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Glacial Isostasy:Regional—Not Global
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作者 Nils-Axel Morner 《International Journal of Geosciences》 2015年第6期577-592,共16页
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 reg... 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. 展开更多
关键词 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
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