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The new digital elevation model was gridded in a similar way to previous grids (Fretwell et al. 2008, Dickens et al. 2014). Gridded datasets were resampled to 200 m resolution and then converted to point data. These points were then given a quality hierarchy; multibeam swath being the highest, then towed data, singlebeam and finally gridded GEBCO and IBSCO data. The data were then re-gridded using the Topogrid algorithm in ArcGIS using the hierarchy to prioritize the data. The resulting grid was then checked for errors such as spikes and holes. Where identified, these were removed from the point datasets and the data were re-gridded. This iterative process was conducted until a clean combined dataset was produced.&#xD;
On land raw ASTER GDEM grids were cleaned and merged with pre-existing survey data to create new digital elevation models and supplemented by coastlines and form-lines taken from archival sketch-maps to produce a full hypsometric elevation model for each island. The bathymetry and elevation dataset was merged and gridded using ArcGIS 10.
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