Nature Communications (Apr 2020)

Sediment controls dynamic behavior of a Cordilleran Ice Stream at the Last Glacial Maximum

  • Ellen A. Cowan,
  • Sarah D. Zellers,
  • Juliane Müller,
  • Maureen H. Walczak,
  • Lindsay L. Worthington,
  • Beth E. Caissie,
  • Wesley A. Clary,
  • John M. Jaeger,
  • Sean P. S. Gulick,
  • Jacob W. Pratt,
  • Alan C. Mix,
  • Stewart J. Fallon

DOI
https://doi.org/10.1038/s41467-020-15579-0
Journal volume & issue
Vol. 11, no. 1
pp. 1 – 9

Abstract

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Tidewater glaciers in fjords can advance/retreat independent of climate due to stabilization by sediments at their termini. We show that an Alaskan paleo-ice stream behaved similarly on an open shelf, suggesting that increased sediment flux may delay catastrophic retreat of outlet glaciers in a warming world.