Cite Article

The Rainfall Effect Analysis of Landslide Occurrence on Mount Slopes of Wilis

Choose citation format

BibTeX

@article{IJASEIT6876,
   author = {Lalu Muhamad Jaelani and Rizha Fahlefi and Mohammad Khoiri and Juan Pandu Gya Nur Rochman},
   title = {The Rainfall Effect Analysis of Landslide Occurrence on Mount Slopes of Wilis},
   journal = {International Journal on Advanced Science, Engineering and Information Technology},
   volume = {10},
   number = {1},
   year = {2020},
   pages = {298--303},
   keywords = {landslides hazard; La Nina; Mount Wilis; rainfall effect.},
   abstract = {Water is a significant factor in the occurrence of landslides when rainwater absorbs into the impermeable layer of soil and causes the soil to experience weathering; thus, that the soil is not strong enough to withstand the water load. Therefore, rainfall, as well as a land slope that affects the acceleration of runoff, becomes an important indicator that affects the potential for landslides. In this research, the effect of rainfall intensity on landslide was analyzed based on monthly data collected from 81 rain gauge stations. This idea was an effort to support research related to landslides mapping on the steep area. Thus, the analysis of potential landslides that vary according to rainfall changes monthly was obtained. La Nina phenomenon in 2016 causes the intensity of rainfall in the dry season to be quite high. However, the intensity values continued to show a significant change between dry and rainy seasons. The area of low landslide hazard changed significantly for low rainfall intensity (July 2016) and high intensity in April 2017. The total area of landslide hazard in April 2017 was 1.09 and 0.82 times more massive than in August 2016 for high and moderate potential hazards, respectively. Based on the characteristic of rainfall that change frequently and water as the primary trigger of the landslide, in determining the potential for landslides, rainfall factors need to be considered more detailed.},
   issn = {2088-5334},
   publisher = {INSIGHT - Indonesian Society for Knowledge and Human Development},
   url = {http://ijaseit.insightsociety.org/index.php?option=com_content&view=article&id=9&Itemid=1&article_id=6876},
   doi = {10.18517/ijaseit.10.1.6876}
}

EndNote

%A Jaelani, Lalu Muhamad
%A Fahlefi, Rizha
%A Khoiri, Mohammad
%A Nur Rochman, Juan Pandu Gya
%D 2020
%T The Rainfall Effect Analysis of Landslide Occurrence on Mount Slopes of Wilis
%B 2020
%9 landslides hazard; La Nina; Mount Wilis; rainfall effect.
%! The Rainfall Effect Analysis of Landslide Occurrence on Mount Slopes of Wilis
%K landslides hazard; La Nina; Mount Wilis; rainfall effect.
%X Water is a significant factor in the occurrence of landslides when rainwater absorbs into the impermeable layer of soil and causes the soil to experience weathering; thus, that the soil is not strong enough to withstand the water load. Therefore, rainfall, as well as a land slope that affects the acceleration of runoff, becomes an important indicator that affects the potential for landslides. In this research, the effect of rainfall intensity on landslide was analyzed based on monthly data collected from 81 rain gauge stations. This idea was an effort to support research related to landslides mapping on the steep area. Thus, the analysis of potential landslides that vary according to rainfall changes monthly was obtained. La Nina phenomenon in 2016 causes the intensity of rainfall in the dry season to be quite high. However, the intensity values continued to show a significant change between dry and rainy seasons. The area of low landslide hazard changed significantly for low rainfall intensity (July 2016) and high intensity in April 2017. The total area of landslide hazard in April 2017 was 1.09 and 0.82 times more massive than in August 2016 for high and moderate potential hazards, respectively. Based on the characteristic of rainfall that change frequently and water as the primary trigger of the landslide, in determining the potential for landslides, rainfall factors need to be considered more detailed.
%U http://ijaseit.insightsociety.org/index.php?option=com_content&view=article&id=9&Itemid=1&article_id=6876
%R doi:10.18517/ijaseit.10.1.6876
%J International Journal on Advanced Science, Engineering and Information Technology
%V 10
%N 1
%@ 2088-5334

IEEE

Lalu Muhamad Jaelani,Rizha Fahlefi,Mohammad Khoiri and Juan Pandu Gya Nur Rochman,"The Rainfall Effect Analysis of Landslide Occurrence on Mount Slopes of Wilis," International Journal on Advanced Science, Engineering and Information Technology, vol. 10, no. 1, pp. 298-303, 2020. [Online]. Available: http://dx.doi.org/10.18517/ijaseit.10.1.6876.

