Rainfall intensity (I)–duration (D) induced debris flow occurrences in Peninsular Malaysia
This paper evaluates the rainfall-induced debris flow in Peninsular Malaysia from the perspective of rainfall threshold. Eight selected debris flow occurrences in Peninsular Malaysia have been used for this study. Rainfall records are obtained from the nearest meteorological station of Drainage a...
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2020
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my.iium.irep.792962024-02-23T08:31:40Z http://irep.iium.edu.my/79296/ Rainfall intensity (I)–duration (D) induced debris flow occurrences in Peninsular Malaysia Kasim, Norhidayu Abu Taib, Kamaruddin Ghazali, N.A.A. Wan Azahar, Wan Nur Aifa Ismail, Norfarah Nadia Md. Husain, Nadiah Ramli, Ahmad Bukhari Saad, Siti Asmahani Masjuki, Siti Aliyyah Ibrahim, Saerahany Legori TC401 River, lake, and water-supply engineering (General) This paper evaluates the rainfall-induced debris flow in Peninsular Malaysia from the perspective of rainfall threshold. Eight selected debris flow occurrences in Peninsular Malaysia have been used for this study. Rainfall records are obtained from the nearest meteorological station of Drainage and Irrigation Department and the Malaysia Meteorology Department. In order to determine the reasonable correlation of rainfall with the occurrence of debris flow, the relationship between rainfall intensity (I) and duration (D) has been analysed. Furthermore, to analyze the empirical rainfall threshold, the values of the maximum hourly rainfall intensity and durations that correlate with debris flow have been plotted along with the intensity against duration in log-log graph. Comparison made between the compiled Peninsular Malaysia data and the worldwide threshold value shows that the triggering threshold is mostly higher for the Peninsular Malaysia events. The presence of thicker soil layers are likely the reason of higher thresholds limit, as more rainfalls are required to cause extensive localized failures to occur. Springer, Cham 2020 Book Chapter PeerReviewed application/pdf en http://irep.iium.edu.my/79296/7/79296%20%20Rainfall%20Intensity.pdf application/pdf en http://irep.iium.edu.my/79296/8/79296%20%20Rainfall%20Intensity%20SCOPUS.pdf Kasim, Norhidayu and Abu Taib, Kamaruddin and Ghazali, N.A.A. and Wan Azahar, Wan Nur Aifa and Ismail, Norfarah Nadia and Md. Husain, Nadiah and Ramli, Ahmad Bukhari and Saad, Siti Asmahani and Masjuki, Siti Aliyyah and Ibrahim, Saerahany Legori (2020) Rainfall intensity (I)–duration (D) induced debris flow occurrences in Peninsular Malaysia. In: Proceedings of AICCE’19. Lecture Notes in Civil Engineering (53). Springer, Cham, pp. 897-903. ISBN 978-3-030-32815-3 https://link.springer.com/chapter/10.1007/978-3-030-32816-0_66 10.1007/978-3-030-32816-0_66 |
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TC401 River, lake, and water-supply engineering (General) |
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TC401 River, lake, and water-supply engineering (General) Kasim, Norhidayu Abu Taib, Kamaruddin Ghazali, N.A.A. Wan Azahar, Wan Nur Aifa Ismail, Norfarah Nadia Md. Husain, Nadiah Ramli, Ahmad Bukhari Saad, Siti Asmahani Masjuki, Siti Aliyyah Ibrahim, Saerahany Legori Rainfall intensity (I)–duration (D) induced debris flow occurrences in Peninsular Malaysia |
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This paper evaluates the rainfall-induced debris flow in Peninsular
Malaysia from the perspective of rainfall threshold. Eight selected debris flow
occurrences in Peninsular Malaysia have been used for this study. Rainfall records
are obtained from the nearest meteorological station of Drainage and Irrigation
Department and the Malaysia Meteorology Department. In order to determine the
reasonable correlation of rainfall with the occurrence of debris flow, the relationship
between rainfall intensity (I) and duration (D) has been analysed. Furthermore, to
analyze the empirical rainfall threshold, the values of the maximum hourly rainfall
intensity and durations that correlate with debris flow have been plotted along with
the intensity against duration in log-log graph. Comparison made between the
compiled Peninsular Malaysia data and the worldwide threshold value shows that
the triggering threshold is mostly higher for the Peninsular Malaysia events. The
presence of thicker soil layers are likely the reason of higher thresholds limit, as
more rainfalls are required to cause extensive localized failures to occur. |
format |
Book Chapter |
author |
Kasim, Norhidayu Abu Taib, Kamaruddin Ghazali, N.A.A. Wan Azahar, Wan Nur Aifa Ismail, Norfarah Nadia Md. Husain, Nadiah Ramli, Ahmad Bukhari Saad, Siti Asmahani Masjuki, Siti Aliyyah Ibrahim, Saerahany Legori |
author_facet |
Kasim, Norhidayu Abu Taib, Kamaruddin Ghazali, N.A.A. Wan Azahar, Wan Nur Aifa Ismail, Norfarah Nadia Md. Husain, Nadiah Ramli, Ahmad Bukhari Saad, Siti Asmahani Masjuki, Siti Aliyyah Ibrahim, Saerahany Legori |
author_sort |
Kasim, Norhidayu |
title |
Rainfall intensity (I)–duration (D) induced debris flow occurrences in Peninsular Malaysia |
title_short |
Rainfall intensity (I)–duration (D) induced debris flow occurrences in Peninsular Malaysia |
title_full |
Rainfall intensity (I)–duration (D) induced debris flow occurrences in Peninsular Malaysia |
title_fullStr |
Rainfall intensity (I)–duration (D) induced debris flow occurrences in Peninsular Malaysia |
title_full_unstemmed |
Rainfall intensity (I)–duration (D) induced debris flow occurrences in Peninsular Malaysia |
title_sort |
rainfall intensity (i)–duration (d) induced debris flow occurrences in peninsular malaysia |
publisher |
Springer, Cham |
publishDate |
2020 |
url |
http://irep.iium.edu.my/79296/7/79296%20%20Rainfall%20Intensity.pdf http://irep.iium.edu.my/79296/8/79296%20%20Rainfall%20Intensity%20SCOPUS.pdf http://irep.iium.edu.my/79296/ https://link.springer.com/chapter/10.1007/978-3-030-32816-0_66 |
_version_ |
1792146416342138880 |