A successful Paris Climate Agreement could halve the ice we lose by 2100

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Sea level rise due to melting ice could be halved by 2100 relative to current forecasts if the Paris Climate Agreement reaches its best case scenario, according to international researchersThe team modelled the impact of limiting global warming to 1.5 degrees Celsius on land ice melting, and found the median sea level rise by 2100 as a result of land ice melting was 13 centimetres, compared with 25 centimetres based on current emissions reduction pledges. In a separate paper, modelling shows reducing global warming to two degrees Celsius or less could keep the Antarctic Ice Sheet melting at its current level, preventing a dramatic jump in ice loss in 40 years if current policies allowing three degrees of warming continue.

Journal/conference: Nature

Link to research (DOI): 10.1038/s41586-021-03302-y

Organisation/s: King’s College London, London, UK, University of Massachusetts Amhers, USA

Funder: Projected land ice contributions to twenty-first-century sea level rise: See paper for funding. The Paris Climate Agreement and future sea-level rise from Antarctica: This research was supported by the NSF under awards 1664013, 2035080, 1443347 and 1559040, and by a grant to the NASA Sea Level Change Team 80NSSC17K0698.

Media release

From: Springer Nature

Climate change: Assessing the impact of melting land ice on sea-level rise

Limiting global warming to 1.5 °C could halve contributions from melting land ice to 21st-century sea-level rise, relative to projections based on current emission pledges by 2100, suggests a paper published in Nature. A second paper, also published in Nature, indicates that warming of 3 °C could cause sea level to increase by 0.5 cm every year by 2100 as a result of melting Antarctic land ice. The findings provide further insight into the impact of melting land ice on global sea-level rises.

Since 1993, land ice has contributed to around half of all global sea-level rise and this contribution is expected to increase as the world warms. The Antarctic Ice Sheet is the largest land ice reservoir and its ice loss is accelerating. Complex ice sheet models can be used to project the contribution of land ice to sea-level rise, but they require massive computational power and cannot explore all possible outcomes, owing to uncertainties in the projections.

Tamsin Edwards and colleagues use a statistical and computationally efficient approach to emulate the behaviour of more-complex models to project glacier and ice sheet contributions to sea-level rise under a range of scenarios. They find that if the ambitious Paris Agreement target of limiting warming to 1.5 °C was met, the contribution of land ice to sea-level rise could be halved by 2100—from the median projected sea-level rise of 25 cm under current climate projections, to 13 cm. The authors also suggest that melting from the Greenland Ice Sheet would fall by around 70% and that the contribution of melting glaciers to sea-level rise would also halve. The authors indicate that there is no clear difference for Antarctica under different emissions scenarios, owing to uncertainties in the competing processes of snowfall accumulation and ice loss. However, if the most extreme ice sheet behaviour is assumed, Antarctic ice loss could be five times higher, which would increase median sea-level rise to 42 cm under current pledges.

In a separate modelling study, Robert DeConto and colleagues find that limiting warming to the Paris Agreement’s alternative target of 2 °C maintains roughly constant Antarctic ice loss at current rates. However, in a scenario with warming of 3 °C—the warming trajectory consistent with current fossil fuel emissions—the authors predict that the rate of ice loss will increase substantially from 2060, triggering sea-level increases of 0.5 cm per year by 2100. Once a threshold of rapid sea-level rise is reached, modelling of optimistic, yet theoretical, approaches to remove carbon dioxide from the atmosphere shows a reduction, but not cessation, of further sea-level rise over the coming centuries.

The two papers highlight that aggressive efforts to limit global warming will sharply reduce future sea-level rise. For Antarctica, Tamsin Edwards and colleagues find that the complexity of competing processes on the ice sheet make it difficult to make concrete predictions about its future, and Robert DeConto and colleagues show that it is keenly sensitive to warming of 3 °C and greater. Thus, for the largest body of ice on the planet, important uncertainties remain.

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  • Icebergs in Sermilik Fjord, SE Greenland
    Icebergs in Sermilik Fjord, SE Greenland

    Icebergs in Sermilik Fjord, SE Greenland

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  • Antarctic model simulations

    This animation shows the rate at which the ice thickness is changing in meters per year (more red/yellow means faster thinning and thus faster ice loss) as the Antarctic Ice Sheet responds to changes in the atmosphere and ocean due to one potential climate scenario. This simulation, using the BISICLES ice sheet model, represents one of hundreds of such simulations used for this work to characterize ice sheet response to changes in the climate.

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