GIS dataset of high-resolution rebound surfaces and ice-free paleotopography of glaciated North America since the LGM based on the ICE-xG (VMy) models' predictions ...
The postglacial rebound is component of the glacial isostatic adjustment which causes the Earth's crust to rebound in regions formerly covered by or adjacent to ice sheets, and subside beneath ocean basins. In North America, the observed postglacial rebound is mainly the result of the Laurentid...
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ftdatacite:10.1594/pangaea.947536 2024-03-31T07:53:20+00:00 GIS dataset of high-resolution rebound surfaces and ice-free paleotopography of glaciated North America since the LGM based on the ICE-xG (VMy) models' predictions ... Godbout, Pierre-Marc Brouard, Etienne Roy, Martin 2022 text/tab-separated-values https://dx.doi.org/10.1594/pangaea.947536 https://doi.pangaea.de/10.1594/PANGAEA.947536 en eng PANGAEA https://dx.doi.org/10.1038/s41597-023-02566-5 Creative Commons Attribution 4.0 International https://creativecommons.org/licenses/by/4.0/legalcode cc-by-4.0 File content Binary Object Binary Object File Size Model dataset Dataset 2022 ftdatacite https://doi.org/10.1594/pangaea.94753610.1038/s41597-023-02566-5 2024-03-04T13:55:22Z The postglacial rebound is component of the glacial isostatic adjustment which causes the Earth's crust to rebound in regions formerly covered by or adjacent to ice sheets, and subside beneath ocean basins. In North America, the observed postglacial rebound is mainly the result of the Laurentide Ice Sheet deglaciation after it reached its maximum thickness and extent at the Last Glacial Maximum (26.5-19 ka). Global-scale numerical models of glacial isostatic adjustment faithfully reproduce past and current changes in postglacial rebound, but the integration their predictions in a geographic information system to facilitate high-resolution paleotopographic reconstructions remains challenging. We therefore present high-resolution raster datasets of land-deformation and ice-free paleotopography of glaciated North America for several time slices since the Last Glacial Maximum to support geological, paleoenvironmental and archeological studies. ... Dataset Ice Sheet DataCite Metadata Store (German National Library of Science and Technology) |
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DataCite Metadata Store (German National Library of Science and Technology) |
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English |
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File content Binary Object Binary Object File Size Model Godbout, Pierre-Marc Brouard, Etienne Roy, Martin GIS dataset of high-resolution rebound surfaces and ice-free paleotopography of glaciated North America since the LGM based on the ICE-xG (VMy) models' predictions ... |
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File content Binary Object Binary Object File Size Model |
description |
The postglacial rebound is component of the glacial isostatic adjustment which causes the Earth's crust to rebound in regions formerly covered by or adjacent to ice sheets, and subside beneath ocean basins. In North America, the observed postglacial rebound is mainly the result of the Laurentide Ice Sheet deglaciation after it reached its maximum thickness and extent at the Last Glacial Maximum (26.5-19 ka). Global-scale numerical models of glacial isostatic adjustment faithfully reproduce past and current changes in postglacial rebound, but the integration their predictions in a geographic information system to facilitate high-resolution paleotopographic reconstructions remains challenging. We therefore present high-resolution raster datasets of land-deformation and ice-free paleotopography of glaciated North America for several time slices since the Last Glacial Maximum to support geological, paleoenvironmental and archeological studies. ... |
format |
Dataset |
author |
Godbout, Pierre-Marc Brouard, Etienne Roy, Martin |
author_facet |
Godbout, Pierre-Marc Brouard, Etienne Roy, Martin |
author_sort |
Godbout, Pierre-Marc |
title |
GIS dataset of high-resolution rebound surfaces and ice-free paleotopography of glaciated North America since the LGM based on the ICE-xG (VMy) models' predictions ... |
title_short |
GIS dataset of high-resolution rebound surfaces and ice-free paleotopography of glaciated North America since the LGM based on the ICE-xG (VMy) models' predictions ... |
title_full |
GIS dataset of high-resolution rebound surfaces and ice-free paleotopography of glaciated North America since the LGM based on the ICE-xG (VMy) models' predictions ... |
title_fullStr |
GIS dataset of high-resolution rebound surfaces and ice-free paleotopography of glaciated North America since the LGM based on the ICE-xG (VMy) models' predictions ... |
title_full_unstemmed |
GIS dataset of high-resolution rebound surfaces and ice-free paleotopography of glaciated North America since the LGM based on the ICE-xG (VMy) models' predictions ... |
title_sort |
gis dataset of high-resolution rebound surfaces and ice-free paleotopography of glaciated north america since the lgm based on the ice-xg (vmy) models' predictions ... |
publisher |
PANGAEA |
publishDate |
2022 |
url |
https://dx.doi.org/10.1594/pangaea.947536 https://doi.pangaea.de/10.1594/PANGAEA.947536 |
genre |
Ice Sheet |
genre_facet |
Ice Sheet |
op_relation |
https://dx.doi.org/10.1038/s41597-023-02566-5 |
op_rights |
Creative Commons Attribution 4.0 International https://creativecommons.org/licenses/by/4.0/legalcode cc-by-4.0 |
op_doi |
https://doi.org/10.1594/pangaea.94753610.1038/s41597-023-02566-5 |
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1795032950682681344 |