Articles | Volume 18, issue 5
Research article
22 Sep 2022
Research article |  | 22 Sep 2022

Import of Atlantic Water and sea ice controls the ocean environment in the northern Barents Sea

Øyvind Lundesgaard, Arild Sundfjord, Sigrid Lind, Frank Nilsen, and Angelika H. H. Renner


Interactive discussion

Status: closed

Comment types: AC – author | RC – referee | CC – community | EC – editor | CEC – chief editor | : Report abuse
  • RC1: 'Comment on os-2022-17', Anonymous Referee #1, 18 May 2022
    • AC2: 'Reply on RC1', Øyvind Lundesgaard, 29 Jul 2022
  • RC2: 'Comment on os-2022-17', Yueng-Djern Lenn, 17 Jun 2022
    • AC3: 'Reply on RC2', Øyvind Lundesgaard, 29 Jul 2022
  • EC1: 'Comment on os-2022-17', Karen J. Heywood, 19 Jun 2022
    • AC1: 'Reply on EC1', Øyvind Lundesgaard, 29 Jul 2022
      • EC2: 'Reply on AC1', Karen J. Heywood, 29 Jul 2022

Peer review completion

AR: Author's response | RR: Referee report | ED: Editor decision
AR by Øyvind Lundesgaard on behalf of the Authors (29 Jul 2022)  Author's response    Author's tracked changes    Manuscript
ED: Publish as is (31 Jul 2022) by Karen J. Heywood
Short summary
In this study, 2-year mooring observations show the evolution of temperature, salinity, and currents in the northern Barents Sea. Inflow of Atlantic Water from the north in autumn and winter was the main driver of the seasonal cycle in the ocean. Winds modulated the inflow on shorter timescales. The upper-ocean state reflected how much sea ice had previously melted in the area. The import of ocean water and sea ice from adjacent regions plays a key role in the complex air–ice–ocean interplay.