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Showing 1–11 of 11 results
Advanced filters: Author: Natalya Gomez Clear advanced filters

  • The retreat of the Antarctic Ice Sheet and its potential contribution to future sea-level rise, is a major focus of climate research. Here, the authors show that positive feedbacks involving bedrock uplift and sea surface drop, may significantly impact the timing and extent of local ice-sheet retreat.

    • Natalya Gomez
    • David Pollard
    • David Holland
    ResearchOpen Access
    Nature Communications
    Volume: 6, P: 1-8

  • Interactive climate and ice sheet simulations project substantial East Antarctic ice loss under high emissions, amplified regional sea level rise in the Pacific, and enhanced northern latitude warming despite dampened global mean temperature rise.

    • Shaina Sadai
    • Ambarish V. Karmalkar
    • Alan Condron
    ResearchOpen Access
    Nature Communications
    Volume: 16, P: 1-13

  • Models of the West Antarctic Ice Sheet predict substantial ice loss over the next few centuries — and that a glacier expected to contribute greatly to sea-level rise may already be unstable.

    • Natalya Gomez
    News & Views
    Nature
    Volume: 526, P: 510-511

  • Climate change could potentially destabilize marine ice sheets such as the West Antarctic ice sheet. A suite of predictions of sea-level change following grounding-line migration suggests that the gravitational effects of melting on local sea levels can exert a stabilizing influence on marine ice sheets on a reverse slope.

    • Natalya Gomez
    • Jerry X. Mitrovica
    • Peter U. Clark
    Research
    Nature Geoscience
    Volume: 3, P: 850-853

  • An observationally calibrated ice sheet–shelf model suggests that global warming of 3 °C will trigger rapid Antarctic ice loss, contributing about 0.5 cm per year of sea-level rise by 2100.

    • Robert M. DeConto
    • David Pollard
    • Andrea Dutton
    Research
    Nature
    Volume: 593, P: 83-89

  • Increased meltwater from the Greenland and Antarctic ice sheets will slow the Atlantic overturning circulation and warm the subsurface ocean around Antarctica, further increasing Antarctic ice loss.

    • Nicholas R. Golledge
    • Elizabeth D. Keller
    • Tamsin L. Edwards
    Research
    Nature
    Volume: 566, P: 65-72

  • The evolution of the Antarctic Ice Sheet is driven by a combination of climate forcing and non-climatic feedbacks. In this review, the authors focus on feedbacks between the Antarctic Ice Sheet and the solid Earth, and the role of these feedbacks in shaping the response of the ice sheet to past and future climate changes.

    • Pippa L. Whitehouse
    • Natalya Gomez
    • Douglas A. Wiens
    ReviewsOpen Access
    Nature Communications
    Volume: 10, P: 1-14