However, some scenarios alternatively suggest that the volume added to the ice sheet by snowfall will surpass what is lost through melting, partially offsetting the rise - by 7.8 cm at best. This wide range in estimates [2] mainly reflects incomplete knowledge of melting that occurs on the bottom of ice shelves. But these floating glacial fringes, which can cover an area half the size of France, pen in the rest of the ice sheet. Were they to be lost, the new projections indicate that the ocean would rise several meters over 500 years. Over the same 2015–2100 period, the Greenland Ice Sheet would contribute an additional 1.5 to 14 cm, depending on the level of our greenhouse gas emissions. These findings have been discussed in a spate of scientific articles, including five published in The Cryosphere on 17 September 2020. To refine their predictions, scientists are turning to a new generation of climate models that directly integrate data on the cryosphere, in addition to atmospheric, oceanic, and biogeochemical inputs.

 

1. Working at the Institute of Environmental Geosciences (CNRS/Université Grenoble Alpes/IRD/Grenoble INP) and Laboratory for Sciences of Climate and Environment (CNRS/CEA/UVSQ). These labs are members of the Observatoire des sciences de l’Univers de Grenoble and Institut Pierre Simon Laplace, respectively.
2. These estimates are higher than previous ones: the 2019 IPCC Special Report on the Ocean and Cryosphere in a Changing Climate posited that melting of the Antarctic Ice Sheet would account for 3 to 28 cm of sea level rise between 2000 and 2100. However, not only have an insufficient number of studies been conducted, but those available based their findings on simpler models of the interactions between ice, the ocean, and the atmosphere.