Three-dimensional velocity variations due to ice mass changes in Greenland – Insights from a compressible glacial isostatic adjustment model ...
<!--!introduction!--> Glacial isostatic adjustment (GIA) models provide estimates for velocity, gravity and sea-level change based on ice loading scenarios of past glaciations. The input to GIA models is quite extensive and consists of ice histories and a variety of Earth model parameters that...
| Main Authors: | , , , , , |
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| Format: | Conference Object |
| Language: | unknown |
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GFZ German Research Centre for Geosciences
2023
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| Online Access: | https://dx.doi.org/10.57757/iugg23-0512 https://gfzpublic.gfz-potsdam.de/pubman/item/item_5016991 |
| Summary: | <!--!introduction!--> Glacial isostatic adjustment (GIA) models provide estimates for velocity, gravity and sea-level change based on ice loading scenarios of past glaciations. The input to GIA models is quite extensive and consists of ice histories and a variety of Earth model parameters that describe the three-dimensional (3D) structure and rheology. Here, we will show the effect of a range of lithospheric thickness models on vertical and horizontal velocities in Greenland using a 3D compressible GIA Earth model. The lithospheric thickness beneath and around Greenland varies from a few tens of kilometres in offshore regions to several tens of kilometres (up to 200 – 250 km) in land areas. However, to date, no one has done an analysis of the impact of lateral lithospheric variation on the 3D velocity field for Greenland as horizontal velocities from incompressible GIA models, which are commonly used, are not suitable to be used due to the neglect of material parameter changes related to the ... : The 28th IUGG General Assembly (IUGG2023) (Berlin 2023) ... |
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