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dc.contributor.authorAllan, Thomas D.
dc.date.accessioned2018-10-11T14:07:39Z
dc.date.available2018-10-11T14:07:39Z
dc.date.issued1966/10
dc.identifier2375
dc.identifier.govdocTR-66
dc.identifier.urihttp://hdl.handle.net/20.500.12489/348
dc.description.abstractSound 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.
dc.formati, 30 p. : ill.
dc.languageEnglish
dc.publisherNATO. SACLANTCEN
dc.relation.ispartofseriesAD0802091
dc.subjectStrait of Gibraltar
dc.subjectInternal waves
dc.subjectOcean thermocline
dc.subjectAcoustic measurements
dc.subjectEnvironmental acoustics
dc.subjectAcoustic propagation
dc.subjectSeawater thermal properties
dc.subjectOceanography - Observations
dc.titleObserved sound velocity and temperature profiles in the Strait of Gibraltar during the passage of an internal wave
dc.typeScientific Technical reports (TR)


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