Articles | Volume 17, issue 10
https://doi.org/10.5194/tc-17-4421-2023
https://doi.org/10.5194/tc-17-4421-2023
Research article
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19 Oct 2023
Research article | Highlight paper |  | 19 Oct 2023

Mapping Antarctic crevasses and their evolution with deep learning applied to satellite radar imagery

Trystan Surawy-Stepney, Anna E. Hogg, Stephen L. Cornford, and David C. Hogg

Data sets

Data accompanying the article "Mapping Antarctic Crevasses and their Evolution with Deep Learning Applied to Satellite Radar Imagery" (Version 1) Trystan Surawy-Stepney and Anna E. Hogg https://doi.org/10.5281/zenodo.8296992

Model code and software

Code accompanying the article "Mapping Antarctic Crevasses and their Evolution with Deep Learning Applied to Satellite Radar Imagery" (Version 1) T. Surawy-Stepney https://doi.org/10.5281/zenodo.8410599

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Co-editor-in-chief
This research is part of an exciting advancement in the field of glaciology, driven by machine learning. The study focuses on crevasse detection, a highly relevant topic from a scientific and logistic perspective. Crevasses may aid surface meltwater to penetrate through the ice thus impacting ice dynamics. Crevasses also pose a logistical challenge for fieldwork in the polar regions. In this study, the authors are able to automatically spot grounded crevasses using a Convolutional Neural Networks algorithm. One of the focus areas is the Thwaites Glacier, an area that has recently been subject to extensive scientific research due to its importance for the stability of the West Antarctic Ice Sheet.
Short summary
The presence of crevasses in Antarctica influences how the ice sheet behaves. It is important, therefore, to collect data on the spatial distribution of crevasses and how they are changing. We present a method of mapping crevasses from satellite radar imagery and apply it to 7.5 years of images, covering Antarctica's floating and grounded ice. We develop a method of measuring change in the density of crevasses and quantify increased fracturing in important parts of the West Antarctic Ice Sheet.