Automated Extraction of Antarctic Glacier and Ice Shelf Fronts from Sentinel-1 Imagery Using Deep Learning

• Published in: Remote Sensing
• Main Authors: Baumhoer, Celia A., Dietz, Andreas J., Kneisel, C., Kuenzer, C.
• Format: Article in Journal/Newspaper
• Language: English
• Published: 2019
• Subjects: ddc:526; Antarctic; DeVicq Glacier; Getz; Getz Ice Shelf; The Antarctic; Antarc*; Ice Sheet; Ice Shelf; Sea ice
• Online Access: https://opus.bibliothek.uni-wuerzburg.de/frontdoor/index/index/docId/19315; https://nbn-resolving.org/urn:nbn:de:bvb:20-opus-193150; https://doi.org/10.3390/rs11212529; https://opus.bibliothek.uni-wuerzburg.de/files/19315/remotesensing-11-02529.pdf

Sea level rise contribution from the Antarctic ice sheet is influenced by changes in glacier and ice shelf front position. Still, little is known about seasonal glacier and ice shelf front fluctuations as the manual delineation of calving fronts from remote sensing imagery is very time-consuming. The major challenge of automatic calving front extraction is the low contrast between floating glacier and ice shelf fronts and the surrounding sea ice. Additionally, in previous decades, remote sensing imagery over the often cloud-covered Antarctic coastline was limited. Nowadays, an abundance of Sentinel-1 imagery over the Antarctic coastline exists and could be used for tracking glacier and ice shelf front movement. To exploit the available Sentinel-1 data, we developed a processing chain allowing automatic extraction of the Antarctic coastline from Seninel-1 imagery and the creation of dense time series to assess calving front change. The core of the proposed workflow is a modified version of the deep learning architecture U-Net. This convolutional neural network (CNN) performs a semantic segmentation on dual-pol Sentinel-1 data and the Antarctic TanDEM-X digital elevation model (DEM). The proposed method is tested for four training and test areas along the Antarctic coastline. The automatically extracted fronts deviate on average 78 m in training and 108 m test areas. Spatial and temporal transferability is demonstrated on an automatically extracted 15-month time series along the Getz Ice Shelf. Between May 2017 and July 2018, the fronts along the Getz Ice Shelf show mostly an advancing tendency with the fastest moving front of DeVicq Glacier with 726 ± 20 m/yr.