Model output for Chester et al. (2024): On the origin of Holocene sea-level transgressions in formerly glaciated regions

Model output files and post-processing/plotting scripts for Chester et al. (2024, QSR). This repository contains: Files for reproducing figures: hingeline_tracker_zenodo.m. This code takes GIA model output and identifies the hinge line for a given transect following Chester et al. (2024) (e.g. Figures 4-6). transgression_magnitude_id_loop_zenodo.m. This code takes GIA model output and identifies and magnitude of a transgression and timing of the highstand for a given region (e.g. Figures 9, 10 and 12 in Chester et al., 2024). Zip files with GIA model output in .mat form: LN-SL_ICE7G_100km_plusBestFitting.zip: output from the LN-SL model with the ICE7G reconstruction, a 100 km lithosphere, and a range of viscosity values. The folder also includes the output from the two best-fitting simulations used to create Figures 9 and 10 in Chester et al. (2024). LN-NO_ICE7G_100km.zip: output from the LN-NO model with the ICE7G reconstruction, a lithospheric thickness of 100 km, and a range of mantle viscosities. FN-NO_discload_figure_3.zip: output from two simulations with the FN-NO model. The model was run with the disc load ice sheet and the two earth structures used in Figure 3. For GIA model runs with different parameter combinations please contact me at: [e-mail]. Note on file labeling: 'rsl_ice7g.l60CC.ump1.lm10.mat' translates to, ice model: ICE7G, lithospheric thickness: 60 km, upper mantle viscosity: 0.1 * 10^21 Pa s, lower mantle viscosity: 10 * 10^21 Pa s.