Abstract:
The dataset encompasses the processed point clouds (.pts format), a panoramic tour, and a video flythrough of registered point clouds capturing a 122 m long reach of an englacial cut-and-closure channel in the glacier, Austre Broggerbreen, Svalbard, in March 2016. Point clouds were derived from 28 Terrestrial Laser Scanning (TLS) surveys, to characterise the morphology of the channel in three-dimensions and enable extraction of features reflective of hydrological flow conditions. The panoramic tour shows a greyscale image of the scan reflectivity values at each survey location, whereby the lighter the pixel colour, the greater the intensity of the laser beam return. This panoramic tour enables the viewer to self-navigate through the channel to see the morphological features within it. The video flythrough of the point cloud provides a visualisation of the point cloud data, travelling from the glacier surface, down the moulin and along the extent of the scanned reach. The point cloud has been coloured to reflect differences in height.
Funding source
Knowledge Economy Skills Scholarship (KESS II) under Project AU10003, a pan-Wales higher-level skills initiative led by Bangor University of behalf of the HE sector in Wales. It is part funded by the Welsh Government's European Social Fund (ESF) convergence programme for West Wales and the Valleys. Funding was awarded to TDLI-F and JEK, with support from Deri Jones & Associates Ltd. Additional support is acknowledged from Aberystwyth University (Department of Geography and Earth Sciences).
Keywords:
Austre Broggerbreen, englacial, point clouds, terrestrial laser scanning
Kamintzis, J., Jennings, S., Irvine-Fynn, T., Holt, T., Jones, J., Hubbard, B., & Bunting, P. (2019). Point cloud data and visualisation of an englacial cut-and-closure channel on Austre Broggerbreen, Svalbard, in March 2016 (Version 1.0) [Data set]. UK Polar Data Centre, Natural Environment Research Council, UK Research & Innovation. https://doi.org/10.5285/65abc40d-e256-414b-8b50-a5569556d1be
| Access Constraints: | No restrictions apply. |
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| Use Constraints: | This data is supplied under Open Government Licence v3.0 http://www.nationalarchives.gov.uk/doc/open-government-licence/version/3/. |
| Creation Date: | 2019-06-20 |
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| Dataset Progress: | Complete |
| Dataset Language: | English |
| ISO Topic Categories: |
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| Parameters: |
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| Personnel: | |
| Name | UK PDC |
| Role(s) | Metadata Author |
| Organisation | British Antarctic Survey |
| Name | Pete Bunting |
| Role(s) | Investigator |
| Organisation | Aberystwyth University |
| Name | Thomas O Holt |
| Role(s) | Investigator |
| Organisation | Aberystwyth University |
| Name | Bryn Hubbard |
| Role(s) | Investigator |
| Organisation | Aberystwyth University |
| Name | Tristram D L Irvine-Fynn |
| Role(s) | Investigator |
| Organisation | Aberystwyth University |
| Name | Stephen J A Jennings |
| Role(s) | Investigator |
| Organisation | Masaryk University |
| Name | John P P Jones |
| Role(s) | Investigator |
| Organisation | Deri Jones and Associates, Ltd. |
| Name | Jayne E Kamintzis |
| Role(s) | Investigator |
| Organisation | Aberystwyth University |
| Parent Dataset: | N/A |
| Reference: | Kamintzis, J.E, Jones, J.P.P, Irvine-Fynn, T.D.L, Holt, T.O, Bunting, P, Jennings, S.J.A, Porter, P.R, and Hubbard, B. (2018) Assessing the applicability of terrestrial laser scanning for mapping englacial conduits, Journal of Glaciology, 64(243), 37-48. doi: 10.1017/jog.2017.81 | |
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| Quality: | Each scan has been registered to the preceding scan with a mean registration accuracy of 3.3 mm. This error is the standard deviation of the orthogonal registration mismatch, expressed as cumulative distance offset in the X, Y and Z planes. Due to the unclosed traverse preventing equal error distribution between scans, the maximum combined absolute error at the end of the traverse is 73 mm, derived as the sum of orthogonal registration mismatches for the 28 scans. Cleaning of the data used the 'distance based' and 'stray' filters within the FARO® SCENE 5 software to remove points > 30 m from each scan position and scan points that resulted from the laser beam hitting two objects. Data losses are the result of the clean, shiny, smooth ice surfaces within the englacial channel, with these surfaces failing to provide laser returns due to the infrared absorption. |
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| Lineage: | Data was collected using a FARO (registered trademark) Focus3D X 330 phase-shift scanner with a shortwave infrared wavelength of 1550 nm, mounted on a GitzoTM Mountaineer carbon fibre tripod using a heavy duty 3/8" camera fast-release mount. Scans were conducted throughout the channel reach at a horizontal spacing of between 2 and 9 m, at a height of 1.5 m. All channel scans were conducted at 1/5 resolution, providing point spacing of 7.67 mm at 10 m distance, with scans at the glacier surface being conducted at 1/4 resolution, providing point spacing of 6.14 mm at 10 m distance. Scan locations were determined by the channel morphology, with positioning of the scanner to obtain the greatest wall coverage with the minimum number of scans, and to prevent channel morphology from occluding parts of the channel. A4 planar checkerboard targets were inserted into the channel walls using ice screws and crocodile clips and A5 planar checkerboard targets were placed at intervals of > 1 m along the channel floor. Targets were placed strategically to enable registration of the point clouds to one another, with a minimum of 3 common targets between each adjacent scan. The initial scan was conducted at the glacier surface and, thus, the GPS location of these scans were used to georeference the scans below the ice. The point clouds were manually registered to one another in a downstream direction from the base of the moulin using the targets in FARO (registered trademark) SCENE 5 software, with the use of distance based and stray filtering processes to remove points > 30 m away from the scanner and points arising from the laser beam hitting 2 surfaces. Jpeg images of the scan reflectivity values were exported from FARO (registered trademark) SCENE 5 and linked in Kolor Panotour Pro 2.5 software to create a 360deg visualisation from each scan location, with inbuilt links to the adjacent scans and a map of the channel planform. Point clouds were imported into Bentley Pointools CONNECT Edition software and the colour range was changed to reflect the height of each point above the initial scan location. Recording of camera positions throughout the channel was used to create a video flythrough of the point clouds. |
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| Temporal Coverage: | |
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| Start Date | 2016-03-10 |
| End Date | 2016-03-16 |
| Spatial Coverage: | |
| Latitude | |
| Southernmost | 78.89384 |
| Northernmost | 78.89384 |
| Longitude | |
| Westernmost | 11.842 |
| Easternmost | 11.842 |
| Altitude | |
| Min Altitude | 178 |
| Max Altitude | 178 |
| Depth | |
| Min Depth | N/A |
| Max Depth | N/A |
| Location: | |
| Location | Svalbard |
| Detailed Location | Broggerhalvoya |
| Sensor(s): |
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| Data Collection: | Terrestrial laser scanner - FARO (registered trademark) Focus3D X 330 Software - FARO (registered trademark) SCENE 5, 3D Reshaper 2018, Bentley Pointools CONNECT Edition, Kolor Panotour Pro 2.5. |
| Data Storage: | There are 28 .pts files, each containing a point cloud from the 28 scan positions established within the channel. Each file is numbered from the moulin surface throughout the channel in a downstream direction. Their approximate size is 16 GB. There is one mp4 file containing the video flythrough of the point clouds, which is 60 MB. The flythrough is in an upstream direction, beginning at the portal exit. |
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