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Showing 1–4 of 4 results
Advanced filters: Author: Reinhard Calov Clear advanced filters

  • The most pronounced deglaciation of Greenland of the last several hundred thousand years occurred during Marine Isotope Stage 11. Here, the authors show that it was the exceptional duration of the interglacial period that allowed Greenland to melt even though temperatures were only moderately warmer than today.

    • Alexander Robinson
    • Jorge Alvarez-Solas
    • Marisa Montoya
    ResearchOpen Access
    Nature Communications
    Volume: 8, P: 1-7

  • Efficient statistical emulation of melting land ice under various climate scenarios to 2100 indicates a contribution from melting land ice to sea level increase of at least 13 centimetres sea level equivalent.

    • Tamsin L. Edwards
    • Sophie Nowicki
    • Thomas Zwinger
    Research
    Nature
    Volume: 593, P: 74-82

  • A comprehensive stability analysis shows that the critical global temperature rise that leads to collapse of the Greenland ice sheet is only 1–2 °C above the pre-industrial climate state, which is significantly lower than previously believed.

    • Alexander Robinson
    • Reinhard Calov
    • Andrey Ganopolski
    Research
    Nature Climate Change
    Volume: 2, P: 429-432

  • Basal melting is widespread in the north-central Greenland ice sheet. Geophysical data and numerical modelling suggest a geothermal anomaly in this region resulting from the earlier passage of Greenland over the Iceland mantle plume.

    • Irina Rogozhina
    • Alexey G. Petrunin
    • Ivan Koulakov
    Research
    Nature Geoscience
    Volume: 9, P: 366-369