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.