Preprints
https://doi.org/10.5194/egusphere-2026-5765
https://doi.org/10.5194/egusphere-2026-5765
01 Oct 2026
 | 01 Oct 2026
Status: this preprint is open for discussion and under review for Earth Observation (EO).

Multi-sensor deep-learning mapping of surface and basal fractures across Antarctic ice shelves during the last four decades

Kaian Shahateet, Colin Prieur, Romain Millan, Lucille Gimenes, Andrea Sofie Haastrup-Vang, Jaime Roas, Maaike Izeboud, Raphaelle Charrassin, Emil Giraldi, and Romain Santiard

Abstract. Ice shelves buttress the discharge of Antarctica’s outlet glaciers, mitigating their contribution to sea-level rise. Yet progressive damage through fracturing remains largely absent from projections, partly because long-term observations of ice-shelf fractures remain limited despite their critical influence on ice-shelf stability. Here, we introduce BASIS (BAsal and Surface Ice-shelf fracture extraction System), a deep-learning model for mapping surface crevasses and basal-fracture across Antarctic ice shelves. Unlike existing approaches based on classical edge detectors or models trained on edge-based datasets, BASIS is designed to delineate the full extent of fracture features, including diffuse basal-fracture signatures and highly damaged, chaotic regions. We train, validate, and test BASIS, based on DeepLabv3, using a unique manually labeled fracture dataset spanning 14 Antarctic ice shelves and the full Landsat observation era. Model performance approaches inter-annotator agreement, while maintaining the distinction between basal and surface fractures. We quantify biases associated with sensor transitions and observation availability and develop a framework for producing consistent multi-sensor fracture records. Annual mosaics reveal the spatiotemporal evolution of ice-shelf damage from the 1980s onward and show that basal-fracture signatures dominate the mapped damage patterns across the ice shelves examined here. At Pine Island Glacier Ice Shelf, BASIS resolves successive stages of shear-margin damage together with a progressive increase in basal-fracture. At Mertz and Borchgrevink ice shelves, it reveals extensive networks of basal-fracture signatures that are poorly represented in existing continent-wide products based on Sentinel-1 SAR imagery. Finally, BASIS demonstrates promising cross-sensor transferability to Sentinel-2 and ASTER optical imagery and, despite having been trained exclusively on Landsat data, also recovers coherent fracture patterns from SAR imagery. These results provide a foundation for large-scale, multi-sensor monitoring of Antarctic ice-shelf damage across unprecedented spatial and temporal scales.

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Kaian Shahateet, Colin Prieur, Romain Millan, Lucille Gimenes, Andrea Sofie Haastrup-Vang, Jaime Roas, Maaike Izeboud, Raphaelle Charrassin, Emil Giraldi, and Romain Santiard

Status: open (until 12 Nov 2026)

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Kaian Shahateet, Colin Prieur, Romain Millan, Lucille Gimenes, Andrea Sofie Haastrup-Vang, Jaime Roas, Maaike Izeboud, Raphaelle Charrassin, Emil Giraldi, and Romain Santiard
Kaian Shahateet, Colin Prieur, Romain Millan, Lucille Gimenes, Andrea Sofie Haastrup-Vang, Jaime Roas, Maaike Izeboud, Raphaelle Charrassin, Emil Giraldi, and Romain Santiard
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Latest update: 01 Oct 2026
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Short summary
We developed a deep-learning tool that uses satellite observations to map fractures across Antarctica’s floating ice shelves over nearly four decades. Applied to images collected since the 1980s, it detects both visible surface cracks and subtle signatures of fractures beneath the ice. The method works across several satellite sensors, paving the way for long-term records of ice-shelf damage across Antarctica.
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