The Ocean’s Overturning Circulation
DOI: 10.1063/1.881425
The ocean is a mysterious place. As terrestrial creatures, we are familiar with a small volume of relatively warm ocean water near the surface. The deep ocean is not so familiar. Isolated from the thermal energy of the Sun and the mechanical energy of atmospheric winds, the deep ocean is completely dark and filled with near‐freezing water. Yet the deep ocean is far from stagnant. Radioactive tracer measurements show that the ocean’s circulation brings its interior water into contact with the atmosphere every 600 years or so.
References
1. W. S. Broecker, G. H. Denton, Sci. Am., January 1990, p. 46.
2. S. Manabe, R. J. Stouffer, Nature 364, 215 (1993).https://doi.org/NATUAS
3. S. R. Rintoul, J. Geophys. Res. 96, 2675 (1991).https://doi.org/JGREA2
4. E. C. Carmack, T. D. Foster, Deep‐Sea Res. 22, 711 (1975).https://doi.org/DESRAY
5. H. G. Öslund, C. Grail, TTO North and tropical Atlantic tritium and radiocarbon, data rep. 17, Tritium Lab., Rostenstiel Sch. Of Marine and Atmos. Sci., U. of Miami, Florida (1987).
6. W. S. Broecker, T.‐H. Peng, H. G. Östlund, M. Stuiver, J. Geophys. Res. 90, 6953 (1985).https://doi.org/JGREA2
7. H. Stommel, A. B. Arons, Deep‐Sea Res. 6, 217 (1960).https://doi.org/DESRAY
8. M. C. Gregg, Oceanography 4, 39 (1991).
9. J. R. Ledwell, A. J. Watson, C. S. Law, Nature 364, 701 (1993).https://doi.org/NATUAS
10. C. Döös, D. J. Webb, J. Phys. Oceanogr. 24, 429 (1994).https://doi.org/JPYOBT
11. B. A. Warren, Deep‐Sea Res. 37, 1899 (1991).
12. J. R. Toggweiler, B. Samuels, in The Global Carbon Cycle, M. Heiman, ed., Springer‐Verlag, New York (1993), p. 333.
J. R. Toggweiler, B. Samuels, to be published in Deep‐Sea Res.13. K. Bryan, J. Comput. Phys. 4, 347 (1969).https://doi.org/JCTPAH
More about the Authors
J. Robert Toggweiler. National Oceanic and Atmospheric Administration's Geophysical Fluid Dynamics Laboratory, Princeton, New Jersey.