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TitleRevised estimates of Greenland ice sheet thinning histories based on ice-core records
AuthorLecavalier, B S; Milne, G A; Vinther, B M; Fisher, D A; Dyke, A S; Simpson, M J R
SourceQuaternary Science Reviews vol. 63, 2013 p. 73-82, https://doi.org/10.1016/j.quascirev.2012.11.030
Year2013
Alt SeriesEarth Sciences Sector, Contribution Series 20120429
PublisherElsevier BV
Documentserial
Lang.English
Mediapaper; on-line; digital
File formatpdf
AreaGreenland
Lat/Long WENS -72.0000 -12.0000 84.0000 60.0000
Subjectssurficial geology/geomorphology; ice; ice conditions; ice sheets; cores; core samples; sea level fluctuations; sea level changes; paleo-sea levels; Holocene; Greenland Ice Sheet; Renland ice cap; Agassiz ice cap; Cenozoic
Illustrationsgraphs; plots; location maps
AbstractIce core records were recently used to infer elevation changes of the Greenland ice sheet throughout the Holocene. The inferred elevation changes show a significantly greater elevation reduction than those output from numerical models, bringing into question the accuracy of the model-based reconstructions and, to some extent, the estimated elevation histories. A key component of the ice core analysis involved removing the influence of vertical surface motion on the d18O signal measured from the Agassiz and Renland ice caps. We re-visit the original analysis with the intent to determine if the use of more accurate land uplift curves can account for some of the above noted discrepancy. To improve on the original analysis, we apply a geophysical model of glacial isostatic adjustment calibrated to sea-level records from the Queen Elizabeth Islands and Greenland to calculate the influence of land height changes on the d18O signal from the two ice cores. This procedure is complicated by the fact that d18O contained in Agassiz ice is influenced by land height changes distant from the ice cap and so selecting a single location at which to compute the land height signal is not possible. Uncertainty in this selection is further complicated by the possible influence of Innuitian ice during the early Holocene (12e8 ka BP). Our results indicate that a more accurate treatment of the uplift correction leads to elevation histories that are, in general, shifted down relative to the original curves at GRIP, NGRIP, DYE-3 and Camp Century. In addition, compared to the original analysis, the 1-s uncertainty is considerably larger at GRIP and NGRIP. These changes reduce the data-model discrepancy reported by Vinther et al. (2009) at GRIP, NGRIP, DYE-3 and Camp Century. A more accurate treatment of isostasy and surface loading also acts to improve the data-model fits such that the residuals at all four sites for the period 8 ka BP to present are significantly reduced compared to the original analysis. Prior to 8 ka BP, the possible influence of Innuitian ice on the inferred elevation histories prevents a meaningful comparison.
GEOSCAN ID292320