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Blue whale calling in the Rottnest trench-2000, Western ... - ANP

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Figure 32: Predicted ranges for <strong>the</strong> 95% probability of detection of <strong>the</strong> blue <strong>whale</strong> type II component for <strong>the</strong> drift<strong>in</strong>g<br />

site, a 200 m Leeuw<strong>in</strong> current and 20 m source depth. Numbers represent tracks at 45 o <strong>in</strong>crements clockwise from<br />

north equals one.<br />

3.6) O<strong>the</strong>r signals recorded<br />

A number of o<strong>the</strong>r signals, of physical, biological and man-made orig<strong>in</strong> were also recorded.<br />

Details of <strong>the</strong>se signals are briefly presented below, with no fur<strong>the</strong>r discussion.<br />

3.6.1) 20 Hz 'click<strong>in</strong>g'<br />

A second call type commonly observed was 20 Hz 'clicks'. An example of several click<br />

waveforms is shown <strong>in</strong> Figure 33.<br />

Figure 33: Example waveforms of 20 Hz clicks recorded.<br />

These were common, occurred <strong>in</strong> bouts of isolated samples to days of click<strong>in</strong>g and were often<br />

recorded at very high levels (up to 153 dB re 1μPa peak-peak). They display several multipath<br />

reflections, from which it should be possible to estimate range and depth us<strong>in</strong>g an extension of<br />

<strong>the</strong> method described <strong>in</strong> Cato (1998). For example <strong>the</strong> middle call of Figure 6 was estimated to<br />

be at a depth of 286 m, and 1987 m from <strong>the</strong> hydrophone us<strong>in</strong>g a surface reflected time relative<br />

to <strong>the</strong> direct arrival of 82 ms and a bottom-surface reflected time of 169 ms relative to <strong>the</strong> direct<br />

arrival time and ignor<strong>in</strong>g refraction effects. Dur<strong>in</strong>g click<strong>in</strong>g bouts and with<strong>in</strong> a 90 s block,<br />

32

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