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The ABCS Program for the Analysis of Echo Sounder Returns for ...

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DSTO-GD-0215Appendix 1: Returned Ping Shape and EnergyVariations with Seafloor Depth<strong>The</strong> shape and energy <strong>of</strong> <strong>the</strong> returned signal can change significantly with seafloordepth (see Figure 13) as a result <strong>of</strong> ping dilation or compression, spreading losses, andabsorption.-60Returned Signal Power (dB re W)-90-12010m depth20m depth30m depth40m depth50m depth60m depth-1500 0.1 0.2 0.3Time (sec)Figure 13: How seafloor depth effects <strong>the</strong> returned signal. Calculated using Levels.Ping Dilation or CompressionWhen <strong>the</strong> depth <strong>of</strong> water changes, <strong>the</strong> start time <strong>of</strong> <strong>the</strong> returned ping changes alongwith <strong>the</strong> duration <strong>of</strong> <strong>the</strong> ping. <strong>The</strong> changing <strong>of</strong> <strong>the</strong> duration <strong>of</strong> <strong>the</strong> returned ping iscalled ping dilation or compression, depending on whe<strong>the</strong>r <strong>the</strong> ping's duration hasincreased or decreased.23

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