Snowball Earth transitions from Last Glacial Maximum conditions provide an independent upper limit on Earth's climate sensitivity
<p>Geological evidence of a snowball Earth state indicate persistent tropical sea ice cover during the Neoproterozoic (<span class="inline-formula">>635</span> million years ago). Current theory is that a strengthening of the positive surface albedo feedback with cooling temperatures, eventually...
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| Hauptverfasser: | , , , |
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| Format: | Artigo |
| Sprache: | Inglês |
| Veröffentlicht: |
Copernicus Publications
2026-03-01
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| Schriftenreihe: | Earth System Dynamics |
| Online-Zugang: | https://esd.copernicus.org/articles/17/303/2026/esd-17-303-2026.pdf |
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