Articles | Volume 7, issue 2
https://doi.org/10.5194/wcd-7-695-2026
https://doi.org/10.5194/wcd-7-695-2026
Research article
 | 
29 Apr 2026
Research article |  | 29 Apr 2026

Sea-effect snowfall in the Baltic Sea area in 1998–2018 derived from convection-permitting climate model data

Meri Virman, Taru Olsson, Petter Lind, and Kirsti Jylhä

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Interactive discussion

Status: closed

Comment types: AC – author | RC – referee | CC – community | EC – editor | CEC – chief editor | : Report abuse
  • RC1: 'Comment on egusphere-2025-3663', Anonymous Referee #1, 29 Oct 2025
  • RC2: 'Comment on egusphere-2025-3663', Anonymous Referee #2, 19 Dec 2025
  • AC1: 'Comment on egusphere-2025-3663', Meri Virman, 21 Jan 2026
  • EC1: 'Comment on egusphere-2025-3663', Johannes Dahl, 22 Jan 2026

Peer review completion

AR – Author's response | RR – Referee report | ED – Editor decision | EF – Editorial file upload
AR by Meri Virman on behalf of the Authors (18 Feb 2026)  Author's response   Author's tracked changes   Manuscript 
ED: Referee Nomination & Report Request started (27 Feb 2026) by Johannes Dahl
RR by Anonymous Referee #2 (02 Mar 2026)
ED: Publish subject to technical corrections (02 Mar 2026) by Johannes Dahl
AR by Meri Virman on behalf of the Authors (09 Mar 2026)  Author's response   Manuscript 
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Short summary
We use a kilometer-scale regional climate model to investigate the occurrence and intensity of sea-effect snowfall in the Baltic Sea region during 1998–2018. Sea-effect snowbands occur most frequently from November to February and when low-level winds have an easterly component near the eastern coast of Sweden and the southern coast of Finland. Over the southern Baltic Sea, snowbands tend to occur under northerly low-level winds and are most common from December to March.
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