Currently
ocean oxygen measurements are relatively sparse.
Not exact matches
For 30 million years, beginning 530 million years ago, the
oxygen levels of the
ocean dropped steadily, four different sets of chemical
measurements suggested.
However,
measurements show that this is not the case even in the large and essentially anoxic
oxygen minimum zones of the tropical
oceans.
The work has implications for how
ocean modelers determine the overall amounts of carbon dioxide taken up by the
oceans, which is typically performed through
oxygen - based
measurements.
Britton Stephens, an NCAR scientist and the project's co-principal investigator, said HIPPO flights have collected the first large - scale
measurements of carbon dioxide and
oxygen cycling into and out of surface waters of the Southern
Ocean.
Based on
oxygen (and d13C)
measurements, we have a rough indication which one takes the most: about 1 / 3rd of the total sink is going into the biosphere, 2 / 3rd into the
oceans.
More exact for the partitioning between
oceans and vegetation are found in the
oxygen balance, but with large margins of error, as
oxygen change
measurements (a few ppmv in 200,000 ppmv) are extremely difficult, at the edge of the accuracy of the methods used.
Facilitated by the invention of an elegant and precise wet - chemical method by Winkler (1888), which has remained essentially unchanged until today, reliable and comparable
oxygen measurements have been made during innumerable research cruises to all parts of world
ocean such that a detailed picture of the distribution of
oxygen has emerged long since.
«From our
measurements, we estimated that the
oxygen consumption within the eddies is some five times larger than in normal
ocean conditions,» Karstensen explained.