LM17.3 - a global vertical land motion model of glacial isostatic adjustment ...

We provide a global 0.5-degree grid of vertical land motion (in mm/a) of the LM17.3 glacial isostatic adjustment (GIA) model. The radially varying earth model part is profile VM5a (Peltier et al. 2015). The ice load is different to any other GIA model and combines regional ice loads without taking c...

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Bibliographic Details
Main Authors: Steffen, Holger, Li, Tanghua, Wu, Patrick, Gowan, Evan J, Ivins, Erik, Lecavalier, Benoit, Tarasov, Lev, Whitehouse, Pippa L
Format: Dataset
Language:English
Published: PANGAEA 2021
Subjects:
glacial isostatic adjustment
sea level
European Gravity Service for Improved Emergency Management EGSIEM
Barents Sea
Briggs
Greenland
New Zealand
Patagonia
Peltier
Antarc*
Antarctica
Fennoscandia
Iceland
Online Access:https://dx.doi.org/10.1594/pangaea.932462
https://doi.pangaea.de/10.1594/PANGAEA.932462
Description
Summary:We provide a global 0.5-degree grid of vertical land motion (in mm/a) of the LM17.3 glacial isostatic adjustment (GIA) model. The radially varying earth model part is profile VM5a (Peltier et al. 2015). The ice load is different to any other GIA model and combines regional ice loads without taking care of balancing the global sea-level equivalent of all ice sheets and glaciers with that expected from paleo-sea-level indicators. The regional models are:* GLAC-1D for North America (Tarasov et al. 2012),* HUY3 for Greenland (Lecavalier et al. 2014),* GLAC #71340 for Fennoscandia/Barents Sea (Tarasov et al., 2014),* ANU-ICE for Iceland, High Mountain Areas, Siberian Mountains and Tibet (Lambeck et al. 2014),* IJ04_Patagonia for Patagonia (updated from Ivins & James 2004),* ICE-6G_C for New Zealand (Argus et al. 2014, Peltier et al. 2015),* GLAC-1D for Antarctica (Briggs et al. 2014).Additional models (W12, Whitehouse et al. 2012, and IJ05_R2, Ivins et al. 2013, for Antarctica; ANU-ICE, Lambeck et al. 2017, ...

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