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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Main Authors: Anders, Katharina, Marx, Sabrina, Boike, Julia, Herfort, Benjamin, Wilcox, Evan J, Langer, Moritz, Marsh, Philip, Höfle, Bernhard
Format: Article in Journal/Newspaper
Language:English
Published: Humboldt-Universität zu Berlin 2020
Subjects:
Ice
Online Access:https://dx.doi.org/10.18452/25057
https://edoc.hu-berlin.de/handle/18452/25740
id ftdatacite:10.18452/25057
record_format openpolar
spelling 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
institution Open Polar
collection 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