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A high-resolution record of surface melt on Antarctic ice shelves using multi-source remote sensing data and deep learning
Husman, S.D.; Lhermitte, S.; Bolibar, J.; Izeboud, M.; Hu, Z.Y.; Shukla, S.; van der Meer, M.; Long, D.; Wouters, B. (2024). A high-resolution record of surface melt on Antarctic ice shelves using multi-source remote sensing data and deep learning. Remote Sens. Environ. 301: 113950. https://dx.doi.org/10.1016/j.rse.2023.113950
In: Remote Sensing of Environment. Elsevier: New York,. ISSN 0034-4257; e-ISSN 1879-0704, more
Peer reviewed article  

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Keyword
    Marine/Coastal
Author keywords
    Antarctica; U-Net; Machine learning; Microwave remote sensing; Enhanced resolution; Google Earth Engine; Surface melt

Authors  Top 
  • Husman, S.D.
  • Lhermitte, S., more
  • Bolibar, J.
  • Izeboud, M.
  • Hu, Z.Y.
  • Shukla, S.
  • van der Meer, M.
  • Long, D.
  • Wouters, B.

Abstract
    While the influence of surface melt on Antarctic ice shelf stability can be large, the duration and affected area of melt events are often small. Therefore, melt events are difficult to capture with remote sensing, as satellite sensors always face the trade-off between spatial and temporal resolution. To overcome this limitation, we developed UMelt: a surface melt record for all Antarctic ice shelves with a high spatial (500 m) and high temporal (12 h) resolution for the period 2016-2021. Our approach is based on a deep learning model, specifically a U-Net, which was developed in Google Earth Engine. The U-Net combines microwave remote sensing observations from three sources: Sentinel-1, Special Sensor Microwave Imager/Sounder (SSMIS), and Advanced Scatterometer (ASCAT). The U-Net was trained on the Shackleton Ice Shelf for melt seasons 2017- 2021, using the fine-scale melt patterns of Sentinel-1 as reference data and SSMIS, ASCAT, a digital elevation model, and multi-year Sentinel-1 melt fraction as predictors. The trained U-Net performed well on the Shackelton Ice Shelf for test melt season 2016-2017 (accuracy: 91.3%; F1-score: 86.9%), and the Larsen C Ice Shelf, which was not considered during training (accuracy: 91.0%; F1-score: 89.3%). Using the trained U-Net model, we have successfully developed the UMelt record. UMelt allows Antarctic-wide surface melt to be detected at a small scale while preserving a high temporal resolution, which could lead to new insights into the response of ice shelves to a changing atmospheric forcing.

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