Articles | Volume 6-osr9
https://doi.org/10.5194/sp-6-osr9-6-2025
https://doi.org/10.5194/sp-6-osr9-6-2025
30 Sep 2025
 | OSR9 | Chapter 2.3
 | 30 Sep 2025 | OSR9 | Chapter 2.3

A new conceptual framework for assessing the physical state of the Baltic Sea

Urmas Raudsepp, Ilja Maljutenko, Priidik Lagemaa, and Karina von Schuckmann

Download

Interactive discussion

Status: closed

Comment types: AC – author | RC – referee | CC – community | EC – editor | CEC – chief editor | : Report abuse
  • RC1: 'Comment on sp-2024-19', Anonymous Referee #1, 09 Oct 2024
    • AC1: 'Reply on RC1', Ilja Maljutenko, 21 Jan 2025
  • RC2: 'Comment on sp-2024-19', Anonymous Referee #2, 09 Dec 2024
    • AC2: 'Reply on RC2', Ilja Maljutenko, 21 Jan 2025

Peer review completion

AR: Author's response | RR: Referee report | ED: Editor decision | EF: Editorial file upload
ED: Publish subject to revisions (further review by editor and referees) (22 Jan 2025) by Johannes Karstensen
AR by Ilja Maljutenko on behalf of the Authors (02 Apr 2025)  Author's response   Author's tracked changes   Manuscript 
ED: Referee Nomination & Report Request started (01 Jun 2025) by Johannes Karstensen
RR by Anonymous Referee #2 (10 Jun 2025)
RR by Anonymous Referee #1 (16 Jun 2025)
ED: Publish subject to revisions (further review by editor and referees) (20 Jun 2025) by Johannes Karstensen
AR by Ilja Maljutenko on behalf of the Authors (31 Jul 2025)  Author's response   Author's tracked changes   Manuscript 
ED: Publish subject to technical corrections (04 Aug 2025) by Johannes Karstensen
ED: Publish as is (07 Aug 2025) by Marilaure Grégoire (Chief editor)
AR by Ilja Maljutenko on behalf of the Authors (12 Aug 2025)
Download
Short summary
Over the past 3 decades, the Baltic Sea has warmed and become saltier, reflecting broader atmospheric trends. Heat content changes are mainly driven by subsurface temperature variations in the upper 100 m, influenced by air temperature, evaporation, and wind stress. Freshwater content changes are largely controlled by salinity shifts in the halocline (40–120 m), with key drivers being saline inflows, precipitation, and zonal wind stress.
Share
Altmetrics
Final-revised paper
Preprint