Abstract

Abstract. The assessment of the physical vulnerability of elements at risk as part of the risk analysis is an essential aspect for the development of strategies and structural measures for risk reduction. Understanding, analysing and, if possible, quantifying physical vulnerability is a prerequisite for designing strategies and adopting tools for its reduction. The most common methods for assessing physical vulnerability are vulnerability matrices, vulnerability curves and vulnerability indicators; however, in most of the cases, these methods are used in a conflicting way rather than in combination. The article focuses on two of these methods: vulnerability curves and vulnerability indicators. Vulnerability curves express physical vulnerability as a function of the intensity of the process and the degree of loss, considering, in individual cases only, some structural characteristics of the affected buildings. However, a considerable amount of studies argue that vulnerability assessment should focus on the identification of these variables that influence the vulnerability of an element at risk (vulnerability indicators). In this study, an indicator-based methodology (IBM) for mountain hazards including debris flow (Kappes et al., 2012) is applied to a case study for debris flows in South Tyrol, where in the past a vulnerability curve has been developed. The relatively "new" indicator-based method is being scrutinised and recommendations for its improvement are outlined. The comparison of the two methodological approaches and their results is challenging since both methodological approaches deal with vulnerability in a different way. However, it is still possible to highlight their weaknesses and strengths, show clearly that both methodologies are necessary for the assessment of physical vulnerability and provide a preliminary "holistic methodological framework" for physical vulnerability assessment showing how the two approaches may be used in combination in the future.

Highlights

  • Climate and environmental change are expected to alter the patterns of risk in mountain areas

  • The most common method for assessing vulnerability is the development of vulnerability curves that often ignore the characteristics of the buildings, especially when the type of hazard under investigation affects a limited amount of buildings, focusing mainly on the intensity of the process and the corresponding loss

  • The spatial distribution of damage and intensity data used for the development of vulnerability curves is not often displayed on a map, this would be simple with the use of GIS

Read more

Summary

Introduction

Climate and environmental change are expected to alter the patterns of risk in mountain areas. The frequency, magnitude and spatial extend of natural hazards is expected to change; on the other hand, extensive development and changes in land use and land cover will certainly alter the spatial pattern of the vulnerability of the elements at risk (Fuchs et al, 2013; Mazzorana et al, 2012). The most common method for assessing vulnerability is the development of vulnerability curves that often ignore the characteristics of the buildings, especially when the type of hazard under investigation affects a limited amount of buildings (e.g. debris flow), focusing mainly on the intensity of the process and the corresponding loss.

Objectives
Methods
Results
Conclusion
Full Text
Published version (Free)

Talk to us

Join us for a 30 min session where you can share your feedback and ask us any queries you have

Schedule a call