Basal Settings Control Fast Ice Flow in the Recovery/Slessor/Bailey Region, East Antarctica

Anja Diez, Kenichi Matsuoka, Fausto Ferraccioli, Tom A. Jordan, Hugh F. Corr, Jack Kohler, Arne V. Olesen, René Forsberg

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Abstract

The region of Recovery Glacier, Slessor Glacier, and Bailey Ice Stream, East Antarctica, has remained poorly explored, despite representing the largest potential contributor to future global sea level rise on a centennial to millennial time scale. Here we use new airborne radar data to improve knowledge about the bed topography and investigate controls of fast ice flow. Recovery Glacier is underlain by an 800 km long trough. Its fast flow is controlled by subglacial water in its upstream and topography in its downstream region. Fast flow of Slessor Glacier is controlled by the presence of subglacial water on a rough crystalline bed. Past ice flow of adjacent Recovery and Slessor Glaciers was likely connected via the newly discovered Recovery‐Slessor Gate. Changes in direction and speed of past fast flow likely occurred for upstream parts of Recovery Glacier and between Slessor Glacier and Bailey Ice Stream. Similar changes could also reoccur here in the future.
Original languageEnglish
JournalGeophysical Research Letters
Volume45
Issue number6
Pages (from-to)2706-2715
ISSN0094-8276
DOIs
Publication statusPublished - 2018

Bibliographical note

©2018. The Authors. This is an open access article under the terms of the Creative Commons Attribution-NonCommercial-NoDerivs License, which permits use and distribution in any medium, provided the original work is properly cited, the use is non-commercial and no modifications or adaptations are made.

Keywords

  • Basal conditions
  • Ice flow
  • Recovery Region
  • Bed topography
  • Antarctica

Cite this

Diez, A., Matsuoka, K., Ferraccioli, F., Jordan, T. A., Corr, H. F., Kohler, J., Olesen, A. V., & Forsberg, R. (2018). Basal Settings Control Fast Ice Flow in the Recovery/Slessor/Bailey Region, East Antarctica. Geophysical Research Letters, 45(6), 2706-2715. https://doi.org/10.1002/2017GL076601