Abstract

Abstract. This contribution discusses the accuracy and the applicability of Photogrammetric point clouds based on dense image matching for the monitoring of gravitational mass movements caused by crevices. Four terrestrial image sequences for three different time epochs have been recorded and oriented using ground control point in a local reference frame. For the first epoch, two sequences are recorded, one in the morning and one in the afternoon to evaluate the noise level within the point clouds for a static geometry and changing light conditions. The second epoch is recorded a few months after the first epoch where also no significant change has occurred in between. The third epoch is recorded after one year with changes detected. As all point clouds are given in the same local coordinate frame and thus are co-registered via the ground control points, change detection is based on calculating the Multiscale-Model-to-Model-Cloud distances (M3C2) of the point clouds. Results show no movements for the first year, but identify significant movements comparing the third epoch taken in the second year. Besides the noise level estimation, the quality checks include the accuracy of the camera orientations based on ground control points, the covariances of the bundle adjustment, and a comparison the Geodetic measurements of additional control points and a laser scanning point cloud of a part of the crevice. Additionally, geological measurements of the movements have been performed using extensometers.

Highlights

  • One of the direct consequences of climate change is the melting of permafrost in alpine areas

  • Several groups from geology, geodesy and photogrammetry were working on the summit and installing ground control points and equipment

  • The results for the 3D object coordinates estimated in the bundle adjustment shows that the standard deviation of the points is below 1 cm in the center of the image set and gets worse to the borders of the set. This is mainly caused by the lower number of images that see these points and by the configuration of the ground control points

Read more

Summary

Introduction

One of the direct consequences of climate change is the melting of permafrost in alpine areas. Hungr et al (2014) classifies five different movement types: fall, topple, slide, spread, and flow. An important task in predicting these mass movements is the classification of the movement type based on a set of indicators. This classification needs a detailed observation of movements. Observing the movement rate and direction of single points over time is not sufficient to model complex changes. This modeling requires the observation of a various number of 3D points for longer time periods and leads to a classification of the movement type and an estimation of possible moving masses

Methods
Results
Conclusion
Full Text
Published version (Free)

Talk to us

Join us for a 30 min session where you can share your feedback and ask us any queries you have

Schedule a call