RefMan/ProCite (RIS)

TY  - JOUR
AU  - Jaelani, Lalu Muhamad
AU  - Fahlefi, Rizha
AU  - Khoiri, Mohammad
AU  - Nur Rochman, Juan Pandu Gya
PY  - 2020
TI  - The Rainfall Effect Analysis of Landslide Occurrence on Mount Slopes of Wilis
JF  - International Journal on Advanced Science, Engineering and Information Technology; Vol. 10 (2020) No. 1
Y2  - 2020
SP  - 298
EP  - 303
SN  - 2088-5334
PB  - INSIGHT - Indonesian Society for Knowledge and Human Development
KW  - landslides hazard; La Nina; Mount Wilis; rainfall effect.
N2  - Water is a significant factor in the occurrence of landslides when rainwater absorbs into the impermeable layer of soil and causes the soil to experience weathering; thus, that the soil is not strong enough to withstand the water load. Therefore, rainfall, as well as a land slope that affects the acceleration of runoff, becomes an important indicator that affects the potential for landslides. In this research, the effect of rainfall intensity on landslide was analyzed based on monthly data collected from 81 rain gauge stations. This idea was an effort to support research related to landslides mapping on the steep area. Thus, the analysis of potential landslides that vary according to rainfall changes monthly was obtained. La Nina phenomenon in 2016 causes the intensity of rainfall in the dry season to be quite high. However, the intensity values continued to show a significant change between dry and rainy seasons. The area of low landslide hazard changed significantly for low rainfall intensity (July 2016) and high intensity in April 2017. The total area of landslide hazard in April 2017 was 1.09 and 0.82 times more massive than in August 2016 for high and moderate potential hazards, respectively. Based on the characteristic of rainfall that change frequently and water as the primary trigger of the landslide, in determining the potential for landslides, rainfall factors need to be considered more detailed.
UR  - http://ijaseit.insightsociety.org/index.php?option=com_content&view=article&id=9&Itemid=1&article_id=6876
DO  - 10.18517/ijaseit.10.1.6876

RefWorks

RT Journal Article
ID 6876
A1 Jaelani, Lalu Muhamad
A1 Fahlefi, Rizha
A1 Khoiri, Mohammad
A1 Nur Rochman, Juan Pandu Gya
T1 The Rainfall Effect Analysis of Landslide Occurrence on Mount Slopes of Wilis
JF International Journal on Advanced Science, Engineering and Information Technology
VO 10
IS 1
YR 2020
SP 298
OP 303
SN 2088-5334
PB INSIGHT - Indonesian Society for Knowledge and Human Development
K1 landslides hazard; La Nina; Mount Wilis; rainfall effect.
AB Water is a significant factor in the occurrence of landslides when rainwater absorbs into the impermeable layer of soil and causes the soil to experience weathering; thus, that the soil is not strong enough to withstand the water load. Therefore, rainfall, as well as a land slope that affects the acceleration of runoff, becomes an important indicator that affects the potential for landslides. In this research, the effect of rainfall intensity on landslide was analyzed based on monthly data collected from 81 rain gauge stations. This idea was an effort to support research related to landslides mapping on the steep area. Thus, the analysis of potential landslides that vary according to rainfall changes monthly was obtained. La Nina phenomenon in 2016 causes the intensity of rainfall in the dry season to be quite high. However, the intensity values continued to show a significant change between dry and rainy seasons. The area of low landslide hazard changed significantly for low rainfall intensity (July 2016) and high intensity in April 2017. The total area of landslide hazard in April 2017 was 1.09 and 0.82 times more massive than in August 2016 for high and moderate potential hazards, respectively. Based on the characteristic of rainfall that change frequently and water as the primary trigger of the landslide, in determining the potential for landslides, rainfall factors need to be considered more detailed.
LK http://ijaseit.insightsociety.org/index.php?option=com_content&view=article&id=9&Itemid=1&article_id=6876
DO  - 10.18517/ijaseit.10.1.6876