Ground-penetrating radar data from the southern sector of Larsen C Ice Shelf, Antarctic Peninsula, 2022
We present here a suite of ground-penetrating radar (GPR) data collected on Larsen C Ice Shelf, Antarctic Peninsula, in November and December 2022 as part of the NERC-funded RiPIce (Rift Propagation for Ice sheet models) research project. All data were acquired with a Sensors&Software pulsEKKO PRO GPR system, fitted with antennas of 50 MHz centre-frequency. The system was towed behind a snowmobile, with distances recorded with GPS.
This project is funded by a NERC standard grant NE-T008016-1.
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- Date (Creation)
- 2025-03-21
- Date (Revision)
- 2025-03-21
- Date (Publication)
- 2025-03-21
- Date (released)
- 2025-03-21
- Edition
- 1.0
- Unique resource identifier
- https://doi.org/10.5285/9c46ec89-e2da-4140-a8a5-443911fe34cc
- Codespace
- doi
- Unique resource identifier
- GB/NERC/BAS/PDC/02033
- Codespace
- https://data.bas.ac.uk/
- Other citation details
- Please cite this item as: Kulessa, B., & Miles, K. (2025). Ground-penetrating radar data from the southern sector of Larsen C Ice Shelf, Antarctic Peninsula, 2022 (Version 1.0) [Data set]. NERC EDS UK Polar Data Centre. https://doi.org/10.5285/9c46ec89-e2da-4140-a8a5-443911fe34cc
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- completed Completed
https://www.bas.ac.uk/team/business-teams/information-services/uk-polar-data-centre/
- Maintenance and update frequency
- asNeeded As needed
- Maintenance note
- completed Completed
- Theme
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- Antarctic Peninsula
- Antarctic ice shelf
- GPR
- Ground-penetrating radar
- Larsen C Ice Shelf
- Place
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- Larsen C Ice Shelf Antarctica
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- doi
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- doi
- Codespace
- doi
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- textTable Text, table
- Metadata language
- engEnglish
- Character set
- utf8 UTF8
- Topic category
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- Elevation
- Geoscientific information
- Begin date
- 2022-11-30
- End date
- 2022-12-06
- Supplemental Information
- It is recommended that careful attention be paid to the contents of any data, and that the author be contacted with any questions regarding appropriate use. If you find any errors or omissions, please report them to polardatacentre@bas.ac.uk.
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Methodology:
The data comprise three lines, collected ~20 km down-flow of the Joerg Peninsula: one flow-parallel (line 19) and two cross-flow (line 20 + 21 and line 22).
Sampling interval was 1.2 ns and each trace represents a distance-average stack of eight individual traces, resulting in an average trace spacing of ~2.5 m.
Data collection:
Data were acquired with a Sensors&Software pulsEKKO PRO GPR system, fitted with antennas of 50 MHz centre-frequency. In a bistatic configuration, the dipole antennas were mounted in a perpendicular-broadside configuration on a plastic sledge (antenna separation 1.4 m), towed behind a skidoo. Sampling interval was 1.2 ns and each trace represents a distance-average stack of eight individual traces, resulting in an average trace spacing of ~2.5 m. Precise (+/- 0.1 m) planimetric location of each trace was achieved with a Leica VIVA GS10 Professional GNSS receiver, mounted on the snowmobile.
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- engEnglish
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- Date stamp
- 2025-03-21
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- Metadata standard version
- ISO 19115:2003(E)
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