Mantle Viscosity and Ice-Age Ice Sheet Topography

Ice-age paleotopography and mantle viscosity can both be inferred from observations of Earth's response to the most recent deglaciation event of the current ice age. This procedure requires iterative application of a theoretical model of the global process of glacial isostatic adjustment. Resul...

Full description

Bibliographic Details
Published in:Science
Main Author: Peltier, W. Richard
Format: Article in Journal/Newspaper
Language:English
Published: American Association for the Advancement of Science (AAAS) 1996
Subjects:
Online Access:http://dx.doi.org/10.1126/science.273.5280.1359
https://www.science.org/doi/pdf/10.1126/science.273.5280.1359
id craaas:10.1126/science.273.5280.1359
record_format openpolar
spelling craaas:10.1126/science.273.5280.1359 2024-04-28T08:24:54+00:00 Mantle Viscosity and Ice-Age Ice Sheet Topography Peltier, W. Richard 1996 http://dx.doi.org/10.1126/science.273.5280.1359 https://www.science.org/doi/pdf/10.1126/science.273.5280.1359 en eng American Association for the Advancement of Science (AAAS) Science volume 273, issue 5280, page 1359-1364 ISSN 0036-8075 1095-9203 Multidisciplinary journal-article 1996 craaas https://doi.org/10.1126/science.273.5280.1359 2024-04-09T06:40:50Z Ice-age paleotopography and mantle viscosity can both be inferred from observations of Earth's response to the most recent deglaciation event of the current ice age. This procedure requires iterative application of a theoretical model of the global process of glacial isostatic adjustment. Results demonstrate that the iterative inversion procedure converges to a paleotopography that is extremely close to that from the ICE-4G model. The accompanying mantle viscosity profile is furthermore shown to reconcile the requirements of aspherical geoid anomalies related to the mantle convection process, thus resolving a fundamental issue concerning mantle rheology. The combined model also explains postglacial sea level histories for the east coast of the United States. Article in Journal/Newspaper Ice Sheet AAAS Resource Center (American Association for the Advancement of Science) Science 273 5280 1359 1364
institution Open Polar
collection AAAS Resource Center (American Association for the Advancement of Science)
op_collection_id craaas
language English
topic Multidisciplinary
spellingShingle Multidisciplinary
Peltier, W. Richard
Mantle Viscosity and Ice-Age Ice Sheet Topography
topic_facet Multidisciplinary
description Ice-age paleotopography and mantle viscosity can both be inferred from observations of Earth's response to the most recent deglaciation event of the current ice age. This procedure requires iterative application of a theoretical model of the global process of glacial isostatic adjustment. Results demonstrate that the iterative inversion procedure converges to a paleotopography that is extremely close to that from the ICE-4G model. The accompanying mantle viscosity profile is furthermore shown to reconcile the requirements of aspherical geoid anomalies related to the mantle convection process, thus resolving a fundamental issue concerning mantle rheology. The combined model also explains postglacial sea level histories for the east coast of the United States.
format Article in Journal/Newspaper
author Peltier, W. Richard
author_facet Peltier, W. Richard
author_sort Peltier, W. Richard
title Mantle Viscosity and Ice-Age Ice Sheet Topography
title_short Mantle Viscosity and Ice-Age Ice Sheet Topography
title_full Mantle Viscosity and Ice-Age Ice Sheet Topography
title_fullStr Mantle Viscosity and Ice-Age Ice Sheet Topography
title_full_unstemmed Mantle Viscosity and Ice-Age Ice Sheet Topography
title_sort mantle viscosity and ice-age ice sheet topography
publisher American Association for the Advancement of Science (AAAS)
publishDate 1996
url http://dx.doi.org/10.1126/science.273.5280.1359
https://www.science.org/doi/pdf/10.1126/science.273.5280.1359
genre Ice Sheet
genre_facet Ice Sheet
op_source Science
volume 273, issue 5280, page 1359-1364
ISSN 0036-8075 1095-9203
op_doi https://doi.org/10.1126/science.273.5280.1359
container_title Science
container_volume 273
container_issue 5280
container_start_page 1359
op_container_end_page 1364
_version_ 1797584905438232576