Recent mass balance of polar ice sheets inferred from patterns of global sea-level change

Jerry X. Mitrovica (), Mark E. Tamisiea, James L. Davis and Glenn A. Milne
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Jerry X. Mitrovica: University of Toronto
Mark E. Tamisiea: University of Toronto
James L. Davis: Harvard-Smithsonian Center for Astrophysics
Glenn A. Milne: University of Durham, Science Laboratories

Nature, 2001, vol. 409, issue 6823, 1026-1029

Abstract: Abstract Global sea level is an indicator of climate change1,2,3, as it is sensitive to both thermal expansion of the oceans and a reduction of land-based glaciers. Global sea-level rise has been estimated by correcting observations from tide gauges for glacial isostatic adjustment—the continuing sea-level response due to melting of Late Pleistocene ice—and by computing the global mean of these residual trends4,5,6,7,8,9. In such analyses, spatial patterns of sea-level rise are assumed to be signals that will average out over geographically distributed tide-gauge data. But a long history of modelling studies10,11,12 has demonstrated that non-uniform—that is, non-eustatic—sea-level redistributions can be produced by variations in the volume of the polar ice sheets. Here we present numerical predictions of gravitationally consistent patterns of sea-level change following variations in either the Antarctic or Greenland ice sheets or the melting of a suite of small mountain glaciers. These predictions are characterized by geometrically distinct patterns that reconcile spatial variations in previously published sea-level records. Under the—albeit coarse—assumption of a globally uniform thermal expansion of the oceans, our approach suggests melting of the Greenland ice complex over the last century equivalent to ∼0.6 mm yr-1 of sea-level rise.

Date: 2001
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DOI: 10.1038/35059054

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