Glacial inception through rapid ice area increase driven by albedo and vegetation feedbacks
<p>We present transient simulations of the last glacial inception using the Earth system model CLIMBER-X with dynamic vegetation, interactive ice sheets, and visco-elastic solid Earth responses. The simulations are initialized at the middle of the Eemian interglacial (125 kiloyears before pres...
| Main Authors: | , , , , , , , |
|---|---|
| Format: | Article |
| Language: | English |
| Published: |
Copernicus Publications
2024-03-01
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| Series: | Climate of the Past |
| Online Access: | https://cp.copernicus.org/articles/20/597/2024/cp-20-597-2024.pdf |