❄ Fast and friendly glacial isostatic adjustment on CPU and GPU.
The two animations above visualise the results of FastIsostasy when forced by ICE6G_D and an external regional mean sea level:
- On the left, the anomaly of ice thickness with respect to the Last Interglacial and, on the right, the bedrock displacement resulting from it.
- A transect of Antarctica between the Thwaites and Amery glaciers.
This computation is performed with
FastIsostasy is a friendly and flexible model that regionally computes the glacial isostatic adjustment (GIA) with laterally-variable mantle viscosity and lithospheric thickness. It is mainly adressed to ice-sheet modellers who seek for (1) a good representation of solid-Earth mechanics at virtually zero computational cost, (2) an approximation of the sea-level equation and (3) ready-to-use inversion tools to calibrate the model parameters to data. The simple interface of FastIsostasy allows to flexibly solve GIA problems within few lines of code. Its open-source code is distributed under GPL3 license and was succesfully benchmarked against analytical, 1D GIA and 3D GIA model solutions.
FastIsostasy relies on a hybrid Fourier/finite-difference collocation of the problem introduced in Cathles (1975) and solved in Lingle and Clark (1985), Bueler et al. (2007). Thanks to a simplification of the full problem from 3D to 2D space and the use of optimized software packages, running kiloyears of regional GIA with
FastIsostasy.jl is a registered julia package. To install it, please run:
using Pkg
Pkg.add("FastIsostasy")
For more information on the model devlopment and validation, please check out our description paper, which should be cited as:
Swierczek-Jereczek, J., Montoya, M., Latychev, K., Robinson, A., Alvarez-Solas, J., & Mitrovica, J. (2024). FastIsostasy v1.0 – a regional, accelerated 2D glacial isostatic adjustment (GIA) model accounting for the lateral variability of the solid Earth. Geoscientific Model Development, 17(13), 5263-5290.