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&#xD;
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These simulations explore the effects of spatial model resolution on sea level projections. We take the bedmachine version 3 data set at 500 metre resolution and resample in order to get the required resolution. For each resolution lower than 500 metres, there are thus numerous different bed realisations. We select a number of these at each resolution, as described in Williams et al. (2023). The bed topography is included in each netCDF file, along with a bed_ref scalar coordinate variable to identify it (numerical value used to distinguish between different bed realisations at each resolution). Details of all other datasets can be found in Williams et al. (2023).&#xD;
&#xD;
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The initialisation algorithm used was evaluated on idealised test cases as described by Arthern and Gudmundsson (2010). Arthern et al (2015) shows maps of discrepancy between model velocity and satellite derived velocity, and histograms of the differences between model elevation changes and elevation changes derived using satellite altimetry. The WAVI.jl package has standard tests to check the performance of the code. These are documented in WAVI.jl/test. A value of -9999 indicates there are no data there.</gco:CharacterString>
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