Reversal of projected European summer precipitation decline in a stabilizing climate

[thumbnail of Open Access]
Preview
Text (Open Access) - Published Version
· Available under License Creative Commons Attribution.
· Please see our End User Agreement before downloading.
| Preview
Available under license: Creative Commons Attribution
[thumbnail of 980197_0_merged_1708620226.pdf]
Text - Accepted Version
· Restricted to Repository staff only
Restricted to Repository staff only

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

Dittus, A. J. orcid id iconORCID: https://orcid.org/0000-0001-9598-6869, Collins, M., Sutton, R. orcid id iconORCID: https://orcid.org/0000-0001-8345-8583 and Hawkins, E. orcid id iconORCID: https://orcid.org/0000-0001-9477-3677 (2024) Reversal of projected European summer precipitation decline in a stabilizing climate. Geophysical Research Letters, 51 (6). e2023GL107448. ISSN 1944-8007 doi: 10.1029/2023GL107448

Abstract/Summary

Precipitation projections in transient climate change scenarios have been extensively studied over multiple climate model generations. Although these simulations have also been used to make projections at specific Global Warming Levels (GWLs), dedicated simulations are more appropriate to study changes in a stabilising climate. Here, we analyse precipitation projections in six multi-century experiments with fixed atmospheric concentrations of greenhouse gases, conducted with the UK Earth System Model (UKESM) and which span a range of GWLs between 1.5 and 5°C of warming. Regions are identified where the sign of precipitation trends in high-emission transient projections is reversed in the stabilisation experiments. For example, stabilisation reverses a summertime precipitation decline across Europe. This precipitation recovery occurs concurrently with changes in the pattern of Atlantic sea surface temperature trends due to a slow recovery of the Atlantic Meridional Overturning Circulation in the stabilisation experiments, along with changes in humidity and atmospheric circulation.

Altmetric Badge

Item Type Article
URI https://reading-clone.eprints-hosting.org/id/eprint/115553
Identification Number/DOI 10.1029/2023GL107448
Refereed Yes
Divisions Science > School of Mathematical, Physical and Computational Sciences > NCAS
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

Search Google Scholar