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Showing 1–12 of 12 results
Advanced filters: Author: Luke D. Trusel Clear advanced filters

  • Coastal west Greenland ice caps fluctuated strongly compared to the interior in response to rapid Common Era changes in snow accumulation, according to modelling of proxy records developed from a Nuussuaq Peninsula ice core covering the last 2,000 years.

    • Matthew B. Osman
    • Benjamin E. Smith
    • Harald Sodemann
    Research
    Nature Geoscience
    Volume: 14, P: 756-761

  • Surface meltwater plays a key role in ice shelf stability, and consequently, Antarctica’s sea level contributions. New satellite observations suggest there is substantially more surface meltwater than previously thought, and models are underestimating it.

    • Luke D. Trusel
    News & Views
    Nature Geoscience
    Volume: 17, P: 588-589

  • Satellite observations reveal that the Conger–Glenzer Ice Shelf collapse in East Antarctica occurred in four stages spanning a period of 25 years, culminating in its rapid disintegration in March 2022.

    • Catherine C. Walker
    • Joanna D. Millstein
    • Helen A. Fricker
    Research
    Nature Geoscience
    Volume: 17, P: 1240-1248

  • High-resolution 2-km Antarctic maps reveal higher snowfall and surface melt than low-resolution products, reconciling satellite-observed ice sheet mass change. Projected higher surface melt near grounding lines threatens future ice shelf stability.

    • Brice Noël
    • J. Melchior van Wessem
    • Michiel R. van den Broeke
    ResearchOpen Access
    Nature Communications
    Volume: 14, P: 1-11

  • 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

  • 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 Antarctic Peninsula is one of the most rapidly warming regions on Earth. A reconstruction of ice melt from an ice core taken near the northeastern tip of the peninsula over the past 2,000 years shows that surface melt has accelerated during the twentieth century.

    • Nerilie J. Abram
    • Robert Mulvaney
    • Carol Arrowsmith
    Research
    Nature Geoscience
    Volume: 6, P: 404-411

  • A continuous, multi-century record of subarctic Atlantic marine productivity shows that a marked decline in net primary productivity has occurred across the subarctic Atlantic basin over the past two centuries.

    • Matthew B. Osman
    • Sarah B. Das
    • Eric S. Saltzman
    Research
    Nature
    Volume: 569, P: 551-555

  • With warming, meltwater will play an increasingly important role in driving ice loss from Antarctica, raising global sea levels. This Perspective discusses the key process through which Antarctic surface hydrology impacts mass balance.

    • Robin E. Bell
    • Alison F. Banwell
    • Jonathan Kingslake
    Reviews
    Nature Climate Change
    Volume: 8, P: 1044-1052

  • This Review synthesizes knowledge on projections of the Antarctic and Greenland ice sheets at 1.5 °C and 2 °C of warming, discussing possible nonlinear responses, and outlining the need for more insight into future atmospheric and oceanic forcings.

    • Frank Pattyn
    • Catherine Ritz
    • Michiel van den Broeke
    Reviews
    Nature Climate Change
    Volume: 8, P: 1053-1061