Combination of UAV and terrestrial photogrammetry to assess rapid glacier evolution and map glacier hazards
Tourists and hikers visiting glaciers all year round face hazards such as sudden terminus collapses, typical of such a dynamically evolving environment. In this study, we analyzed the potential of different survey techniques to analyze hazards of the Forni Glacier, an important geosite located i...
Main Authors: | , , , , , , , |
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Format: | Article |
Language: | English |
Published: |
Copernicus Publications
2018-04-01
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Series: | Natural Hazards and Earth System Sciences |
Online Access: | https://www.nat-hazards-earth-syst-sci.net/18/1055/2018/nhess-18-1055-2018.pdf |
Summary: | Tourists and hikers visiting glaciers all year round face hazards such as
sudden terminus collapses, typical of such a dynamically evolving
environment. In this study, we analyzed the potential of different survey
techniques to analyze hazards of the Forni Glacier, an important geosite
located in Stelvio Park (Italian Alps). We carried out surveys in the
2016 ablation season and compared point clouds generated from an unmanned aerial
vehicle (UAV) survey, close-range photogrammetry and terrestrial laser
scanning (TLS). To investigate the evolution of glacier hazards and evaluate
the glacier thinning rate, we also used UAV data collected in 2014 and a
digital elevation model (DEM) created from an aerial photogrammetric survey
of 2007. We found that the integration between terrestrial and UAV
photogrammetry is ideal for mapping hazards related to the glacier collapse,
while TLS is affected by occlusions and is logistically complex in glacial
terrain. Photogrammetric techniques can therefore replace TLS for glacier
studies and UAV-based DEMs hold potential for becoming a standard tool in
the investigation of glacier thickness changes. Based on our data sets, an
increase in the size of collapses was found over the study period, and the
glacier thinning rates went from 4.55 ± 0.24 m a<sup>−1</sup> between 2007
and 2014 to 5.20 ± 1.11 m a<sup>−1</sup> between 2014 and 2016. |
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ISSN: | 1561-8633 1684-9981 |