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Multi-model ensemble of frost risks across East Asia (1850–2100)

Abstract:
Abstract Frost events can cause the deterioration of a wide range of heritage materials, including stone, brick and earth. In a warming world, the frequency and location of frost events is likely to change, affecting the conservation strategies required at heritage sites. We use a multi-model ensemble approach to investigate three types of frost events in East Asia: freeze–thaw cycles; deep frost days and wet frosts. The study uses nine CMIP6 models for the period 1850 to 2100, with future projections run under the SPS585 scenario. Additional analysis is undertaken for five specific 2° ✕ 2° areas located across East Asia. The three frost event parameters are spatially and temporally distinct. A decrease in all three frost parameters is found in Japan, South Korea and East China, with some areas projected to have no frost events by the end of the twenty-first century. However, Northwest China is distinctive as wet frosts are projected to increase over the twenty-first century, while on the Tibetan plateau of Southwest China, freeze–thaw cycles are projected to increase. This suggests that except in some localised regions, heritage managers can focus on risks other than frost weathering in developing plans to address climate change. Graphical Abstract.
Publication status:
Published
Peer review status:
Peer reviewed

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Publisher copy:
10.1007/s10584-024-03723-4

Authors

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Institution:
University of Oxford
Oxford college:
St John's College
Role:
Author
ORCID:
0000-0003-4061-240X
More by this author
Role:
Author
ORCID:
0000-0002-2233-8761


Publisher:
Springer
Journal:
Climatic Change More from this journal
Volume:
177
Issue:
4
Pages:
68
Article number:
68
Publication date:
2024-04-08
DOI:
EISSN:
1573-1480
ISSN:
0165-0009


Language:
English
Keywords:
Pubs id:
1989590
Local pid:
pubs:1989590
Source identifiers:
W4394579034
Deposit date:
2026-06-10
ARK identifier:
This ORA record was generated from metadata provided by an external service. It has not been edited by the ORA Team.

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