Abstract

In order to lower the risks of large-scale landslides and improve community resilience in Taiwan, a long-term project has been promoted by the Soil and Water Conservation Bureau since 2017. In this study, methods to build an emergency response framework including hazard mapping and early warning system establishment were introduced. For hazard mapping, large-scale landslides were categorized into a landslide, debris flow, or landslide dam type based on the movement of unstable materials and topography. Each disaster type has different hazard zone delineation methods to identify the affected areas. After establishing the possible effected areas, early warning mechanisms, including warning value using rainfall as the indicator and evacuation procedures, should be created for emergency response. To set the warning value, analysis of the occurrence thresholds of previous existing large-scale landslides was conducted to determine the critical rainfall and further utilized to set the warning value considering the evacuation time for the locals. Finally, for integration with the current debris flow emergency response system, potential large-scale landslide areas were further divided into two types based on their spatial relationship with debris flows. For those overlapping with existing debris flow protected targets, the current emergency response system was upgraded considering the impact of large-scale landslides, while the others were suggested for use in building a new emergency response procedure. This integrated framework could provide a feasible risk avoidance method for local government and residents.

Highlights

  • Landslide disasters have happened frequently under climate change, causing serious property losses and casualties

  • Among all the disasters induced by Typhoon Morakot, Hsiaolin Village was attacked by a large-scale landslide causing more than 400 casualties, and half of the village was ruined

  • Large-scale landslides that occurred in Xiaolin Village (Figure 13a) were used to examine the effectiveness of the method

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Summary

Introduction

Landslide disasters have happened frequently under climate change, causing serious property losses and casualties. High-risk/low-frequency events like large-scale landslides have become more common internationally under extreme climate such as the disasters in Kii Peninsula in Japan, 2011 [1], and the Oso landslide in the U.S, 2014 [2]. In 2009, Typhoon Morakot, with more than 3000 mm rainfall, induced one of the most serious disasters in the history of Taiwan. Various landslide disasters, such as shallow landslides, debris flows, large-scale landslides, and landslide dams, occurred during the typhoon and caused hundreds of deaths [3,4]. Among all the disasters induced by Typhoon Morakot, Hsiaolin Village was attacked by a large-scale landslide causing more than 400 casualties, and half of the village was ruined. Post-disaster recovery was a great challenge as the large-scale landslide had devastated the village and paralyzed local infrastructures and access roads

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