Neoproterozoic “snowball Earth”: Dynamic sea ice over a quiescent ocean
- 5 December 2003
- journal article
- Published by American Geophysical Union (AGU) in Paleoceanography and Paleoclimatology
- Vol. 18 (4)
- https://doi.org/10.1029/2003pa000926
Abstract
No abstract availableKeywords
This publication has 32 references indexed in Scilit:
- Ventilation of the North Atlantic Ocean during the Last Glacial Maximum: A comparison between simulated and observed radiocarbon agesPaleoceanography and Paleoclimatology, 2003
- The snowball Earth hypothesis: testing the limits of global changeTerra Nova, 2002
- Impact of geothermal heating on the global ocean circulationGeophysical Research Letters, 2001
- GCM response to Late Precambrian (∼590 Ma) ice—covered continentsGeophysical Research Letters, 2001
- Stratigraphic, geochronological, and paleomagnetic constraints upon the Neoproterozoic climatic paradoxAmerican Journal of Science, 2000
- Geological constraints on the Precambrian history of Earth's rotation and the Moon's orbitReviews of Geophysics, 2000
- The Neoproterozoic climatic paradox: Equatorial palaeolatitude for Marinoan glaciation near sea level in South AustraliaPublished by Elsevier ,1999
- Considering a Neoproterozoic Snowball EarthScience, 1999
- GCM sensitivity test using increased rotation rate, reduced solar forcing and orography to examine low latitude glaciation in the neoproterozoicGeophysical Research Letters, 1998
- Two or four Neoproterozoic glaciations?Geology, 1998