2022
DOI: 10.1017/aog.2023.3
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Paths forward in radioglaciology

Abstract: Ice-penetrating radar sounding is a powerful geophysical tool for studying terrestrial and planetary ice with a rich glaciological heritage reaching back over half a century. Recent years have also seen rapid growth in both the radioglaciological community itself and in the scope and sophistication of its analysis of ice-penetrating radar data. This has been spurred by a combination of growing datasets and improvements in computational resources as well as advances in radar sounding instrumentation and platfor… Show more

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Cited by 4 publications
(2 citation statements)
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“…With this is mind, the framework could be applied to other regions with similar conditions to distinguish frozen and thawed bed patches, though choosing bounds for processing, labeling, and thresholding would need to be updated for the new region. The framework could also be applied to focused data (Heliere et al., 2007; Peters et al., 2007) or other types of ice penetrating radar data (Schlegel et al., 2023), or used to classify other subglacial environments including grounding zone locations or subglacial lake detection. Additionally, the framework's ability to assess uncertainty could be further exploited, either by tracing individual influences from subsampling existing surveys or adding synthetic data.…”
Section: Discussionmentioning
confidence: 99%
“…With this is mind, the framework could be applied to other regions with similar conditions to distinguish frozen and thawed bed patches, though choosing bounds for processing, labeling, and thresholding would need to be updated for the new region. The framework could also be applied to focused data (Heliere et al., 2007; Peters et al., 2007) or other types of ice penetrating radar data (Schlegel et al., 2023), or used to classify other subglacial environments including grounding zone locations or subglacial lake detection. Additionally, the framework's ability to assess uncertainty could be further exploited, either by tracing individual influences from subsampling existing surveys or adding synthetic data.…”
Section: Discussionmentioning
confidence: 99%
“…Since the early 1970s, radar echo sounding (RES) has been the primary means of measuring ice thickness, inferring thickness based on two-way travel times of transmitted radio waves reflected off the ice-bed interface. Over the past two decades, significant advances in radar technology and processing workflows for both surface and airborne surveys have revealed unprecedented detail into the morphology of Greenland's bed, though much uncertainty remains [210,211]. With the launch of NASA's Operation IceBridge (2009-2019), airborne radar coverage of Greenland increased by more than threefold, adding more…”
Section: Bed Topography and Compositionmentioning
confidence: 99%