Elevation-dependent temperature response in early Eocene using paleoclimate model experiment

Mountains become warmer with elevation in response to greenhouse gas warming, an effect known as elevation-dependent warming. The Eocene is considered a replica of the future climate in an epoch with high atmospheric carbon dioxide concentration (CO _2 ). Therefore, the topographic features of the E...

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Bibliographic Details

Published in:	Environmental Research Letters
Main Authors:	Pratik Kad, Manuel Tobias Blau, Kyung-Ja Ha, Jiang Zhu
Format:	Article
Language:	English
Published:	IOP Publishing 2022-01-01
Subjects:	mountains Eocene paleoclimate modeling elevation-dependent warming future paradox CO2
Online Access:	https://doi.org/10.1088/1748-9326/ac9c74