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PHYSICAL OCEANOGRAPHY Part 4: Sound in the Ocean

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Presentation on theme: "PHYSICAL OCEANOGRAPHY Part 4: Sound in the Ocean"— Presentation transcript:

1 PHYSICAL OCEANOGRAPHY Part 4: Sound in the Ocean
GEOL 1033 (Lesson 29)

2 Depth determination (study Exercise #4) Echo sounder used
SOUND IN SEAWATER Sound travels About 4 times faster in water than in air Approximately m/s in water Depth determination (study Exercise #4) Half travel time X 1500 m/s = depth Echo sounder used Record depth profiles Detects deep scattering layers Obtain seismic profiles

3

4 Speed of Sound in Water “Typical” depth profile of sound speed in seawater

5 Speed of Sound in Water Arctic & Antarctic profile Lower latitude profile

6 SOFAR & Shadow Zone Effects of sound speed minimum and maximum:

7 SOFAR Channel Sound velocity minimum at about 1000 m depth at low to mid latitudes

8 SOFAR Experiment in 1991 Successful transmission of sound over great distance

9 Associated with a near-surface sound maximum speed depth
Sound Shadow Zone Associated with a near-surface sound maximum speed depth At approximately 80 to 100 m Ideal detection

10 Sound "Shadow Zone" Due to Refraction

11 END OF FILE


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