Nat. Hazards Earth Syst. Sci., 18, 687–708, 2018 https://doi.org/10.5194/nhess-18-687-2018 © Author(s) 2018. This work is distributed under the Creative Commons Attribution 4.0 License. Scale and spatial distribution assessment of rainfall-induced landslides in a catchment with mountain roads Chih-Ming Tseng1, Yie-Ruey Chen1, and Szu-Mi Wu2 1Department of Land Management and Development, Chang Jung Christian University, Tainan, 71101, Taiwan (ROC) 2Chen-Du Construction Limited, Taoyuan, 33059, Taiwan (ROC) Correspondence: Chih-Ming Tseng (
[email protected]) Received: 14 July 2017 – Discussion started: 4 October 2017 Revised: 27 December 2017 – Accepted: 22 January 2018 – Published: 2 March 2018 Abstract. This study focused on landslides in a catchment Landslide susceptibility can be evaluated by analysing the with mountain roads that were caused by Nanmadol (2011) relationships between landslides and various factors that are and Kong-rey (2013) typhoons. Image interpretation tech- responsible for the occurrence of landslides (Brabb, 1984; niques were employed to for satellite images captured before Guzzetti et al., 1999, 2005). In general, the factors that af- and after the typhoons to derive the surface changes. A mul- fect landslides include predisposing factors (e.g. geology, to- tivariate hazard evaluation method was adopted to establish pography, and hydrology) and triggering factors (e.g. rainfall, a landslide susceptibility assessment model. The evaluation earthquakes, and anthropogenic factors) (Chen et al., 2013a, of landslide locations and relationship between landslide and b; Chue et al., 2015). Geological factors include lithological predisposing factors is preparatory for assessing and map- factors, structural conditions, and soil thickness; topograph- ping landslide susceptibility.