2016
DOI: 10.5194/nhess-16-2769-2016
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Assessing population exposure for landslide risk analysis using dasymetric cartography

Abstract: Abstract. Assessing the number and locations of exposed people is a crucial step in landslide risk management and emergency planning. The available population statistical data frequently have insufficient detail for an accurate assessment of potentially exposed people to hazardous events, mainly when they occur at the local scale, such as with landslides. The present study aims to apply dasymetric cartography to improving population spatial resolution and to assess the potentially exposed population. An additi… Show more

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Cited by 27 publications
(17 citation statements)
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“…In order to assess the exposure of the population and the buildings, the resident population of each BGRI subsection provided by the census of the INE was considered, as well as the buildings location that was provided in vector format by the Loures Municipality (Direcção de Projecto do Plano Director Municipal, or DPPDM). Because the number of residents per building was not available, the resident population per BGRI was distributed into each residential building of the BGRI by dasymetric mapping in function of the area of each building [44], in order to estimate the number of residents in each susceptibility class and in each combined vulnerability class. In addition, the physical vulnerability calculated for each BGRI unit was ascribed for the total buildings existing in the BGRI.…”
Section: Landslide Risk Analysismentioning
confidence: 99%
“…In order to assess the exposure of the population and the buildings, the resident population of each BGRI subsection provided by the census of the INE was considered, as well as the buildings location that was provided in vector format by the Loures Municipality (Direcção de Projecto do Plano Director Municipal, or DPPDM). Because the number of residents per building was not available, the resident population per BGRI was distributed into each residential building of the BGRI by dasymetric mapping in function of the area of each building [44], in order to estimate the number of residents in each susceptibility class and in each combined vulnerability class. In addition, the physical vulnerability calculated for each BGRI unit was ascribed for the total buildings existing in the BGRI.…”
Section: Landslide Risk Analysismentioning
confidence: 99%
“…The estimated population density map appears to have a more scattered pattern than other population maps that use a single ancillary variable. This is because a large number of classes from all the layers can be mixed and considered to judge the population distribution through the disaggregation process within the multi-layer multi-class approach (6,8,16 classes for slope, altitude, and land use, respectively). Also, it should be noted that this dasymetric mapping represents the fine-grain division of hilly area population disaggregation by preserving the pycnophylactic property of population mapping [52], which maintains the same total population in each source zone.…”
Section: Results For Hilly Area Dasymetric Mappingmentioning
confidence: 99%
“…Accurate mapping of population distribution has become very important in a variety of applications, such as urban and regional planning, disaster management, resources and facility allocation, risk-assessment, and socioeconomic development policy [1][2][3][4][5][6][7][8][9][10][11][12]. This is particularly true for developing countries with a rapid population growth and inaccurate or unavailable census data.…”
Section: Introductionmentioning
confidence: 99%
“…Existing literature proposed a multi‐indicator analysis based on the demographic data in administrative units, such as provinces or municipalities, to estimate the exposure of elements at risk to landslide by incorporating the landslide susceptibility or frequency of landslides occurrence within the same areas (Gariano et al., 2017; Martha et al., 2021). Several studies used dasymetric mapping procedures to refine the estimation of the spatial distribution of elements at risk to provide comparatively fine‐scaled estimations of landslide exposure (Emberson et al., 2021; Garcia et al., 2016; Pellicani et al., 2014; Santangelo et al., 2021). Efforts have attempted to estimate landslide exposure at continental or global scales (Emberson et al., 2020; Schlögl & Matulla, 2018).…”
Section: Introductionmentioning
confidence: 99%