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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2015-10-01
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Series: | Geographica Helvetica |
Online Access: | http://www.geogr-helv.net/70/265/2015/gh-70-265-2015.pdf |
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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 |
work_keys_str_mv |
AT cwilli methodsfordetectingchannelbedsurfacechangesinamountaintorrentexperiencesfromthedorfbachtorrent AT cgraf methodsfordetectingchannelbedsurfacechangesinamountaintorrentexperiencesfromthedorfbachtorrent AT ydeubelbeiss methodsfordetectingchannelbedsurfacechangesinamountaintorrentexperiencesfromthedorfbachtorrent AT mkeiler methodsfordetectingchannelbedsurfacechangesinamountaintorrentexperiencesfromthedorfbachtorrent |
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