Multitemporal terrestrial laser scanning point clouds for thaw subsidence observation at Arctic permafrost monitoring sites ...
This paper investigates different methods for quantifying thaw subsidence using terrestrial laser scanning (TLS) point clouds. Thaw subsidence is a slow (millimetre to centimetre per year) vertical displacement of the ground surface common in ice-rich permafrost-underlain landscapes. It is difficult...
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Humboldt-Universität zu Berlin
2020
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Online Access: | https://dx.doi.org/10.18452/25057 https://edoc.hu-berlin.de/handle/18452/25740 |
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ftdatacite:10.18452/25057 2024-09-15T18:11:32+00:00 Multitemporal terrestrial laser scanning point clouds for thaw subsidence observation at Arctic permafrost monitoring sites ... Anders, Katharina Marx, Sabrina Boike, Julia Herfort, Benjamin Wilcox, Evan J Langer, Moritz Marsh, Philip Höfle, Bernhard 2020 https://dx.doi.org/10.18452/25057 https://edoc.hu-berlin.de/handle/18452/25740 en eng Humboldt-Universität zu Berlin Creative Commons Attribution Non Commercial 4.0 International (CC BY-NC 4.0) Attribution-NonCommercial 4.0 International https://creativecommons.org/licenses/by-nc/4.0/legalcode cc-by-nc-4.0 change analysis 3D geoinformation ground surface displacement permafrost monitoring multitemporal LiDAR 910 Geografie und Reisen CreativeWork article 2020 ftdatacite https://doi.org/10.18452/25057 2024-09-02T08:57:59Z This paper investigates different methods for quantifying thaw subsidence using terrestrial laser scanning (TLS) point clouds. Thaw subsidence is a slow (millimetre to centimetre per year) vertical displacement of the ground surface common in ice-rich permafrost-underlain landscapes. It is difficult to quantify thaw subsidence in tundra areas as they often lack stable reference frames. Also, there is no solid ground surface to serve as a basis for elevation measurements, due to a continuous moss–lichen cover. We investigate how an expert-driven method improves the accuracy of benchmark measurements at discrete locations within two sites using multitemporal TLS data of a 1-year period. Our method aggregates multiple experts’ determination of the ground surface in 3D point clouds, collected in a web-based tool. We then compare this to the performance of a fully automated ground surface determination method. Lastly, we quantify ground surface displacement by directly computing multitemporal point cloud ... Article in Journal/Newspaper Ice permafrost Tundra DataCite |
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Open Polar |
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DataCite |
op_collection_id |
ftdatacite |
language |
English |
topic |
change analysis 3D geoinformation ground surface displacement permafrost monitoring multitemporal LiDAR 910 Geografie und Reisen |
spellingShingle |
change analysis 3D geoinformation ground surface displacement permafrost monitoring multitemporal LiDAR 910 Geografie und Reisen Anders, Katharina Marx, Sabrina Boike, Julia Herfort, Benjamin Wilcox, Evan J Langer, Moritz Marsh, Philip Höfle, Bernhard Multitemporal terrestrial laser scanning point clouds for thaw subsidence observation at Arctic permafrost monitoring sites ... |
topic_facet |
change analysis 3D geoinformation ground surface displacement permafrost monitoring multitemporal LiDAR 910 Geografie und Reisen |
description |
This paper investigates different methods for quantifying thaw subsidence using terrestrial laser scanning (TLS) point clouds. Thaw subsidence is a slow (millimetre to centimetre per year) vertical displacement of the ground surface common in ice-rich permafrost-underlain landscapes. It is difficult to quantify thaw subsidence in tundra areas as they often lack stable reference frames. Also, there is no solid ground surface to serve as a basis for elevation measurements, due to a continuous moss–lichen cover. We investigate how an expert-driven method improves the accuracy of benchmark measurements at discrete locations within two sites using multitemporal TLS data of a 1-year period. Our method aggregates multiple experts’ determination of the ground surface in 3D point clouds, collected in a web-based tool. We then compare this to the performance of a fully automated ground surface determination method. Lastly, we quantify ground surface displacement by directly computing multitemporal point cloud ... |
format |
Article in Journal/Newspaper |
author |
Anders, Katharina Marx, Sabrina Boike, Julia Herfort, Benjamin Wilcox, Evan J Langer, Moritz Marsh, Philip Höfle, Bernhard |
author_facet |
Anders, Katharina Marx, Sabrina Boike, Julia Herfort, Benjamin Wilcox, Evan J Langer, Moritz Marsh, Philip Höfle, Bernhard |
author_sort |
Anders, Katharina |
title |
Multitemporal terrestrial laser scanning point clouds for thaw subsidence observation at Arctic permafrost monitoring sites ... |
title_short |
Multitemporal terrestrial laser scanning point clouds for thaw subsidence observation at Arctic permafrost monitoring sites ... |
title_full |
Multitemporal terrestrial laser scanning point clouds for thaw subsidence observation at Arctic permafrost monitoring sites ... |
title_fullStr |
Multitemporal terrestrial laser scanning point clouds for thaw subsidence observation at Arctic permafrost monitoring sites ... |
title_full_unstemmed |
Multitemporal terrestrial laser scanning point clouds for thaw subsidence observation at Arctic permafrost monitoring sites ... |
title_sort |
multitemporal terrestrial laser scanning point clouds for thaw subsidence observation at arctic permafrost monitoring sites ... |
publisher |
Humboldt-Universität zu Berlin |
publishDate |
2020 |
url |
https://dx.doi.org/10.18452/25057 https://edoc.hu-berlin.de/handle/18452/25740 |
genre |
Ice permafrost Tundra |
genre_facet |
Ice permafrost Tundra |
op_rights |
Creative Commons Attribution Non Commercial 4.0 International (CC BY-NC 4.0) Attribution-NonCommercial 4.0 International https://creativecommons.org/licenses/by-nc/4.0/legalcode cc-by-nc-4.0 |
op_doi |
https://doi.org/10.18452/25057 |
_version_ |
1810449122967158784 |