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Showing 1–10 of 10 results
Advanced filters: Author: Fabien Maussion Clear advanced filters

  • The ice volume of glaciers outside the Greenland and Antarctic ice sheets totals about 158,000 km3, with about 27% less ice in High Mountain Asia than thought, according to multiple models that estimate ice thickness from surface characteristics.

    • Daniel Farinotti
    • Matthias Huss
    • Ankur Pandit
    Research
    Nature Geoscience
    Volume: 12, P: 168-173

  • The tropical monsoon is thought to play a key role in glacier change in High Asia. The mass balance of a glacier in the southern Tibetan Plateau is found to be due to May/June precipitation, which is controlled by mid-latitude climate and the tropical monsoon. Further attention should be paid to mid-latitude climate to understand glacier changes.

    • Thomas Mölg
    • Fabien Maussion
    • Dieter Scherer
    Research
    Nature Climate Change
    Volume: 4, P: 68-73

  • How mountain glaciers will react to temporarily overshooting 1.5 °C of warming is poorly understood. Here the authors show irreversible global glacier loss for centuries after overshoot, implying long-term reductions in glacial water resources with amplified impacts in regions where glaciers regrow.

    • Lilian Schuster
    • Fabien Maussion
    • Carl-Friedrich Schleussner
    ResearchOpen Access
    Nature Climate Change
    Volume: 15, P: 634-641

  • Many mountain glaciers will disappear with warming. Here the authors assess how many glaciers will disappear per year under different warming scenarios, finding that a peak in glacier loss will happen during the mid-twenty-first century.

    • Lander Van Tricht
    • Harry Zekollari
    • Daniel Farinotti
    ResearchOpen Access
    Nature Climate Change
    Volume: 16, P: 143-147

  • Aiming for declining global temperatures can limit long-term climate risks compared with a mere stabilization of global warming, including sea-level rise and cryosphere changes.

    • Carl-Friedrich Schleussner
    • Gaurav Ganti
    • Joeri Rogelj
    ResearchOpen Access
    Nature
    Volume: 634, P: 366-373

  • 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

  • An intercomparison exercise reassesses mass loss from glaciers worldwide based on the main in situ and satellite methods from 2000 to 2023; the results are consistent with previous assessments and provide a refined and comprehensive observational baseline for future impact and modelling studies.

    • Michael Zemp
    • Livia Jakob
    • Whyjay Zheng
    ResearchOpen Access
    Nature
    Volume: 639, P: 382-388

  • Providing actionable climate information requires an end-user focused approach that links specific local climate risk thresholds with global emissions pathways.

    • Peter Pfleiderer
    • Thomas L. Frölicher
    • Carl-Friedrich Schleussner
    Reviews
    Nature Geoscience
    Volume: 18, P: 10-19

  • Glaciers outside Greenland and Antarctica have been rapidly losing mass. Contemporary ice declines are shown to be a response to past greenhouse gas emissions, with present mitigation efforts unlikely to be beneficial in preventing future short-term ice loss.

    • Ben Marzeion
    • Georg Kaser
    • Nicolas Champollion
    Research
    Nature Climate Change
    Volume: 8, P: 305-308