Articles | Volume 19, issue 8
https://doi.org/10.5194/tc-19-3065-2025
https://doi.org/10.5194/tc-19-3065-2025
Research article
 | 
15 Aug 2025
Research article |  | 15 Aug 2025

Estimation of duration and its changes in Lagrangian observations relying on ice floes in the Arctic Ocean utilizing a sea ice motion product

Fanyi Zhang, Ruibo Lei, Meng Qu, Na Li, Ying Chen, and Xiaoping Pang

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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-2024-2723', Anonymous Referee #1, 11 Dec 2024
  • RC2: 'Comment on egusphere-2024-2723', Anonymous Referee #1, 13 Dec 2024
  • RC3: 'Comment on egusphere-2024-2723', Anonymous Referee #2, 12 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) (07 Mar 2025) by Xichen Li
AR by Ruibo Lei on behalf of the Authors (01 Apr 2025)  Author's response   Author's tracked changes   Manuscript 
ED: Referee Nomination & Report Request started (02 Apr 2025) by Xichen Li
RR by Anonymous Referee #1 (14 Apr 2025)
RR by Anonymous Referee #2 (21 Apr 2025)
ED: Publish subject to minor revisions (review by editor) (01 May 2025) by Xichen Li
AR by Ruibo Lei on behalf of the Authors (11 May 2025)  Author's response   Author's tracked changes   Manuscript 
ED: Publish as is (30 May 2025) by Xichen Li
AR by Ruibo Lei on behalf of the Authors (02 Jun 2025)  Author's response   Manuscript 
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Short summary
We reconstructed sea ice drift trajectories and identified optimal deployment areas for Lagrangian observations in the central Arctic Ocean. The trajectories revealed a preference for ice advection towards the Transpolar Drift region over the Beaufort Gyre, with endpoints influenced by large-scale atmospheric circulation patterns. This study provides critical support for the planning and implementation of Lagrangian observations relying on ice floes in the central Arctic Ocean under changing environmental conditions.
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