Abstract

Investigating surface displacements in high alpine environments is often subject to challenges due to the difficult accessibility or harsh climatic conditions. Measurement systems have improved greatly in recent years regarding accuracy, range, or energy consumption. Continuously receiving high-precision, real-time monitoring data from a remote location can still support a better understanding of slope dynamics and risk. We present the design, construction, operation, and performance of a complex surface displacement monitoring system installed in the surroundings of the Great Aletsch Glacier in the Swiss Alps, based on two robotic total stations to continuously measure 3D displacements with high accuracies. In addition, GNSS stations are also considered in order to pass from a local to a geographic reference system, as well as to improve the measurement accuracy. The monitoring network is aimed at studying several types of deformation processes, i.e., (i) gravitationally driven and irreversible rockslide movements around the tongue of the Great Aletsch Glacier, (ii) reversible rock slope deformations caused by annual cycles of groundwater recharge and depletion, and (iii) small irreversible deformations of stable rock slopes resulting from progressive rock damage driven by glacier retreat and cyclic hydraulic and thermal loading. We describe the technical details of the monitoring system, which has been in operation successfully for 6 years, and discuss the system performance in terms of its robustness and accuracy.

Highlights

  • This paper describes an exceptional monitoring infrastructure developed and successfully operated for 6 years (2014–2020) in the framework of a large research project focusing on paraglacial rock slope movements and landslide activity

  • A large data set has been recorded using the described monitoring system installed at Chatzulecher (TPS1) and Driest (TPS2) since 2014

  • A high-precision total station monitoring system installed in the surroundings of the glacial tongue of the Great Aletsch Glacier in Switzerland was described in great detail

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Summary

Introduction

The continuous and accurate monitoring of surface displacements in high alpine regions is challenging due to the extreme weather conditions, long snowfall periods, snow creep and avalanches, and rock falls. These data are crucial to investigating the complexities of the slope processes, such as those occurring in glacial and paraglacial environments, where only a few studies have been performed to date [1,2,3,4]. Selected monitoring results are presented in order to document and analyze the reliability and accuracy of the system, both in terms of the small reversible ground surface deformations and the large rapid gravitational slope movements

Study Area
Monitoring Setup
TPS Pillars
Protection of the TPS from Environmental Impacts
TPS Network Management
Data Processing
Results
Measurement Precision
Reversible Displacements at Stable Slopes
Discussion and Conclusions
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