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    Multistability and critical thresholds of the Greenland ice sheet

    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 significantl...

    Alexander Robinson, Reinhard Calov, Andrey Ganopolski in Nature Climate Change (2012)

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    Article

    Exceptional twentieth-century slowdown in Atlantic Ocean overturning circulation

    Possible changes in Atlantic meridional overturning circulation (AMOC) provide a key source of uncertainty regarding future climate change. Maps of temperature trends over the twentieth century show a conspicu...

    Stefan Rahmstorf, Jason E. Box, Georg Feulner, Michael E. Mann… in Nature Climate Change (2015)

  3. Article

    Correction: Corrigendum: Evidence for an exceptional twentieth-century slowdown in Atlantic Ocean overturning

    Nature Clim. Change 5, 475–480 (2015); published online 23 March 2015; corrected after print 3 September 2015 In the version of this Article originally published, in Fig. 1 the data plotted were for the calend...

    Stefan Rahmstorf, Jason Box, Georg Feulner, Michael E. Mann… in Nature Climate Change (2015)

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    The Greenland and Antarctic ice sheets under 1.5 °C global warming

    Even if anthropogenic warming were constrained to less than 2 °C above pre-industrial, the Greenland and Antarctic ice sheets will continue to lose mass this century, with rates similar to those observed over ...

    Frank Pattyn, Catherine Ritz, Edward Hanna, Xylar Asay-Davis… in Nature Climate Change (2018)

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    Article

    Only halving emissions by 2030 can minimize risks of crossing cryosphere thresholds

    Considering cryosphere and warming uncertainties together implies drastically increased risk of threshold crossing in the cryosphere, even under lower-emission pathways, and underscores the need to halve emiss...

    Uta Kloenne, Alexander Nauels, Pam Pearson, Robert M. DeConto… in Nature Climate Change (2023)