EGU23-14307
https://doi.org/10.5194/egusphere-egu23-14307
EGU General Assembly 2023
© Author(s) 2023. This work is distributed under
the Creative Commons Attribution 4.0 License.

Delineating giant Antarctic icebergs with Deep Learning

Anne Braakmann-Folgmann1, Andrew Shepherd1, David Hogg2, and Ella Redmond1
Anne Braakmann-Folgmann et al.
  • 1University of Leeds, School of Earth and Environment, Centre for Polar Observation and Modelling, Leeds, LS2 9JT, UK
  • 2University of Leeds, School of Computer Science, Leeds, LS2 9JT, UK

Icebergs account for half of all ice loss from Antarctica. Their melting affects the surrounding ocean properties through the intrusion of cold, fresh meltwater and the release of terrigenious nutrients. This in turn influences the local ocean circulation, sea ice formation and biological production. To locate and quantify the fresh water flux from Antarctic icebergs, we need to track them and monitor changes in their area and thickness. While the locations of large icebergs are tracked operationally by manual inspection, delineation of iceberg extent requires detailed analysis – either also manually or through automated segmentation of high resolution satellite imagery.

In this study, we apply three machine learning techniques to 191 Sentinel-1 images between 2014 and 2020 and assess their skill to segment seven giant Antarctic icebergs between 54 and 1052 km2 in size. Most previous studies to detect icebergs have focused on smaller bergs. In contrast, we aim to segment selected giant icebergs with the goal to automate the calculation of their changing area, volume, and freshwater input. Two of our techniques are standard segmentation techniques (k-means and Otsu thresholding) and the third one is a deep neural network (U-net). It is the first study to apply a deep learning algorithm to iceberg detection.

We analyse the strengths and weaknesses of the different machine learning approaches across a range of challenging environmental conditions: These include scenes where the iceberg is surrounded by deformed sea ice, when other big bergs are present and when berg fragments are close to the main iceberg. We also cover cases when the iceberg drifts close to the coast and summer images with surface thawing conditions, which invert the backscatter contrast between iceberg and ocean.

How to cite: Braakmann-Folgmann, A., Shepherd, A., Hogg, D., and Redmond, E.: Delineating giant Antarctic icebergs with Deep Learning, EGU General Assembly 2023, Vienna, Austria, 24–28 Apr 2023, EGU23-14307, https://doi.org/10.5194/egusphere-egu23-14307, 2023.