Increasing Spatio-Temporal Resolution for Monitoring Alpine Solifluction Using Terrestrial Laser Scanners and 3D Vector Fields

This article investigates the usage of terrestrial laser scanner (TLS) point clouds for monitoring the gradual movements of soil masses due to freeze–thaw activity and water saturation, commonly referred to as solifluction. Solifluction is a geomorphic process which is characteristic for hillslopes...

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Main Authors: Christoph Holst, Jannik Janßen, Berit Schmitz, Martin Blome, Malte Dercks, Anna Schoch-Baumann, Jan Blöthe, Lothar Schrott, Heiner Kuhlmann, Tomislav Medic
Format: Article
Language:English
Published: MDPI AG 2021-03-01
Series:Remote Sensing
Subjects:
Online Access:https://www.mdpi.com/2072-4292/13/6/1192
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spelling doaj-7114ac984efa4db194d5c0dad14ee1982021-03-21T00:02:49ZengMDPI AGRemote Sensing2072-42922021-03-01131192119210.3390/rs13061192Increasing Spatio-Temporal Resolution for Monitoring Alpine Solifluction Using Terrestrial Laser Scanners and 3D Vector FieldsChristoph Holst0Jannik Janßen1Berit Schmitz2Martin Blome3Malte Dercks4Anna Schoch-Baumann5Jan Blöthe6Lothar Schrott7Heiner Kuhlmann8Tomislav Medic9Institute of Geodesy and Geoinformation, University of Bonn, 53115 Bonn, GermanyInstitute of Geodesy and Geoinformation, University of Bonn, 53115 Bonn, GermanyInstitute of Geodesy and Geoinformation, University of Bonn, 53115 Bonn, GermanyInstitute of Geodesy and Geoinformation, University of Bonn, 53115 Bonn, GermanyInstitute of Geodesy and Geoinformation, University of Bonn, 53115 Bonn, GermanyDepartment of Geography, University of Bonn, 53115 Bonn, GermanyInstitute of Environmental Social Sciences and Geography, University of Freiburg, 79085 Freiburg im Breisgau, GermanyDepartment of Geography, University of Bonn, 53115 Bonn, GermanyInstitute of Geodesy and Geoinformation, University of Bonn, 53115 Bonn, GermanyInstitute of Geodesy and Geoinformation, University of Bonn, 53115 Bonn, GermanyThis article investigates the usage of terrestrial laser scanner (TLS) point clouds for monitoring the gradual movements of soil masses due to freeze–thaw activity and water saturation, commonly referred to as solifluction. Solifluction is a geomorphic process which is characteristic for hillslopes in (high-)mountain areas, primarily alpine periglacial areas and the arctic. The movement can reach millimetre-to-centimetre per year velocities, remaining well below the typical displacement mangitudes of other frequently monitored natural objects, such as landslides and glaciers. Hence, a better understanding of solifluction processes requires increased spatial and temporal resolution with relatively high measurement accuracy. To that end, we developed a workflow for TLS point cloud processing, providing a 3D vector field that can capture soil mass displacement due to solifluction with high fidelity. This is based on the common image-processing techniques of feature detection and tracking. The developed workflow is tested on a study area placed in Hohe Tauern range of the Austrian Alps with a prominent assemblage of solifluction lobes. The derived displacements were compared with the established geomonitoring approach with total station and signalized markers and point cloud deformation monitoring approaches. The comparison indicated that the achieved results were in the same accuracy range as the established methods, with an advantage of notably higher spatial resolution. This improvement allowed for new insights considering the solifluction processes.https://www.mdpi.com/2072-4292/13/6/1192terrestrial laser scanningdeformation monitoring3D vector fieldspoint cloudschange detectiontotal station
collection DOAJ
language English
format Article
sources DOAJ
author Christoph Holst
Jannik Janßen
Berit Schmitz
Martin Blome
Malte Dercks
Anna Schoch-Baumann
Jan Blöthe
Lothar Schrott
Heiner Kuhlmann
Tomislav Medic
spellingShingle Christoph Holst
Jannik Janßen
Berit Schmitz
Martin Blome
Malte Dercks
Anna Schoch-Baumann
Jan Blöthe
Lothar Schrott
Heiner Kuhlmann
Tomislav Medic
Increasing Spatio-Temporal Resolution for Monitoring Alpine Solifluction Using Terrestrial Laser Scanners and 3D Vector Fields
Remote Sensing
terrestrial laser scanning
deformation monitoring
3D vector fields
point clouds
change detection
total station
author_facet Christoph Holst
Jannik Janßen
Berit Schmitz
Martin Blome
Malte Dercks
Anna Schoch-Baumann
Jan Blöthe
Lothar Schrott
Heiner Kuhlmann
Tomislav Medic
author_sort Christoph Holst
title Increasing Spatio-Temporal Resolution for Monitoring Alpine Solifluction Using Terrestrial Laser Scanners and 3D Vector Fields
title_short Increasing Spatio-Temporal Resolution for Monitoring Alpine Solifluction Using Terrestrial Laser Scanners and 3D Vector Fields
title_full Increasing Spatio-Temporal Resolution for Monitoring Alpine Solifluction Using Terrestrial Laser Scanners and 3D Vector Fields
title_fullStr Increasing Spatio-Temporal Resolution for Monitoring Alpine Solifluction Using Terrestrial Laser Scanners and 3D Vector Fields
title_full_unstemmed Increasing Spatio-Temporal Resolution for Monitoring Alpine Solifluction Using Terrestrial Laser Scanners and 3D Vector Fields
title_sort increasing spatio-temporal resolution for monitoring alpine solifluction using terrestrial laser scanners and 3d vector fields
publisher MDPI AG
series Remote Sensing
issn 2072-4292
publishDate 2021-03-01
description This article investigates the usage of terrestrial laser scanner (TLS) point clouds for monitoring the gradual movements of soil masses due to freeze–thaw activity and water saturation, commonly referred to as solifluction. Solifluction is a geomorphic process which is characteristic for hillslopes in (high-)mountain areas, primarily alpine periglacial areas and the arctic. The movement can reach millimetre-to-centimetre per year velocities, remaining well below the typical displacement mangitudes of other frequently monitored natural objects, such as landslides and glaciers. Hence, a better understanding of solifluction processes requires increased spatial and temporal resolution with relatively high measurement accuracy. To that end, we developed a workflow for TLS point cloud processing, providing a 3D vector field that can capture soil mass displacement due to solifluction with high fidelity. This is based on the common image-processing techniques of feature detection and tracking. The developed workflow is tested on a study area placed in Hohe Tauern range of the Austrian Alps with a prominent assemblage of solifluction lobes. The derived displacements were compared with the established geomonitoring approach with total station and signalized markers and point cloud deformation monitoring approaches. The comparison indicated that the achieved results were in the same accuracy range as the established methods, with an advantage of notably higher spatial resolution. This improvement allowed for new insights considering the solifluction processes.
topic terrestrial laser scanning
deformation monitoring
3D vector fields
point clouds
change detection
total station
url https://www.mdpi.com/2072-4292/13/6/1192
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