Sea-level reconstructions suggest significant contributions from the East Antarctic Ice Sheet may be required to reconcile high interglacial sea levels. Understanding the mechanism(s) that drove this loss is critical to projecting our future commitment to sea-level rise.
CITATION STYLE
Fogwill, C. J., Golledge, N., Millman, H., & Turney, S. (2016). The East Antarctic Ice Sheet as a source of sea-level rise: A major tipping element in the climate system? Past Global Change Magazine, 24(1), 8–9. https://doi.org/10.22498/pages.24.1.8
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