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Clark, J.A. (1980) A Numerical Model of Worldwide Sea Level Changes on a Viscoelastic Earth. In: M?rner, N.-A., Ed., Earth Rheology, Isostasy and Eustasy, John Wiley & Sons, London, 525-534.

has been cited by the following article:

• TITLE: Glacial Isostasy: Regional—Not Global

  AUTHORS: Nils-Axel Mörner

  KEYWORDS: Glacial Isostasy, Fennoscandia, Postglacial Uplift, Uplift Cone, Subsidences Trough, Forebulge, Low Viscosity Channel Flow, Global Sea Level Data, Correcting Satellite Altimetry, Removing Global GIA Correction

  JOURNAL NAME: International Journal of Geosciences, Vol.6 No.6, June 18, 2015

  ABSTRACT: The load of the continental ice caps of the Ice Ages deformed the bedrock, and when the ice melted in postglacial time, land rose. This process is known as glacial isostasy. The deformations are compensated either regionally or globally. Fennoscandian data indicate a regional compensation. Global sea level data support a regional, not global, compensation. Subtracting GIA corrections from satellite altimetry records brings—for the first time—different sea level indications into harmony of a present mean global sea level rise of 0.0 to 1.0 mm/yr.