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Showing 1–4 of 4 results
Advanced filters: Author: Faron S. Anslow Clear advanced filters

  • The demise of the Laurentide ice sheet during the early Holocene epoch allows rates of ice sheet decay under natural conditions to be assessed. Analysis of terrestrial and marine records of the deglaciation along with a climate model reveal two periods of rapid melting during the final retreat of this ice sheet, with rates of sea level rise of up to 1.3 cm per year.

    • Anders E. Carlson
    • Allegra N. LeGrande
    • Elizabeth A. Obbink
    Research
    Nature Geoscience
    Volume: 1, P: 620-624

  • The glaciers in western Canada are experiencing rapid mass loss. Projections of their fate with a model that couples physics-based ice dynamics with a surface mass balance model suggest that glacier volume will shrink by 70% by 2100.

    • Garry K. C. Clarke
    • Alexander H. Jarosch
    • Brian Menounos
    Research
    Nature Geoscience
    Volume: 8, P: 372-377

  • The factors leading to the full retreat of ice sheets during deglaciation are debated. Numerical modelling suggests that the Laurentide ice sheet retreated only after a threshold for warming and radiative forcing was passed in the Holocene.

    • David J. Ullman
    • Anders E. Carlson
    • Joseph M. Licciardi
    Research
    Nature Geoscience
    Volume: 8, P: 534-537