Brief communication reveals bed mapping of glaciers in southern Greenland, indicating depth limits and detection capabilities.
Here we present the first southern Greenland deployment of the re-designed Airborne Ice Radar of ETH Zürich (AIRETH). We surveyed a total of 348 km of profiles over three outlet glaciers, identifying basal reflections along 102 km (29 %) of the flight lines. The 25 MHz antennas configuration achieved an effective penetration depth of about 300 m and a maximum measured ice thickness of about 340 m, with bed detectability decreasing over thicker and/or heavily crevassed ice. These results define the depth limitation of our system and show that terrain-following helicopter surveys can provide targeted constraints that complement existing datasets in complex topography.
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Santin et al. (2026) studied this question.
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