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 28 August 2009:
Vol. 325. no. 5944, pp. 1085 - 1086
DOI: 10.1126/science.1176186

Perspectives

Atmosphere:

Antarctica's Orbital Beat

Peter Huybers

Alternating glacial and interglacial conditions have dominated Earth's climate for at least the past 800,000 years (1, 2). Such a global rhythm of glaciation is surprising—at least if summer solar radiation controls glaciation (3)—because variations in Earth's orbit cause opposite changes in the intensity of northern and southern summer radiation. Deciphering the origins of the orbital period variations found in Antarctic proxies of climate may tell us why glaciations are global.

Department of Earth and Planetary Sciences, Harvard University, 20 Oxford Street, Cambridge, MA 02138, USA.

E-mail: phuybers{at}fas.harvard.edu

Read the Full Text





To Advertise     Find Products


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