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Cited by 913

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Stability of the Junction of an Ice Sheet and an Ice Shelf

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Weertman, J.·1974·Journal of Glaciology

Abstract

An analysis is made of the steady-state size of a two-dimensional ice sheet whose base is below sea-level and which terminates in floating ice shelves. Under the assumption of perfect plasticity it is found that an ice sheet placed on a bed whose surface was initially flat cannot exist if the depth of the bed below sea-level exceeds a critical depth. If this depth is less than the critical level, the ice sheet extends out to the edge of the continental shelf. Similar results are found with more realistic assumptions about the laws governing the flow of ice. If the bed slopes away from the centre, the ice sheet can have a stable width that increases in value as the accumulation rate increases or as sea-level is lowered. It is not possible to decide whether or not the West Antarctic ice sheet is in stable equilibrium. It is entirely possible that this ice sheet is disintegrating at present, as suggested by Hughes.

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Metadata

Authors
Weertman, J.
Venue
Journal of Glaciology
Published
1974
Volume
13
Issue
67
Pages
3-11
ISSN
  • 0022-1430 (ISSN-L)
  • 1727-5652
OpenAlex
W92483960
Cited by
913
References
0
FWCI
5.33
Type
journal article
Language
en
Open access
bronze

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CoChat. (2026). Citation check: Stability of the Junction of an Ice Sheet and an Ice Shelf. https://app.cochat.ai/papers/10.1017/s0022143000023327
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Weertman, J. (1974). Stability of the Junction of an Ice Sheet and an Ice Shelf. Journal of Glaciology. https://doi.org/10.1017/s0022143000023327

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Bibliographic data: Semantic Scholar, OpenAlex, Crossref.

Contains information from the Semantic Scholar Academic Graph Datasets, made available under the ODC Attribution License (ODC-BY 1.0).

Semantic Scholar’s data is described in: Kinney, R., et al. (2023). The Semantic Scholar Open Data Platform. arXiv:2301.10140.