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

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

Internet

https://doi.org/10.1088/1748-9326/ac9c74

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