Sediment deposition at the modern grounding zone of Whillans Ice Stream, West Antarctica

Huw J. Horgan, Knut Christianson, Robert W. Jacobel, Sridhar Anandakrishnan, Richard B. Alley

Research output: Contribution to journalArticle

23 Citations (Scopus)

Abstract

Much of the threshold behavior of marine ice sheets is thought to result from processes occurring at the grounding zone, where the ice sheet transitions into the ice shelf. At short timescales (decades to centuries), grounding zone behavior is likely to be influenced by ongoing sediment deposition, which can stabilize the grounding zone position. We present a ground-based geophysical study across the modern grounding zone of Whillans Ice Stream. Within an embayment setting, where subglacial meltwater drains, we image sedimentary deposits; however, we do not observe the classic asymmetric grounding zone wedge deposits, which are found in the paleorecord and are thought to stabilize the grounding zone position. At an adjacent peninsula, we image the grounding zone and an ice-shelf pinning point and again observe no wedge deposits.

Original languageEnglish (US)
Pages (from-to)3934-3939
Number of pages6
JournalGeophysical Research Letters
Volume40
Issue number15
DOIs
StatePublished - Aug 16 2013

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ice stream
Antarctic regions
land ice
sediments
ice
deposits
wedges
sediment
peninsulas
ice shelf
ice sheet
thresholds
Antarctica
meltwater
drain
timescale

All Science Journal Classification (ASJC) codes

  • Geophysics
  • Earth and Planetary Sciences(all)

Cite this

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Sediment deposition at the modern grounding zone of Whillans Ice Stream, West Antarctica. / Horgan, Huw J.; Christianson, Knut; Jacobel, Robert W.; Anandakrishnan, Sridhar; Alley, Richard B.

In: Geophysical Research Letters, Vol. 40, No. 15, 16.08.2013, p. 3934-3939.

Research output: Contribution to journalArticle

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AU - Christianson, Knut

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AU - Alley, Richard B.

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