The snow/ice instability as a mechanism for rapid climate change: A Neoproterozoic Snowball Earth model example
Author:
Affiliation:
1. Dept. of OceanographyTexas A&M University College Station Texas USA
2. Division of Earth and Ocean Sciences, Nicholas School of the Environment and Earth SciencesDuke University Durham North Carolina USA
Publisher
American Geophysical Union (AGU)
Subject
General Earth and Planetary Sciences,Geophysics
Link
https://onlinelibrary.wiley.com/doi/pdf/10.1029/2003GL017333
Reference25 articles.
1. Seasonal snowline instability in a climate model with realistic geography: Application to carboniferous (∼300 MA) glaciation
2. GCM response to Late Precambrian (∼590 Ma) ice-covered continents
3. The effect of solar radiation variations on the climate of the Earth
4. Effect of decreased solar luminosity on late Precambrian ice extent
5. Snowline instability in a general circulation model: application to Carboniferous glaciation
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3. Chapter 10 Modelling the Snowball Earth;Geological Society, London, Memoirs;2011
4. Chapter 6 A review of the Chemical Index of Alteration (CIA) and its application to the study of Neoproterozoic glacial deposits and climate transitions;Geological Society, London, Memoirs;2011
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