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Annual Report for 2010/11 and Forward Programme - Sellafield Ltd

Annual Report for 2010/11 and Forward Programme - Sellafield Ltd

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3.3 Interpretation of gross geomorphological features (objective 2)Although bed<strong>for</strong>m features cannot be identified from the 2009 swath bathymetry data, agross interpretation of the morphological changes can be attempted. After gridding the 2002<strong>and</strong> 2009 surveys in the Fledermaus package on a similar basis, the volumetric differencebetween the surfaces was calculated. This was then exported <strong>for</strong> visualisation in a GISpackage as shown in Figure 8. This revealed apparent differences in elevation, but there aresignificant uncertainties associated with interpretation due to differences in relative coverageof swath (‘complete’) vs. single beam (

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