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Climatology and convective mode of severe hail in the United Kingdom

Lookup NU author(s): Dr Abdullah KahramanORCiD

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This is the final published version of an article that has been published in its final definitive form by Elsevier, 2024.

For re-use rights please refer to the publisher's terms and conditions.


Abstract

Severe or large hail, with diameter ≥ 20 mm, is a hazard associated with severe convective storms (SCS) that can cause significant damage. In the UK, the rarity and small footprint of severe hail events makes obtaining well-documented hail reports difficult, and the reports are spread across multiple databases. In this study, three databases of UK severe hail reports are merged for the first time. The combined dataset set (1979–2022), comprising >800 reports, is used to investigate interannual variability and the seasonal, spatial and size distributions of severe hail. The seasonal cycle peaks in early–mid summer, and the peak month has shifted from June to July since around 2005. The distribution of reported hail size is exponential, with a slower decay (larger hail) during summer. The time of day, basic convective mode (isolated, clustered or linear), and presence or absence of supercellular characteristics are assessed for 274 of the reports since 2006, using composite radar rainrate data. The diurnal cycle is strong year-round, peaking during the late afternoon (1500–1800 UTC). 53% of severe hail events are associated with isolated cells, 33% with clusters, and 14% with linear storms. Around 35% of severe hail-producing storms are probable supercells, increasing to 70% for storms producing ≥40 mm hail. This demonstrates that the prevalence of supercells producing very large hail extends to temperate maritime climates. These results may be of relevance in other regions with a relatively low incidence of severe hail in the present climate. This comprehensive analysis of severe and potentially impactful hail in the UK provides novel insight into its characteristics, enabling improved assessment of climate risk from this hazard.


Publication metadata

Author(s): Wells HM, Hillier J, Garry FK, Dunstone N, Clark MR, Kahraman A, Chen H

Publication type: Article

Publication status: Published

Journal: Atmospheric Research

Year: 2024

Volume: 309

Print publication date: 15/10/2024

Online publication date: 04/07/2024

Acceptance date: 03/07/2024

Date deposited: 24/09/2024

ISSN (print): 0169-8095

ISSN (electronic): 1873-2895

Publisher: Elsevier

URL: https://doi.org/10.1016/j.atmosres.2024.107569

DOI: 10.1016/j.atmosres.2024.107569

Data Access Statement: he TORRO severe hail database is available for research purposes on request from TORRO. ESWD reports can be viewed at https://eswd.eu and the full database is available on request (charges may apply). The British Flash Flood Chronology is available at https://www.jbatrust.org/about-the-jba-trust/how-we-help/publications-resources/riversand-coasts/british-chronology-of-flash-floods/. Met Office NIMROD 1 km composite radar data is available to licensed users on the Centre for Environmental Data Analysis (CEDA) archive at https://catalogue.ceda.ac.uk/uuid/27dd6ffba67f667a18c62de5c3456350.


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Funding

Funder referenceFunder name
UK Research and Innovation (UKRI) Natural Environment Research Council (NERC) DTP2 CENTA2 Grant (NE/S007350/1)
Strategic Priority Fund for UK Climate Resilience
UKRI KE Fellowship NE/V018698/ 1.
UKRI NERC funded project FUTURE-STORMS (NE/ R01079X/1)

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