Note to users. If you're seeing this message, it means that your browser cannot find this page's style/presentation instructions -- or possibly that you are using a browser that does not support current Web standards. Find out more about why this message is appearing, and what you can do to make your experience of our site the best it can be.


Science 29 November 2002:
Vol. 298. no. 5599, pp. 1724 - 1725
DOI: 10.1126/science.1079238

Perspectives

OCEANOGRAPHY:
Oceanic Salt Switch

Ed Boyle

Salinity and temperature, the two determinants of the density of ocean waters, play an important role in ocean circulation. In today's ocean, the saltiest deep waters derive from the northern North Atlantic. But as Boyle explains in his Perspective, the situation was very different during the last glaciation. He highlights the report by Adkins et al., who show that the saltiest waters then formed in the Southern Ocean. The ocean circulation must thus differ substantially between glacial and interglacial periods.


The author is in the Department of Earth, Atmospheric, and Planetary Sciences, Massachusetts Institute of Technology, Cambridge, MA 02139, USA. E-mail: eaboyle{at}mit.edu

Read the Full Text






To Advertise     Find Products


Science. ISSN 0036-8075 (print), 1095-9203 (online)