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Influence of the grounding zone on the internal structure of ice shelves

K. E. Miles Orcid Logo, B. Hubbard Orcid Logo, Adrian Luckman Orcid Logo, Bernd Kulessa Orcid Logo, Suzanne Bevan Orcid Logo, S. Thompson, Glenn Jones

Nature Communications, Volume: 16, Issue: 1, Start page: 4383

Swansea University Authors: Adrian Luckman Orcid Logo, Bernd Kulessa Orcid Logo, Suzanne Bevan Orcid Logo, Glenn Jones

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Abstract

Antarctic ice shelves typically comprise continental meteoric ice, in situ-accumulated meteoric ice, and marine ice accumulated at the shelf base. Using borehole optical televiewer logs from across Larsen C Ice Shelf, Antarctic Peninsula, we identify and report an intermediate ice unit, located betw...

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Published in: Nature Communications
ISSN: 2041-1723
Published: Springer Nature 2025
Online Access: Check full text

URI: https://cronfa.swan.ac.uk/Record/cronfa69502
Abstract: Antarctic ice shelves typically comprise continental meteoric ice, in situ-accumulated meteoric ice, and marine ice accumulated at the shelf base. Using borehole optical televiewer logs from across Larsen C Ice Shelf, Antarctic Peninsula, we identify and report an intermediate ice unit, located between continental and in situ meteoric ice, that is tens of metres thick and formed of layers that progressively increase in dip (by ~60°) with depth. The unit’s stratigraphic position and depth, supported by flowline modelling, indicate formation at the grounding zone. We hypothesise that the unit forms due to changes in the surface slope of feeder glaciers at the grounding zone, resulting in both variable surface accumulation and intense deformation. The top of the unit also marks the depth at which lateral consistency in radar layering is lost from radargrams, which may, to some degree, mark the depth of grounding zone ice across all ice shelves.
College: Faculty of Science and Engineering
Funders: This research was funded by the “Rift Propagation for Ice sheet models (RiPIce)” Natural Environment Research Council grant awarded to Aberystwyth and Swansea Universities (NE/T008016/1). We thank the British Antarctic Survey for logistical support, particularly the project’s Field Guides: Samuel Hunt, Sarah Crowsley, and Min Willis.
Issue: 1
Start Page: 4383