Loading…
Fast‐Forward to Perturbed Equilibrium Climate
The equilibrium climate sensitivity, that is, the global‐mean surface‐air temperature change in response to a doubling of the carbon dioxide concentration is a widely used metric in climate change studies. Its exact value is rarely known because its estimation requires a long integration time of sev...
Saved in:
Published in: | Geophysical research letters 2019-08, Vol.46 (15), p.8969-8975 |
---|---|
Main Authors: | , , , , , , , , |
Format: | Article |
Language: | English |
Subjects: | |
Citations: | Items that this one cites Items that cite this one |
Online Access: | Get full text |
Tags: |
Add Tag
No Tags, Be the first to tag this record!
|
Summary: | The equilibrium climate sensitivity, that is, the global‐mean surface‐air temperature change in response to a doubling of the carbon dioxide concentration is a widely used metric in climate change studies. Its exact value is rarely known because its estimation requires a long integration time of several thousand years. We propose a method to estimate an accurate value of the equilibrium response from fully coupled climate models at a reasonable computational cost. Using this method, our state‐of‐the‐art climate model CNRM‐CM6‐1 reaches a stationary state after only few hundred of years of integration. This “Fast‐Forward” method consists of an optimal two‐step forcing pathway designed using the framework of a two‐layer energy balance model. It can be applied easily to any coupled climate model.
Key Points
A simple method for estimating the equilibrium climate sensitivity is proposed
The method allows to simulate the stationary climate corresponding to any given radiative perturbation with a limited computational cost
The method can be applied to any atmosphere‐ocean coupled climate model |
---|---|
ISSN: | 0094-8276 1944-8007 |
DOI: | 10.1029/2019GL083031 |