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The minimum oxygen concentration in the western basin of the North Atlantic

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dc.contributor.author Seiwell, Harry Richard
dc.date.accessioned 2006-07-11T16:24:05Z
dc.date.available 2006-07-11T16:24:05Z
dc.date.issued 1937-05
dc.identifier.uri http://hdl.handle.net/1912/1090
dc.description.abstract With the advance in knowledge of oceanic circulation there now exists a demand for additional identifying properties which will serve to trace the origin and movements of water masses in the sea, and to check earlier conclusions based entirely on temperature and salinity distribution. Of all the known identifying properties (except temperature and salinity) oxygen appears to be the most useful, not only because of the ease with which it can be accurately measured at sea, but also because of the large amount of data available on its distribution in the open ocean. en
dc.format.extent 1191233 bytes
dc.format.mimetype application/pdf
dc.language.iso en_US en
dc.publisher Massachusetts Institute of Technology and Woods Hole Oceanographic Institution en
dc.relation.ispartofseries Papers in Physical Oceanography and Meteorology en
dc.relation.ispartofseries v.5, no.3 en
dc.subject Water en
dc.subject Dissolved oxygen en
dc.subject Oceanography en
dc.title The minimum oxygen concentration in the western basin of the North Atlantic en
dc.type Book en
dc.identifier.doi 10.1575/1912/1090


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