Preprints
https://doi.org/10.5194/nhess-2024-210
https://doi.org/10.5194/nhess-2024-210
25 Nov 2024
 | 25 Nov 2024
Status: this preprint is currently under review for the journal NHESS.

Brief Communication: Investigating trends in European hailstorm damage using CMIP6-DAMIP climate models

Stephen Cusack and Tyler Cox

Abstract. Warming seas around Europe have been driving recent upward trends in hailstorm severity. Therefore, learning more about changes to sea temperatures can give insights into hail climate too. Here, we use the DAMIP (Detection and Attribution Model Intercomparison Project) set of climate model experiments to explore how external forcings have modified Mediterranean temperatures. Climate models indicate external forcings caused most of the multidecadal changes in modern times, with anthropogenic aerosols explaining the cool period from about 1900 to the late 1970s, and greenhouse gas increases mainly responsible for the rapid 0.5 K/decade warming of the Mediterranean since then. Current trends in anthropogenic forcing are expected to continue warming seas which suggests European hailstorm risk will keep rising.

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Stephen Cusack and Tyler Cox

Status: open (until 06 Jan 2025)

Comment types: AC – author | RC – referee | CC – community | EC – editor | CEC – chief editor | : Report abuse
  • CC1: 'Comment on nhess-2024-210', Cameron Rye, 12 Dec 2024 reply
Stephen Cusack and Tyler Cox
Stephen Cusack and Tyler Cox

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Short summary
Warming seas have been driving greater hailstorm risk in Europe over the past few decades. Modern climate models indicate anthropogenic aerosols caused the observed cooling of seas from about 1900 to the 1970s, while the recent rapid warming is mostly explained by rising greenhouse gases. Current trends in anthropogenic forcing are likely to persist, suggesting seas will continue warming, and hailstorm risk over Europe will continue rising over the next couple of decades, at least.
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