Methods for detecting channel bed surface changes in a mountain torrent – experiences from the Dorfbach torrent

The erosion of and depositions on channel bed surfaces are instrumental to understanding debris flow processes. We present an overview of existing field methods and highlight their respective advantages and disadvantages. Terrestrial laser scanning (TLS), airborne laser scanning (ALS), erosion senso...

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Main Authors: C. Willi, C. Graf, Y. Deubelbeiss, M. Keiler
Format: Article
Language:deu
Published: Copernicus Publications 2015-10-01
Series:Geographica Helvetica
Online Access:http://www.geogr-helv.net/70/265/2015/gh-70-265-2015.pdf
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spelling doaj-7cf3ad38cb464229bffc340debb2433f2020-11-24T22:54:26ZdeuCopernicus PublicationsGeographica Helvetica0016-73122194-87982015-10-0170426527910.5194/gh-70-265-2015Methods for detecting channel bed surface changes in a mountain torrent – experiences from the Dorfbach torrentC. Willi0C. Graf1Y. Deubelbeiss2M. Keiler3WSL Swiss Federal Institute for Forest, Snow and Landscape Research, Birmensdorf, SwitzerlandWSL Swiss Federal Institute for Forest, Snow and Landscape Research, Birmensdorf, SwitzerlandWSL Swiss Federal Institute for Forest, Snow and Landscape Research, Birmensdorf, SwitzerlandUniversity of Bern, Institute of Geography, Bern, SwitzerlandThe erosion of and depositions on channel bed surfaces are instrumental to understanding debris flow processes. We present an overview of existing field methods and highlight their respective advantages and disadvantages. Terrestrial laser scanning (TLS), airborne laser scanning (ALS), erosion sensors, cross sections (CS) and geomorphological mapping are compared. Additionally, two of these approaches (i.e. TLS and CS) are tested and applied in the channel reaches of the torrent catchments. The results of the comparison indicate that the methods are associated with variable temporal and spatial resolution as well as data quality and invested effort. TLS data were able to quantify small-scale variations of erosion and deposition volumes. While the same changes could be detected with CS and geomorphological mapping, it was only possible with lower precision and coarser spatial resolution. The study presents a range of potential methods that can be applied accordingly to address the objectives and to support the analyses of specific applications. The availability of erosion data, acquired mainly by TLS and ALS, in combination with debris-flow monitoring data, provides promising sources of information to further support torrent risk management.http://www.geogr-helv.net/70/265/2015/gh-70-265-2015.pdf
collection DOAJ
language deu
format Article
sources DOAJ
author C. Willi
C. Graf
Y. Deubelbeiss
M. Keiler
spellingShingle C. Willi
C. Graf
Y. Deubelbeiss
M. Keiler
Methods for detecting channel bed surface changes in a mountain torrent – experiences from the Dorfbach torrent
Geographica Helvetica
author_facet C. Willi
C. Graf
Y. Deubelbeiss
M. Keiler
author_sort C. Willi
title Methods for detecting channel bed surface changes in a mountain torrent – experiences from the Dorfbach torrent
title_short Methods for detecting channel bed surface changes in a mountain torrent – experiences from the Dorfbach torrent
title_full Methods for detecting channel bed surface changes in a mountain torrent – experiences from the Dorfbach torrent
title_fullStr Methods for detecting channel bed surface changes in a mountain torrent – experiences from the Dorfbach torrent
title_full_unstemmed Methods for detecting channel bed surface changes in a mountain torrent – experiences from the Dorfbach torrent
title_sort methods for detecting channel bed surface changes in a mountain torrent – experiences from the dorfbach torrent
publisher Copernicus Publications
series Geographica Helvetica
issn 0016-7312
2194-8798
publishDate 2015-10-01
description The erosion of and depositions on channel bed surfaces are instrumental to understanding debris flow processes. We present an overview of existing field methods and highlight their respective advantages and disadvantages. Terrestrial laser scanning (TLS), airborne laser scanning (ALS), erosion sensors, cross sections (CS) and geomorphological mapping are compared. Additionally, two of these approaches (i.e. TLS and CS) are tested and applied in the channel reaches of the torrent catchments. The results of the comparison indicate that the methods are associated with variable temporal and spatial resolution as well as data quality and invested effort. TLS data were able to quantify small-scale variations of erosion and deposition volumes. While the same changes could be detected with CS and geomorphological mapping, it was only possible with lower precision and coarser spatial resolution. The study presents a range of potential methods that can be applied accordingly to address the objectives and to support the analyses of specific applications. The availability of erosion data, acquired mainly by TLS and ALS, in combination with debris-flow monitoring data, provides promising sources of information to further support torrent risk management.
url http://www.geogr-helv.net/70/265/2015/gh-70-265-2015.pdf
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