Subglacial floods beneath ice sheets

G. W. Evatt, A. C. Fowler, C. D. Clark, N. R.J. Hulton

Research output: Contribution to journalArticlepeer-review

Abstract

Subglacial floods (jökulhlaups) are well documented as occurring beneath present day glaciers and ice caps. In addition, it is known that massive floods have occurred from ice-dammed lakes proximal to the Laurentide ice sheet during the last ice age, and it has been suggested that at least one such flood below the waning ice sheet was responsible for a dramatic cooling event some 8000 years ago. We propose that drainage of lakes from beneath ice sheets will generally occur in a time-periodic fashion, and that such floods can be of severe magnitude. Such hydraulic eruptions are likely to have caused severe climatic disturbances in the past, and may well do so in the future.

Original languageEnglish
Pages (from-to)1769-1794
Number of pages26
JournalPhilosophical Transactions of the Royal Society A: Mathematical, Physical and Engineering Sciences
Volume364
Issue number1844
DOIs
Publication statusPublished - 15 Jul 2006
Externally publishedYes

Keywords

  • Dansgaard-Oeschger events
  • Ice sheets
  • Jökulhlaups
  • Sub-Antarctic lakes
  • Subglacial hydrology

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