Show simple item record

dc.contributor.authorSeiwell, Harry Richard
dc.date.accessioned2006-07-11T16:24:05Z
dc.date.available2006-07-11T16:24:05Z
dc.date.issued1937-05
dc.identifier.urihttp://hdl.handle.net/1912/1090
dc.description.abstractWith 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.extent1191233 bytes
dc.format.mimetypeapplication/pdf
dc.language.isoen_USen
dc.publisherMassachusetts Institute of Technology and Woods Hole Oceanographic Institutionen
dc.relation.ispartofseriesPapers in Physical Oceanography and Meteorologyen
dc.relation.ispartofseriesv.5, no.3en
dc.subjectWateren
dc.subjectDissolved oxygenen
dc.subjectOceanographyen
dc.titleThe minimum oxygen concentration in the western basin of the North Atlanticen
dc.typeBooken
dc.identifier.doi10.1575/1912/1090


Files in this item

Thumbnail

This item appears in the following Collection(s)

Show simple item record