Characterising spectral, spatial and morphometric properties of landslides for semi-automatic detection using object-oriented methods

Recognition and classification of landslides is a critical requirement in pre- and post-disaster hazard analysis. This has been primarily done through field mapping or manual image interpretation. However, image interpretation can also be done semi-automatically by creating a routine in object-based...

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Veröffentlicht in:Geomorphology (Amsterdam, Netherlands) Netherlands), 2010-03, Vol.116 (1), p.24-36
Hauptverfasser: Martha, Tapas R., Kerle, Norman, Jetten, Victor, van Westen, Cees J., Kumar, K. Vinod
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container_start_page 24
container_title Geomorphology (Amsterdam, Netherlands)
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creator Martha, Tapas R.
Kerle, Norman
Jetten, Victor
van Westen, Cees J.
Kumar, K. Vinod
description Recognition and classification of landslides is a critical requirement in pre- and post-disaster hazard analysis. This has been primarily done through field mapping or manual image interpretation. However, image interpretation can also be done semi-automatically by creating a routine in object-based classification using the spectral, spatial and morphometric properties of landslides, and by incorporating expert knowledge. This is a difficult task since a fresh landslide has spectral properties that are nearly identical to those of other natural objects, such as river sand and rocky outcrops, and they also do not have unique shapes. This paper investigates the use of a combination of spectral, shape and contextual information to detect landslides. The algorithm is tested with a 5.8 m multispectral data from Resourcesat-1 and a 10 m digital terrain model generated from 2.5 m Cartosat-1 imagery for an area in the rugged Himalayas in India. It uses objects derived from the segmentation of a multispectral image as classifying units for object-oriented analysis. Spectral information together with shape and morphometric characteristics was used initially to separate landslides from false positives. Objects recognised as landslides were subsequently classified based on material type and movement as debris slides, debris flows and rock slides, using adjacency and morphometric criteria. They were further classified for their failure mechanism using terrain curvature. The procedure was developed for a training catchment and then applied without further modification on an independent catchment. A total of five landslide types were detected by this method with 76.4% recognition and 69.1% classification accuracies. This method detects landslides relatively quickly, and hence has the potential to aid risk analysis, disaster management and decision making processes in the aftermath of an earthquake or an extreme rainfall event.
doi_str_mv 10.1016/j.geomorph.2009.10.004
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subjects Applied geophysics
Disaster management
Earth sciences
Earth, ocean, space
Engineering and environment geology. Geothermics
Exact sciences and technology
Internal geophysics
Landslide characterisation
Marine and continental quaternary
Natural hazards: prediction, damages, etc
Object-oriented analysis
Segmentation
Semi-automatic detection
Surficial geology
The Himalayas
title Characterising spectral, spatial and morphometric properties of landslides for semi-automatic detection using object-oriented methods
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