Present-day gravity changes induced by glacial isostatic adjustment from 
ensemble simulations with 3D Earth structures

Bagge, Meike; Klemann, V.; Dill, R.; Dobslaw, Henryk

doi:10.5880/GFZ.1.3.2023.002

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Present-day gravity changes induced by glacial isostatic adjustment from ensemble simulations with 3D Earth structures

Bagge, M., Klemann, V., Dill, R., Dobslaw, H. (2023): Present-day gravity changes induced by glacial isostatic adjustment from ensemble simulations with 3D Earth structures.
https://doi.org/10.5880/GFZ.1.3.2023.002

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Datensatz-Permalink: https://gfzpublic.gfz-potsdam.de/pubman/item/item_5024215 Versions-Permalink: https://gfzpublic.gfz-potsdam.de/pubman/item/item_5024215_3

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Urheber:
Bagge, Meike¹, Autor
Klemann, V.¹, Autor
Dill, R.¹, Autor
Dobslaw, Henryk¹, Autor

Affiliations:
11.3 Earth System Modelling, 1.0 Geodesy, Departments, GFZ Publication Database, Deutsches GeoForschungsZentrum, ou_146027

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Schlagwörter: Glacial isostatic adjustment (GIA); Gravity changes; Stoke's coefficients; GIA model ensemble; GRACE-F0

Zusammenfassung: We provide present-day glacial isostatic adjustment (GIA) gravity changes simulated with the numerical model VILMA. The effects of Earth and ocean pole tide due to rotational deformation (considered in VILMA) were removed. The dataset contains the solutions for 56 GIA model ensemble members including 54 3D models and 2 1D models. The results are provided as Stokes coefficients with a resolution of degree/order 170.