4.6 Article

Effects of different land use and land cover data on the landslide susceptibility zonation of road networks

Journal

NATURAL HAZARDS AND EARTH SYSTEM SCIENCES
Volume 19, Issue 3, Pages 471-487

Publisher

COPERNICUS GESELLSCHAFT MBH
DOI: 10.5194/nhess-19-471-2019

Keywords

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Funding

  1. FCT-Portuguese Foundation for Science and Technology, I.P. [PTDC/GES-AMB/30052/2017]
  2. Centre for Geographical Studies [UID/GEO/00295/2013]
  3. Institute of Geography and Spatial Planning and Universidade de Lisboa, IGOT-UL (BD2015)
  4. Fundação para a Ciência e a Tecnologia [PTDC/GES-AMB/30052/2017] Funding Source: FCT

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This work evaluates the influence of land use and land cover (LUC) data with different properties on the landslide susceptibility zonation of the road network in the Zezere watershed (Portugal). The information value method was used to assess the landslide susceptibility using two models: one including detailed LUC data (the Portuguese Land Cover Map - COS) and the other including more generalized LUC data (the CORINE Land Cover - CLC). A set of fixed independent layers was considered as landslide predisposing factors (slope angle, slope aspect, slope curvature, slope-over-area ratio, soil, and lithology) while COS and CLC were used to find the differences in the landslide susceptibility zonation. A landslide inventory was used as a dependent layer, including 259 shallow landslides obtained from the photointerpretation of orthophotos from 2005, and further validated in three sample areas. The landslide susceptibility maps were assigned to the road network data and resulted in two landslide susceptibility road network maps. The models' performance was evaluated with prediction and success rate curves and the area under the curve (AUC). The landslide susceptibility results obtained in the two models present a high accuracy in terms of the AUC (>90 %), but the model with more detailed LUC data (COS) produces better results in the landslide susceptibility zonation on the road network with the highest landslide susceptibility.

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