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dc.contributor.authorMidttun, Lars
dc.date.accessioned2011-04-19T10:29:49Z
dc.date.available2011-04-19T10:29:49Z
dc.date.issued1964
dc.identifier.issn0071-5638
dc.identifier.urihttp://hdl.handle.net/11250/113757
dc.description.abstractAn echo sounder is adjusted for constant sound velocity, usually 1500 m/sec. Since the velocity of sound in the sea is varying with temperature, salinity and depth, a correction is necessary if accurate soundings are required. The present paper shows a practical method for the computation of this correction. 49 of the "G. Sars" stations, taken in the years 1951-55, are fairly well covering the Norwegian Sea (Fig. 3). These stations have been used as basic material for the computation of the depth correction presented in Figs. 4-10. The correction is given as percentage of measured echo depth for the following depths (meters): 500, 1000, 1500, 2000, 2500, 3000, and 3500.en_US
dc.language.isonoben_US
dc.publisherHavforskningsinstitutteten_US
dc.relation.ispartofseriesFisken og havet;1964 - Nr. 3
dc.subjectecho sounderen_US
dc.subjectekkolodden_US
dc.titleEn korreksjon til ekkoloddets dybdeangivelseen_US
dc.typeResearch reporten_US
dc.subject.nsiVDP::Agriculture and fishery disciplines: 900::Fisheries science: 920::Fisheries technology: 924en_US
dc.source.pagenumber11 s.en_US


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