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Semi-automatic approach for identifying locations of shallow debris slides/flows based on lidar-derived morphological features

机译:基于激光雷达的形态特征识别浅层碎片幻灯片/流的位置的半自动方法

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摘要

Identification of landslides at the regional scale has always been a challenging problem. Various automatic landslide identification methods, mainly relying on spectral information from aerial photographs or satellite imagery, have been developed. This paper proposes a semi-automatic approach to identify locations of small-sized shallow debris slides and flows using airborne lidar (light detection and ranging) data. Cells related to landslide components were first extracted by using a new method based on local Moran's 1 (LMI). Subsequently, cell clusters representing landslide components and other terrain objects were discriminated through geometric and contextual analysis at cluster level. The approach was tested in a study area in Hong Kong and the identification result was verified by a landslide inventory. Locations of 93.5% of recent landslides and 23.8% of old landslides were identified by the proposed approach. The result indicates that the proposed approach is able to identify both recent and old landslides with distinct morphological features. However, the proposed approach also identified a large number of locations (77.6% of all locations) unrelated to landslides. These locations may correspond to terrain objects with similar morphology to debris slides or flows, and indicate rough terrain in the study area. In addition, the effects of DEM (digital elevation model) resolution on landslide identification were analysed by applying the LMI-based method to digital elevation models (DEMs) at different resolutions. The results indicate that the smoothing effect caused by lowering DEM resolution led to extraction of fewer landslide components.
机译:在区域范围内识别滑坡一直是一个具有挑战性的问题。已经开发了主要依靠航空照片或卫星图像的光谱信息的各种自动滑坡识别方法。本文提出了一种半自动方法,可使用机载激光雷达(光检测和测距)数据来识别小型浅层碎片滑道和流动的位置。首先使用基于局部Moran's 1(LMI)的新方法提取与滑坡成分有关的单元格。随后,通过几何和上下文分析在聚类水平上区分了代表滑坡成分和其他地形对象的细胞聚类。该方法在香港的一个研究区域进行了测试,并通过滑坡清单验证了识别结果。拟议的方法确定了近期滑坡的93.5%和旧滑坡的23.8%的位置。结果表明,所提出的方法能够识别具有不同形态特征的新近滑坡和旧滑坡。但是,建议的方法还确定了大量与滑坡无关的位置(占所有位置的77.6%)。这些位置可能对应于具有与碎片滑坡或流动相似的形态的地形对象,并指示研究区域中的崎terrain地形。此外,通过将基于LMI的方法应用于不同分辨率的数字高程模型(DEM),分析了DEM(数字高程模型)分辨率对滑坡识别的影响。结果表明,由降低DEM分辨率引起的平滑效果导致提取了更少的滑坡分量。

著录项

  • 来源
    《International journal of remote sensing》 |2014年第10期|3741-3763|共23页
  • 作者

    Susu Deng; Wenzhong Shi;

  • 作者单位

    Department of Land Surveying and Geoinformatics, The Hong Kong Polytechnic University, Kowloon, Hong Kong;

    Department of Land Surveying and Geoinformatics, The Hong Kong Polytechnic University, Kowloon, Hong Kong;

  • 收录信息 美国《科学引文索引》(SCI);美国《工程索引》(EI);
  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类
  • 关键词

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