Articles | Volume 17, issue 11
https://doi.org/10.5194/tc-17-4549-2023
https://doi.org/10.5194/tc-17-4549-2023
Research article
 | 
01 Nov 2023
Research article |  | 01 Nov 2023

Assessing the potential for ice flow piracy between the Totten and Vanderford glaciers, East Antarctica

Felicity S. McCormack, Jason L. Roberts, Bernd Kulessa, Alan Aitken, Christine F. Dow, Lawrence Bird, Benjamin K. Galton-Fenzi, Katharina Hochmuth, Richard S. Jones, Andrew N. Mackintosh, and Koi McArthur

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Latest update: 21 Jun 2024
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Short summary
Changes in Antarctic surface elevation can cause changes in ice and basal water flow, impacting how much ice enters the ocean. We find that ice and basal water flow could divert from the Totten to the Vanderford Glacier, East Antarctica, under only small changes in the surface elevation, with implications for estimates of ice loss from this region. Further studies are needed to determine when this could occur and if similar diversions could occur elsewhere in Antarctica due to climate change.