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Dynamic Contributions to Recent Observed Wintertime Precipitation Trends in Mediterranean‐Type Climate Regions

Abstract:
Many Mediterranean‐type climates (MCs) have experienced wintertime drying trends since 1979. Using a dynamical adjustment method, we separate the effects of circulation‐induced drying trends from other residual trends. Our analysis reveals that circulation trends are the leading cause of the observed drying in Central Chile and the US Southwest, and that models show the drying across Southern Hemisphere MCs is independent of trends in the Southern Annular Mode. All Mediterranean‐type climates have exhibited residual drying trends from both internal variability and externally forced thermodynamic processes. Large ensembles suggest internal variability contributes significantly to the observed drying. However, in many regions the observed drying lies outside the ensemble distribution, raising questions about model accuracy.
Publication status:
Published
Peer review status:
Peer reviewed

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Publisher copy:
10.1029/2024gl114258

Authors


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Institution:
University of Oxford
Role:
Author
ORCID:
0000-0002-7428-4398
More by this author
Institution:
University of Oxford
Role:
Author
ORCID:
0000-0002-5815-9079
More by this author
Role:
Author
ORCID:
0000-0002-2915-1377


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Funder identifier:
https://ror.org/02b5d8509


Publisher:
Wiley
Journal:
Geophysical Research Letters More from this journal
Volume:
52
Issue:
12
Article number:
e2024GL114258
Publication date:
2025-06-19
Acceptance date:
2025-06-08
DOI:
EISSN:
1944-8007
ISSN:
0094-8276


Language:
English
Keywords:
Source identifiers:
3036725
Deposit date:
2025-06-19
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