Publishing |
publishDate |
2020 |
url |
http://irep.iium.edu.my/87849/1/87849_Rainfall-Induced%20Landslides%20in%20Cameron%20Highland%20Area.pdf http://irep.iium.edu.my/87849/2/87849_Rainfall-Induced%20Landslides%20in%20Cameron%20Highland%20Area%20SCOPUS.pdf http://irep.iium.edu.my/87849/ https://iopscience.iop.org/article/10.1088/1757-899X/917/1/012019/pdf |
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