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  1. No Access

    Article

    Twentieth-century contribution to sea-level rise from uncharted glaciers

    Global-mean sea-level rise (GMSLR) during the twentieth century was primarily caused by glacier and ice-sheet mass loss, thermal expansion of ocean water and changes in terrestrial water storage1. Whether based o...

    David Parkes, Ben Marzeion in Nature (2018)

  2. No Access

    Article

    Projected land ice contributions to twenty-first-century sea level rise

    The land ice contribution to global mean sea level rise has not yet been predicted1 using ice sheet and glacier models for the latest set of socio-economic scenarios, nor using coordinated exploration of uncertai...

    Tamsin L. Edwards, Sophie Nowicki, Ben Marzeion, Regine Hock, Heiko Goelzer… in Nature (2021)

  3. Article

    Open Access

    Global and regional ocean mass budget closure since 2003

    In recent sea level studies, discrepancies have arisen in ocean mass observations obtained from the Gravity Recovery and Climate Experiment and its successor, GRACE Follow-On, with GRACE estimates consistently...

    Carsten Bjerre Ludwigsen, Ole Baltazar Andersen, Ben Marzeion… in Nature Communications (2024)

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  4. Article

    Open Access

    Heterogeneous impacts of ocean thermal forcing on ice discharge from Greenland's peripheral tidewater glaciers over 2000–2021

    The Greenland Ice Sheet is losing mass at increasing rates. Substantial amounts of this mass loss occur by ice discharge which is influenced by ocean thermal forcing. The ice sheet is surrounded by thousands o...

    Marco Möller, Beatriz Recinos, Philipp Rastner, Ben Marzeion in Scientific Reports (2024)

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