The thinning of floating ice shelves around Antarctica enhances upstream ice flow, contributing to sea-level rise. Ice-shelf thinning is now shown to influence glacial movement over much larger distances than previously thought.
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Hogg, A. E. & Gudmundsson, G. H. Nat. Clim. Change 7, 540–542 (2017).
Fretwell, P. et al. Cryosphere http://doi.org/f22853 (2013).
Reese, R. et al. Nat. Clim. Change https://doi.org/10.1038/S41558-017-0020-x (2017).
Rignot, E. et al. Geophys. Res. Lett. 31, L18401 (2004).
Scambos, T. A., Bohlander, J. A., Shuman, C. A. & Skvarca, P. Geophys. Res. Lett. 31, L18402 (2004).
Rignot, E. et al. Science 34, 6143 (2013).
Lenaerts, J. T. M. et al. Nat. Clim. Change 7, 58–62 (2017).
Fürst, J. J. et al. Nat. Clim. Change 6, 479–482 (2016).
Ritz, C. et al. Nature 528, 115 (2015).
DeConto, R. M. & Pollard, D. Nature 531, 591–597 (2016).
Pattyn, F. et al. Current Clim. Change Rep. 3.3, 174–184 (2017).
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Gagliardini, O. The health of Antarctic ice shelves. Nature Clim Change 8, 15–16 (2018). https://doi.org/10.1038/s41558-017-0037-1
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