Articles | Volume 14, issue 7
https://doi.org/10.5194/tc-14-2313-2020
https://doi.org/10.5194/tc-14-2313-2020
Research article
 | 
22 Jul 2020
Research article |  | 22 Jul 2020

Lateral meltwater transfer across an Antarctic ice shelf

Rebecca Dell, Neil Arnold, Ian Willis, Alison Banwell, Andrew Williamson, Hamish Pritchard, and Andrew Orr

Model code and software

Fully Automated Supraglacial-Water Tracking algorithm for Ice Shelves (FASTISh). Rebecca Dell, Neil Arnold, Ian Willis, Alison Banwell, Andrew Williamson, Hamish Pritchard, and Andrew Orr https://doi.org/10.17863/CAM.54008

Video supplement

S.2 (GIF of all 11 RGB base images) Rebecca Dell, Neil Arnold, Ian Willis, Alison Banwell, Andrew Williamson, Hamish Pritchard, and Andrew Orr https://doi.org/10.5446/47526

S.3 (GIF of all 11 area matrices) Rebecca Dell, Neil Arnold, Ian Willis, Alison Banwell, Andrew Williamson, Hamish Pritchard, and Andrew Orr https://doi.org/10.5446/47524

S.4 (GIF of all 11 depth matrices) Rebecca Dell, Neil Arnold, Ian Willis, Alison Banwell, Andrew Williamson, Hamish Pritchard, and Andrew Orr https://doi.org/10.5446/47525

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Short summary
A semi-automated method is developed from pre-existing work to track surface water bodies across Antarctic ice shelves over time, using data from Sentinel-2 and Landsat 8. This method is applied to the Nivlisen Ice Shelf for the 2016–2017 melt season. The results reveal two large linear meltwater systems, which hold 63 % of the peak total surface meltwater volume on 26 January 2017. These meltwater systems migrate towards the ice shelf front as the melt season progresses.