Sea-ice thermodynamics can determine waterbelt scenarios for Snowball Earth
<p>Snowball Earth refers to multiple periods in the Neoproterozoic during which geological evidence indicates that the Earth was largely covered in ice. A Snowball Earth results from a runaway ice–albedo feedback, but there is an ongoing debate about how the feedback stopped: with fully ice-co...
| Hlavní autoři: | , |
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| Médium: | Článek |
| Jazyk: | English |
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Copernicus Publications
2024-03-01
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| Edice: | Earth System Dynamics |
| On-line přístup: | https://esd.copernicus.org/articles/15/215/2024/esd-15-215-2024.pdf |