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Oceans of noise - Whale and Dolphin Conservation Society

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Box 2. The effects <strong>of</strong> temperature, salinity <strong>and</strong> pressure on sound speed<br />

Figure 2.5. A typical sound velocity pr<strong>of</strong>ile showing the “Layer” depth (depth <strong>of</strong> maximum sound<br />

velocity or Vmax), the sound velocity minimum (Vmin), the signatures <strong>of</strong> seasonal <strong>and</strong> permanent<br />

thermoclines, <strong>and</strong> the signature <strong>of</strong> the deep water isothermal layer.<br />

Depth (m)<br />

-500<br />

-1000<br />

-1500<br />

-2000<br />

-2500<br />

-3000<br />

0<br />

1445 1465 1485<br />

C (ms -1 )<br />

Layer depth (Vmax)<br />

Sound velocity<br />

minimum (Vmin)<br />

16<br />

Seasonal thermocline<br />

Permanent thermocline<br />

Deep-water isothermal layer

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