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Wise MG, Dowdeswell JA, Jakobsson M, et al. Evidence of marine ice-cliff instability in Pine Island Bay from iceberg-keel plough marks. Nature. 2017;550(7677):506-510doi: 10.1038/nature24458.
Wise, M. G., Dowdeswell, J. A., Jakobsson, M., & Larter, R. D. (2017). Evidence of marine ice-cliff instability in Pine Island Bay from iceberg-keel plough marks. Nature, 550(7677), 506-510. https://doi.org/10.1038/nature24458
Wise, Matthew G, et al. "Evidence of marine ice-cliff instability in Pine Island Bay from iceberg-keel plough marks." Nature vol. 550,7677 (2017): 506-510. doi: https://doi.org/10.1038/nature24458
Wise MG, Dowdeswell JA, Jakobsson M, Larter RD. Evidence of marine ice-cliff instability in Pine Island Bay from iceberg-keel plough marks. Nature. 2017 Oct 25;550(7677):506-510. doi: 10.1038/nature24458. PMID: 29072274.
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Nature. 2017 Oct 25;550(7677):506-510. doi: 10.1038/nature24458.

Evidence of marine ice-cliff instability in Pine Island Bay from iceberg-keel plough marks.

Nature

Matthew G Wise, Julian A Dowdeswell, Martin Jakobsson, Robert D Larter

Affiliations

  1. Scott Polar Research Institute, University of Cambridge, Lensfield Road, Cambridge CB2 1ER, UK.
  2. Department of Geological Sciences and Bolin Centre for Climate Research, Stockholm University, 10691 Stockholm, Sweden.
  3. British Antarctic Survey, Natural Environment Research Council, High Cross, Madingley Road, Cambridge CB3 0ET, UK.

PMID: 29072274 DOI: 10.1038/nature24458

Abstract

Marine ice-cliff instability (MICI) processes could accelerate future retreat of the Antarctic Ice Sheet if ice shelves that buttress grounding lines more than 800 metres below sea level are lost. The present-day grounding zones of the Pine Island and Thwaites glaciers in West Antarctica need to retreat only short distances before they reach extensive retrograde slopes. When grounding zones of glaciers retreat onto such slopes, theoretical considerations and modelling results indicate that the retreat becomes unstable (marine ice-sheet instability) and thus accelerates. It is thought that MICI is triggered when this retreat produces ice cliffs above the water line with heights approaching about 90 metres. However, observational evidence confirming the action of MICI has not previously been reported. Here we present observational evidence that rapid deglacial ice-sheet retreat into Pine Island Bay proceeded in a similar manner to that simulated in a recent modelling study, driven by MICI. Iceberg-keel plough marks on the sea-floor provide geological evidence of past and present iceberg morphology, keel depth and drift direction. From the planform shape and cross-sectional morphologies of iceberg-keel plough marks, we find that iceberg calving during the most recent deglaciation was not characterized by small numbers of large, tabular icebergs as is observed today, which would produce wide, flat-based plough marks or toothcomb-like multi-keeled plough marks. Instead, it was characterized by large numbers of smaller icebergs with V-shaped keels. Geological evidence of the form and water-depth distribution of the plough marks indicates calving-margin thicknesses equivalent to the threshold that is predicted to trigger ice-cliff structural collapse as a result of MICI. We infer rapid and sustained ice-sheet retreat driven by MICI, commencing around 12,300 years ago and terminating before about 11,200 years ago, which produced large numbers of icebergs smaller than the typical tabular icebergs produced today. Our findings demonstrate the effective operation of MICI in the past, and highlight its potential contribution to accelerated future retreat of the Antarctic Ice Sheet.

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