In:
Science, Washington, DC : American Association for the Advancement of Science, 1880, 306(2004), 5700, Seite 1337, 1095-9203
In:
volume:306
In:
year:2004
In:
number:5700
In:
pages:1337
Description / Table of Contents:
Deep convection is the major mechanism for replenishing oxygen in the deep interior of the world ocean, and its variability affects the use of atmospheric oxygen to monitor the global carbon cycle. Sensors mounted on autonomous floats allow this episodic breathing of the ocean to be monitored in near real time. The results suggest that the tools are available now to make oxygen a key parameter in marine global change research.
Type of Medium:
Online Resource
Pages:
graph. Darst
ISSN:
1095-9203
DOI:
10.1126/science.1102557
Language:
English
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