Refinement of Eocene lapse rates, fossil-leaf altimetry, and North American Cordilleran surface elevation estimates
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文摘

We simulate Eocene climate of western North America with a global climate model.

Eocene temperature and moist enthalpy lapse rates differ from present-day.

Eocene temperature and moist enthalpy vary non-linearly with increasing elevation.

Proxies agree with simulations when Cordilleran elevation is prescribed to be 2–3 km.

Model suggests foreland elevations are significantly lower than the Cordillera hinterland.

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