Landslide susceptibility mapping & prediction using Support Vector Machine for Mandakini River Basin, Garhwal Himalaya, India

被引:120
作者
Kumar, Deepak [2 ]
Thakur, Manoj [2 ]
Dubey, Chandra S. [3 ]
Shukla, Dericks P. [1 ]
机构
[1] Indian Inst Technol Mandi, Sch Engn, Mandi 175001, HP, India
[2] Indian Inst Technol Mandi, Sch Basic Sci, Mandi 175001, HP, India
[3] Univ Delhi, Ctr Adv Studies, Dept Geol, Delhi 110007, India
关键词
Landslide susceptibility mapping; Support Vector Machine (SVM); Remote sensing; GIS; Mandakini Basin; Uttarakhand; LOGISTIC-REGRESSION MODELS; ARTIFICIAL NEURAL-NETWORK; FINITE NEWTON METHOD; LESSER HIMALAYA; HAZARD ZONATION; KEDARNATH DISASTER; GIS; UTTARAKHAND; MALAYSIA; REGION;
D O I
10.1016/j.geomorph.2017.06.013
中图分类号
P9 [自然地理学];
学科分类号
0705 ; 070501 ;
摘要
In recent years, various machine learning techniques have been applied for landslide susceptibility mapping. In this study, three different variants of support vector machine viz., SVM, Proximal Support Vector Machine (PSVM) and L-2-Support Vector Machine - Modified Finite Newton (L-2-SVM-MFN) have been applied on the Mandakini River Basin in Uttarakhand, India to carry out the landslide susceptibility mapping. Eight thematic layers such as elevation, slope, aspect, drainages, geology/lithology, buffer of thrusts/faults, buffer of streams and soil along with the past landslide data were mapped in GIS environment and used for landslide susceptibility mapping in MATLAB. The study area covering 1625 km(2) has merely 0.11% of area under landslides. There are 2009 pixels for past landslides out of which 50% (1000) landslides were considered as training set while remaining 50% as testing set. The performance of these techniques has been evaluated and the computational results show that L-2-SVM-MFN obtains higher prediction values (0.829) of receiver operating characteristic curve (AUC-area under the curve) as compared to 0.807 for PSVM model and 0.79 for SVM. The results obtained from L-2-SVM-MFN model are found to be superior than other SVM prediction models and suggest the usefulness of this technique to problem of landslide susceptibility mapping where training data is very less. However, these techniques can be used for satisfactory determination of susceptible zones with these inputs.
引用
收藏
页码:115 / 125
页数:11
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