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Glacier sliding, regelation water flow and development of basal ice

  • Peter G. Knight (a1) and Debbie A. Knight (a1)
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Boulton, G.S. 1975. Processes and patterns of subglacial sedimentation: a theoretical approach. In Wright, A. E. and Moseley, F. eds. Ice ages: ancient and modern. Liverpool, Seel House Press, 742.
Knight, P.G. 1987. Observations at the edge of the Greenland ice sheet: boundary condition implications for modellers. International Association of Hydrotogical Sciences Publication 170 (Symposium at Vancouver 1987. — The Physical Basis of Ice Sheet Modelling), 359366.
Knight, P. G., Sugden, D.E. and Minty, C. D. 1994. Ice flow around large obstacles as indicated by basal ice exposed at the margin of the Greenland ice sheet. J. Glacial., 40 (135), 359367.
Lawson, D.E. 1979. Sedimentological analysis of the western terminus of the Matanuska Glacier, Alaska. CRREL Rep. 799.
Lliboutry, L. 1986. A discussion of Robin’s “heat pump” effect by extending Nye’s model for the sliding of a temperate glacier. Eidg. Tech. Hochschule, Zürich. Versuchsanst. Wasserbau, Hydrat. Glazial. Mitt. 90, 7477.
Lliboutry, L. 1993. Internal melting and ice accretion at the bottom of temperate glaciers. J.Glaciol., 39 (131), 5064.
Mader, H.M. 1992. The thermal behaviour of the water-vein system in polycrystalline ice. J. Glacial., 38 (130), 359374.
Robin, G. de Q, 1976. Is the basal ice of a temperate glacier at the pressure melting point? J. Glacial., 16 (74), 183196.
Souchez, R. Lemmens, A., M., R, Lorrain., Tison, J. L., J, Jouzel and D, Sugden. 1990. Influence of hydroxyl-bearing minerals on the isotopic composition of ice from the basal zone of an ice sheet. Nature, 345 (6272), 244246.
Sugden, D.E. and 6 others. 1987. Evidence for two zones of debris entrainment beneath the Greenland ice sheet. Mature, 328 (6127.), 238241.
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Journal of Glaciology
  • ISSN: 0022-1430
  • EISSN: 1727-5652
  • URL: /core/journals/journal-of-glaciology
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