CO2 levels required for deglaciation of a "near-snowball" Earth

Geologic evidence suggests that in the Late Neoproterozoic (∼600 Ma) almost all land masses were glaciated, with sea‐level glaciation existing even at the equator. A recent modeling study has shown that it is possible to simulate an ice‐covered Earth glaciation with a coupled climate/ice‐sheet model...

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Veröffentlicht in:	Geophysical research letters 2001-01, Vol.28 (2), p.283-286
Hauptverfasser:	Crowley, Thomas J., Hyde, William T., Peltier, W. Richard
Format:	Artikel
Sprache:	eng
Schlagworte:	Earth sciences Earth, ocean, space Exact sciences and technology Stratigraphy
Online-Zugang:	Volltext
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