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dc.contributor.authorShonting, David H.
dc.contributor.authorNacini, Elvio
dc.date.accessioned2018-10-11T14:08:47Z
dc.date.available2018-10-11T14:08:47Z
dc.date.issued1972/09
dc.identifier111
dc.identifier.govdocCP-7
dc.identifier.urihttp://hdl.handle.net/20.500.12489/515
dc.description.abstractObservations of temperature and salinity using a TSD profiling system were made down to 500 m in a deep water area southeast of Pantelleria Island in the Strait of Sicily in May, 1970. The usual two layer system was observed, consisting of upper Atlantic water flowing ESE over a WNW flow of high-salinity eastern Mediterranean "intermediate" water. The variability observed in both the space and time stations occurred mainly in the upper 180 m layer, where the strongest temperature and salinity gradients occur. At a 1.2-hour time-station less variability in ,the ,profiles of- temper.ature was observed than appeared at either of two 45-km long six-station spatial sections made 6 days apart in the same area.
dc.format23 p. : ill. ; digital, PDF file
dc.languageEnglish
dc.publisherNATO. SACLANTCEN
dc.sourceIn: SACLANTCEN Conference Proceedings 7 (1972), pp. 45-67
dc.subjectStrait of Sicily
dc.subjectPhysical oceanography
dc.subjectOceanography - Observations
dc.subjectMILOCMED SURV 70 survey
dc.subjectDeep water
dc.titleA summary of oceanographic data obtained in deep water in the Strait of Sicily in May 1970: MILOCMED surv 70
dc.typePapers and Articles
dc.typeConference Proceedings (CP)


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