Abstract

Airborne laser scans present an optimal tool to describe geomorphological features in natural environments. However, a challenge arises in the detection of such phenomena, as they are embedded in the topography, tend to blend into their surroundings and leave only a subtle signature within the data. Most object-recognition studies address mainly urban environments and follow a general pipeline where the data are partitioned into segments with uniform properties. These approaches are restricted to man-made domain and are capable to handle limited features that answer a well-defined geometric form. As natural environments present a more complex set of features, the common interpretation of the data is still manual at large. In this paper, we propose a data-aware detection scheme, unbound to specific domains or shapes. We define the recognition question as an energy optimization problem, solved by variational means. Our approach, based on the level-set method, characterizes geometrically local surfaces within the data, and uses these characteristics as potential field for minimization. The main advantage here is that it allows topological changes of the evolving curves, such as merging and breaking. We demonstrate the proposed methodology on the detection of collapse sinkholes.

Highlights

  • Airborne laser scanning technology offers detailed description of landforms and surface variability

  • We present in this paper an autonomous detection model, and demonstrate it on collapse sinkholes using airborne laser scanning data

  • The application of the proposed detection methodology is demonstrated on high-resolution airborne laser scanning data along the Dead-Sea coast whose ongoing desiccation has triggered a range of dramatic geomorphic processes, among them are the incision of gullies and rapid development collapse sinkholes

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Summary

INTRODUCTION

Airborne laser scanning technology offers detailed description of landforms and surface variability It provides an excellent means for measuring and monitoring morphological changes across a variety of spatial scales. Civico et al (2015) carry morphotectonic analysis via airborne laser scan-based DEMs. Topographic profiles between the basin floor and the highest footwall surfaces are constructed, according to a best-displaced geomorphic marker (an identifiable feature that has been displaced). Filin and Baruch (2010) and Baruch and Filin (2011) suggested an energy-based detection, where dominant concave areas were first detected via curvature maps, according to which the curve was to propagate It required a good initialization of the sinkhole boundary.

DETECTION
ANALYSIS AND DISCUSSION
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