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dc.contributor.authorHopkins, Tom Sawyer
dc.contributor.authorPovero, P.
dc.contributor.authorPiacsek, Steve
dc.date.accessioned2018-10-11T14:06:03Z
dc.date.available2018-10-11T14:06:03Z
dc.date.issued1989/12
dc.identifier1703
dc.identifier.govdocSM-225
dc.identifier.urihttp://hdl.handle.net/20.500.12489/190
dc.description.abstractThe data from the SACLANTCEN June 1986 Cruise is analysed
dc.description.abstractto characterise sound-propagation environment. The cruise was conducted in the Faeroese Channel and the southern Norwegian Sea as the initial cruise of
dc.description.abstractthe Atlantic Inflow Experiment. The sound propagation environment of the
dc.description.abstractupper portion of the water column is described. The mixed layer is defined in terms of the density, Brunt-Vaisala frequency, temperature, and in terms of the sound velocity minimum. The sound-velocity profile and the characteristics of its horizontal distribution are described. The importance of wind and vertical heat flux to the mixed layer is discussed relative to its distribution.
dc.formatvi, 13, [22] p. : ill. ; 36 fig.
dc.languageEnglish
dc.publisherNATO. SACLANTCEN
dc.relation.ispartofseriesADB141996
dc.subjectGIN Sea
dc.subjectGIN Sea'86 trial
dc.subjectCurrents
dc.subjectSea surface
dc.subjectSound velocity in sea water
dc.subjectAcoustic propagation
dc.subjectSeawater thermal properties
dc.subjectOcean thermocline
dc.titleUpper layer environmental parameters from CTD data - GIN '86 cruise
dc.typeScientific Memorandum (SM)


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