UAV Laser Scanning surveys of the lake terminating glacier Fjallsjokull in SE Iceland, captured in July, 2021.
UAV Laser Scanning surveys of the lake terminating glacier Fjallsjokull in SE Iceland, captured in July, 2021.
This dataset consists of 5 separate laser scanning surveys performed between the 8th and 15th July, 2021. Two surveys were conducted in the morning and afternoon of the 8th and the 9th, and then only the morning of the 15th. The point clouds have been cleaned to remove erroneous points. The point clouds were processed using the methods and code available at Direct_Georeferencing. All point clouds are georeferenced in the projected WGS 1984 UTM 28N system, and provided in the widely used compressed 'laz' format. An accuracy assessment of the data showed that all surveys were consistent to within 0.1 m of each other, apart from the second flight (afternoon) on the 8th July. Any users of this data should be aware of its limitations in a challenging cryospheric environment.
Baurley, Nathaniel
4f7b08da-72ac-42c8-be5d-a2893f09318b
Tomsett, Chris
5b0ab386-98e3-4ba9-bca6-41f058a3ad0e
Baurley, Nathaniel
4f7b08da-72ac-42c8-be5d-a2893f09318b
Tomsett, Chris
5b0ab386-98e3-4ba9-bca6-41f058a3ad0e
(2022)
UAV Laser Scanning surveys of the lake terminating glacier Fjallsjokull in SE Iceland, captured in July, 2021.
Zenodo
doi:10.5281/zenodo.7018549
[Dataset]
Abstract
This dataset consists of 5 separate laser scanning surveys performed between the 8th and 15th July, 2021. Two surveys were conducted in the morning and afternoon of the 8th and the 9th, and then only the morning of the 15th. The point clouds have been cleaned to remove erroneous points. The point clouds were processed using the methods and code available at Direct_Georeferencing. All point clouds are georeferenced in the projected WGS 1984 UTM 28N system, and provided in the widely used compressed 'laz' format. An accuracy assessment of the data showed that all surveys were consistent to within 0.1 m of each other, apart from the second flight (afternoon) on the 8th July. Any users of this data should be aware of its limitations in a challenging cryospheric environment.
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More information
Published date: 24 August 2022
Identifiers
Local EPrints ID: 471339
URI: http://eprints.soton.ac.uk/id/eprint/471339
PURE UUID: d2835495-3fd8-401f-abb5-716f96da753c
Catalogue record
Date deposited: 03 Nov 2022 17:52
Last modified: 21 Nov 2023 03:04
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Contributors
Contributor:
Nathaniel Baurley
Contributor:
Chris Tomsett
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