4.7 Article

A Semi-Automated Object-Based Approach for Landslide Detection Validated by Persistent Scatterer Interferometry Measures and Landslide Inventories

期刊

REMOTE SENSING
卷 4, 期 5, 页码 1310-1336

出版社

MDPI AG
DOI: 10.3390/rs4051310

关键词

object-based image analysis (OBIA); landslide mapping; persistent scatterers (PS); radar-interpretation; validation

资金

  1. European Community's Seventh Framework Programme under the SAFER (Services and Applications For Emergency Response) project [218802]
  2. Natural Environment Research Council [bgs05008] Funding Source: researchfish
  3. NERC [bgs05008] Funding Source: UKRI

向作者/读者索取更多资源

Geoinformation derived from Earth observation (EO) plays a key role for detecting, analyzing and monitoring landslides to assist hazard and risk analysis. Within the framework of the EC-GMES-FP7 project SAFER (Services and Applications For Emergency Response) a semi-automated object-based approach for landslide detection and classification has been developed. The method was applied to a case study in North-Western Italy using SPOT-5 imagery and a digital elevation model (DEM), including its derivatives slope, aspect, curvature and plan curvature. For the classification in the object-based environment spectral, spatial and morphological properties as well as context information were used. In a first step, landslides were classified on a coarse segmentation level to separate them from other features with similar spectral characteristics. Thereafter, the classification was refined on a finer segmentation level, where two categories of mass movements were differentiated: flow-like landslides and other landslide types. In total, an area of 3.77 km(2) was detected as landslide-affected area, 1.68 km(2) were classified as flow-like landslides and 2.09 km(2) as other landslide types. The outcomes were compared to and validated by pre-existing landslide inventory data (IFFI and PAI) and an interpretation of PSI (Persistent Scatterer Interferometry) measures derived from ERS1/2, ENVISAT ASAR and RADARSAT-1 data. The spatial overlap of the detected landslides and existing landslide inventories revealed 44.8% (IFFI) and 50.4% (PAI), respectively. About 32% of the polygons identified through OBIA are covered by persistent scatterers data.

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