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Lookup NU author(s): Professor Andrew RussellORCiD
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We present evidence of glaciohydraulic supercooling under jökulhlaup and ablation-dominated conditions from two temperate Icelandic glaciers. Observations show that freezing of sediment-laden meltwater leads to intraglacial debris entrainment during normal and extreme hydrological regimes. Intraglacial frazil ice propagation under normal ablation-dominated conditions can trap copious volumes of sediment, which forms anomalously thick outcrops of debris-rich ice. Glaciohydraulic supercooling plays an important role in intraglacial debris entrainment and should be given more attention in models of basal ice development. Extreme jökulhlaup conditions can result in significant intraglacial sediment accretion by supercooling, which may explain the concentration of englacial sediments deposited in Heinrich layers in the North Atlantic during the last glaciation.
Author(s): Roberts MJ, Tweed FS, Russell AJ, Knudsen Ó, Lawson DE, Larson GJ, Evenson EB, Björnsson H
Publication type: Article
Publication status: Published
Journal: Geology
Year: 2002
Volume: 30
Issue: 5
Pages: 439-442
ISSN (print): 0091-7613
ISSN (electronic): 1943-2682
URL: http://dx.doi.org/10.1130/0091-7613(2002)030<0439:GSII>2.0.CO;2
DOI: 10.1130/0091-7613(2002)030<0439:GSII>2.0.CO;2
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