PLEASE READ FOR INFORMATION ON DATA

All data are in *.mat format, which contain Ice-Sheet and Sea-Level System 
Model 500-yr transient output for Thwaites and Pine Island glaciers as 
presented in the associated paper. Please refer to Schwans et al., 2023 for 
the particulars of each setting described below and finer details regarding 
workflow and output. Full list of models can be found in the publication's 
appendix.


Naming convention for output:


c/f = mesh resolution; either coarse (c) or fine (f) as described in 
  section 2.2

m1/m8 = choice of basal rheology via power-law sliding exponent, m; 
  either 1 (linear-viscous) or 8 (plastic) (see section 2.2.2)

h/l/p = sub-shelf melt scheme used; either static ocean forcing with high (h) 
  or low (l) inland-extrapolated values or dynamic forcing using PICOP 
  module (p) from Pelle et al., 2019. (see section 2.3.1)

subelon/subeloff = indicates whether subelement friction was enabled in 
  model run

if = ice-front prescription; either static (ifstat), dynamic (ifdyn), or 
  dynamic with the basal friction coefficient, alpha, extrapolated seaward 
  (ifdynxalpha) (see section 2.2.1/2.2.2)

smf/smb = shear-margin perturbation, if applied; either reduction in basal 
  friction (smf) or softening of the shear-margin ice fabric (smb) (see 
  section 2.3.2)


EX: f-m8-p-subelon-ifdyn.mat is a model that uses a fine mesh and simulates 
ice-flow over a plastic bed with the sliding-law coefficient set to 8, where 
ocean forcing is calculated by the PICOP module. This model resolves basal 
friction on a subelement basis, and uses a dynamic ice-front prescription, 
but without friction coefficient extrapolation. No shear-margin perturbation 
is applied.