What drives the ice age cycle?

Science

Volumn 313, Issue 5786, 2006, Pages 455-456

  Paillard, Didier ^a  

^a LABORATOIRE DES SCIENCES DU CLIMAT ET DE L ENVIRONNEMENT   (France)

Author keywords

[No Author keywords available]

Indexed keywords

GLACIERS; NATURAL SCIENCES;

ICE AGES;

ICE;

CARBON DIOXIDE; ICE;

PERIODICITY; PLEISTOCENE;

ASTRONOMY; ATMOSPHERIC DEPOSITION; CLIMATE CHANGE; FORCE; GEOLOGICAL TIME; GLACIAL MASS BALANCE; ICE AGE; MELTING POINT; OSCILLATION; PALEOCLIMATE; PARAMETER; PLEISTOCENE; PRIORITY JOURNAL; REVIEW; ROTATION; SEA LEVEL; SUMMER; SUMMER INSOLATION;

EID: 33746592853     PISSN: 00368075     EISSN: 10959203     Source Type: Journal    
DOI: 10.1126/science.1131297     Document Type: Review

References (10)

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8. To build this figure, the model in (5) was extrapolated using a decay e-folding time of 400,000 years for the removal by silicate weathering of a remaining 8% long-lived part of total anthropogenic carbon, following (10).
9. L. E. Lisiecki, M. E. Raymo, Paleoceanography 20, PA1003 (2005).
10. D. Archer, J. Geophys. Res. 110, C09505 (2005).