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Observed sound velocity and temperature profiles in the Strait of Gibraltar during the passage of an internal wave

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Abstract
Sound velocity and temperature measurements taken from the sea-surface to 350 m depth, close to one spot over a 24-hour period revealed the passage of an internal wave of approximately 60 m amplitude. The effect of this wave in breaking up a previously well-developed thermocline is demonstrated. The results of computer calculations on the effect of such a wave on the ray paths from a hypothetical sound source are presented.

URI
http://hdl.handle.net/20.500.12489/348

Report Number
TR-66

Collections
  • Technical Reports

Date
1966/10

Author(s)
Allan, Thomas D.

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TR-66.pdf (20.26Mb)

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