Climate and ocean circulation in the aftermath of a Marinoan snowball Earth
When a snowball Earth deglaciates through a very high atmospheric CO2 concentration, the resulting inflow of freshwater leads to a stably stratified ocean, and the strong greenhouse conditions drive the climate into a very warm state. Here, we use a coupled atmosphere-ocean general circulation model...
| Main Authors: | , |
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| Format: | Article |
| Language: | English |
| Published: |
Copernicus GmbH
2022
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| Subjects: | |
| Online Access: | View Fulltext in Publisher |