In: Journal of Applied Geodesy, 2017, vol. 11, no. 2, p. 89-98
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In: Geophysical Research Letters, 2020, vol. 47, no. 2, p. e2019GL085578
Glaciers in the European Alps rapidly lose mass to adapt to changes in climate conditions. Here, we investigate the relationship and lag between climate forcing and geometric glacier response with a regional glacier evolution model accounting for ice dynamics. The volume loss occurring as a result of the glacier‐climate imbalance increased over the early 21st century, from about 35% in...
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In: Remote Sensing, 2020, vol. 12, no. 3, p. 559
Active rock glaciers represent the best visual expression of mountain permafrost that can be mapped and monitored directly using remotely sensed data. Active rock glaciers are bodies that consist of a perennially frozen ice/rock mixture and express a distinct flow-like morphology indicating downslope permafrost creep movement. Annual rates of motion have ranged from a few millimeters to...
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In: Remote Sensing Letters, 2019, vol. 10, no. 1, p. 11–20
In geomorphology, PhotoScan is a software that is used to produce Digital Surface Models (DSMs). It constructs 3D environments from 2D imagery (often taken by Unmanned Aerial Vehicles (UAV)) based on Structure-from-Motion (SfM) and Multi- View Stereo (MVS) principles. However, unpublished computer-vision algorithms used, contain random elements which can affect the accuracy of the outputs. For...
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In: Trees, 2013, vol. 27, no. 1, p. 111-121
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In: Applied Physics A, 2004, vol. 79, no. 4-6, p. 1215-1218
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In: Boundary-Layer Meteorology, 2008, vol. 127, no. 3, p. 449-467
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In: Journal of Geodesy, 2012, vol. 86, no. 4, p. 257-270
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In: GeoInformatica, 2008, vol. 12, no. 1, p. 73-89
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In: Boundary-Layer Meteorology, 2013, vol. 147, no. 3, p. 401-419
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