The minimum oxygen concentration in the western basin of the North Atlantic
Seiwell, Harry Richard
MetadataShow full item record
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.
Suggested CitationBook: Seiwell, Harry Richard, "The minimum oxygen concentration in the western basin of the North Atlantic", Papers in Physical Oceanography and Meteorology, v.5, no.3, 1937-05, DOI:10.1575/1912/1090, https://hdl.handle.net/1912/1090
Showing items related by title, author, creator and subject.
Transient structure in benthic communities : the effects of oxygen stress, burial and high rates of sedimentation Nichols-Driscoll, Jean (Massachusetts Institute of Technology and Woods Hole Oceanographic Institution, 1975-04)The influence of natural short-term fluctuations in environmental parameters on three components of transient benthic invertebrate community structure: abundance of individuals and species, biomass of individuals, ...
Mass, heat, oxygen and nutrient fluxes at 30°S and their implications for the Pacific-Indian through flow and the global heat budget Macdonald, Alison M. (Massachusetts Institute of Technology and Woods Hole Oceanographic Institution, 1991-07)Six hydrographic basinwide sections, two in each of the three major ocean basins, are employed in a set of inverse calculations to determine the extent of exchange between the Pacific and Indian Oceans through the ...
Ganachaud, Alexandre S. (Massachusetts Institute of Technology and Woods Hole Oceanographic Institution, 1999-12)A new, global inversion is used to estimate the large scale oceanic circulation based on the World Ocean Circulation Experiment and Java Australia Dynamic Experiment hydrographic data. A linear inverse "box" model is ...