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Early Eocene low orography and high methane enhance Arctic warming via polar stratospheric clouds - Nature Geoscience

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Early Eocene low orography and high methane enhance Arctic warming via polar stratospheric clouds - Nature Geoscience

Proxy data suggest that the early Eocene (∼56–47.8 million years ago) was characterized by a much weaker equator-to-pole temperature gradient than today. However, general circulation models consistently underestimate high-latitude temperatures indicated by proxy records, suggesting that they may miss important processes.

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Early Eocene low orography and high methane enhance Arctic warming via polar stratospheric clouds - Nature Geoscience

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Early Eocene low orography and high methane enhance Arctic warming via polar stratospheric clouds - Nature Geoscience

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