Radar investigation of two subglacial lake drainage sites at Isunnguata Sermia, West Greenland, 2024


GB/NERC/BAS/PDC/02182

Abstract:
The ice-penetrating radar data were acquired over two ice surface elevation anomalies on Isunnguata Sermia, West Greenland. The elevation anomalies are inferred to result from the drainage of active subglacial lakes. The radar data were acquired between 2024-09-26 and 2024-10-04 using a Blue Systems Integration IceRadar with 10 MHz antennas and a Nugen Narod transmitter, with a pulse repetition frequency of 10 MHz. A total of 26.5 km of survey transects were recorded and a basal interface was picked at 5 m intervals using a semi-automated method across 91% of the full survey. Ice thicknesses of greater than 500 m, to the north of the elevation anomalies, showed a reduced signal to noise ratio and therefore confidence in these picks is lower than in shallower ice. Reflected power is extracted from each bed picks and used to estimate the reflection coefficient. Ice thickness picks were combined with an ArcticDEM surface elevation model (2024-07-27) to generate an interpolated bed elevation dataset on a 20 m grid. Hydraulic potential surfaces, accumulation patterns and minima using the ice thickness and bed elevation datasets are calculated for a range of subglacial pressure values inferred from observations with an englacial pressure sensor.
An additional reconnaissance dataset was acquired between 2023-04-17 and 2023-04-24 using the same radar system with 5 MHz antennas. A total of 7.9 km of survey transects were recorded and raw data are included for completeness.
The radar data were acquired to image and characterise the setting of an active subglacial lake, as part of the NERC-funded SLIDE (Subglacial Lakes at Isunnguata Sermia - Dynamics and Evolution) research project.

The SLIDE project is funded by the Natural Environmental Research Council Standard Grant NE/X000257/1. JDH and LC were supported by a UKRI Future Leaders Fellowship (to Michael Prior-Jones, MR/V022237/1). We acknowledge the support of Kangerlussuaq International Science Support and the local knowledge and guidance of Chris Sorensen.


Citation:
Hawkins, J., Peacey, M., Killingbeck, S., Ross, N., Livingstone, S., Le Bris, T., Barruol, G., Young, T., Sole, A., Doyle, S., Craw, L., Thorpe, S., Veness, R., Booth, A., Bagshaw, E., Buzzard, S., Edwards, L., Storrar, R., & Prior-Jones, M. (2026). Radar investigation of two subglacial lake drainage sites at Isunnguata Sermia, West Greenland, 2024 (Version 1.0) [Data set]. NERC EDS UK Polar Data Centre. https://doi.org/10.5285/b90093f6-2431-42f3-a6d8-7365f368e188