Sea level and global ice volumes from the Last Glacial Maximum to the Holocene
By K. Lambeck, H. Rouby, Anthony W. Purcell, Yiying Sun, Malcolm Sambridge. Proceedings of the National Academy of Sciences of the United States of America, 2014
2,210 citations recorded by the source corpus.
Subfields: Archeology, Atmospheric Science, Earth-Surface Processes
View Paper: https://www.semanticscholar.org/paper/65aeb46cb3a99702f1218542a2cd27569c18e0ef
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Citations in the corpus
- GIA Model Statistics for GRACE Hydrology, Cryosphere, and Ocean Science (2018, methodology): “A scaled version of the ANU ice history (Lambeck et al., 2010, 2014) was employed, except for Antarctica and Patagonia where ice models having more contemporary constraints are available (Briggs & Tarasov, 2013; Ivins & James, 2004; Ivins et al., 2013; Whitehouse, Bentley, Milne, et al., 2012).”
- Glacial isostatic adjustment modelling: historical perspectives, recent advances, and future directions (2018, methodology): “Impressively, his estimate for the mean sea-level change associated with “the formation 155 of the Pleistocene ice-caps” was 130 m, a value that is almost identical to contemporary estimates (Lambeck et al., 2014).”
- Young People's Burden: Requirement of Negative CO2 Emissions (2016, positive): “◦ C from early Holocene maximum temperature to a “Little Ice Age” minimum in the early 1800s (that minimum being better defined by higher resolution data of Abram et al., 2016 Concatenation of the modern and Holocene temperature records (Fig.”