Constraints on climate change stabilization based on observations of Earth's energy imbalance

[thumbnail of Open Access]
Preview
Text (Open Access)
- Published Version
· Available under License Creative Commons Attribution Non-commercial.
[thumbnail of draft1_ref.pdf]
Text
- Accepted Version
· Restricted to Repository staff only
· The Copyright of this document has not been checked yet. This may affect its availability.

Please see our End User Agreement.

It is advisable to refer to the publisher's version if you intend to cite from this work. See Guidance on citing.

Add to AnyAdd to TwitterAdd to FacebookAdd to LinkedinAdd to PinterestAdd to Email

Douville, H. ORCID: https://orcid.org/0000-0002-6074-6467 and Allan, R. P. ORCID: https://orcid.org/0000-0003-0264-9447 (2026) Constraints on climate change stabilization based on observations of Earth's energy imbalance. Geophysical Research Letters, 53 (10). ISSN 0094-8276 doi: 10.1029/2025GL121056

Abstract/Summary

The Earth's energy imbalance (EEI) at the top of the atmosphere is a key indicator of climate change that determines the Earth's heating rate. Here, we use a global reconstruction of surface temperature and EEI measurements to constrain global projections of the Earth heating rate until the end of the century. Our robust statistical method is shown to withstand changes in the prior distribution or the length of the EEI record, and to perform well when evaluated against independent pseudo-observations. Results show that the reversal of the Earth heating rate is very unlikely to occur before the early 2040s, even under a low emission scenario. This is more than 10 years later than expected from the raw projections, with significant implications for both mitigation and adaptation policies. Future research is however needed to better attribute the observed EEI changes and to explore the patterns of recent versus future EEI changes. Plain Language Summary The Earth is currently gaining more energy from the Sun than it is losing back to space. This imbalance-called the Earth's Energy Imbalance (EEI) In this study, we combine global surface temperature data with measurements of this heat imbalance at the top of the atmosphere to estimate how fast the planet will keep warming through the rest of the century. For this purpose, we use a robust statistical method and test it in different ways to make sure the results are reliable. Our findings suggest that the Earth will keep gaining heat for at least the next couple of decades. Even in a scenario where greenhouse gas emissions are kept low, it's very unlikely that this warming trend will start to reverse before the early 2040s. This is more than 10 years later than earlier estimates suggested, which matters for planning how to reduce emissions and adapt to climate impacts. The study also notes that more research is needed to better understand why the Earth's heat imbalance is increasing faster than expected.ed

Altmetric Badge

Dimensions Badge

Item Type Article
URI https://centaur.reading.ac.uk/id/eprint/129999
Identification Number/DOI 10.1029/2025GL121056
Refereed Yes
Divisions Science > School of Mathematical, Physical and Computational Sciences > National Centre for Earth Observation (NCEO)
Science > School of Mathematical, Physical and Computational Sciences > Department of Meteorology
Publisher American Geophysical Union
Download/View statistics View download statistics for this item

Downloads

Downloads per month over past year

University Staff: Request a correction | Centaur Editors: Update this record