Articles | Volume 16, issue 1
Development and technical paper
04 Jan 2023
Development and technical paper |  | 04 Jan 2023

How does 4DVar data assimilation affect the vertical representation of mesoscale eddies? A case study with observing system simulation experiments (OSSEs) using ROMS v3.9

David E. Gwyther, Shane R. Keating, Colette Kerry, and Moninya Roughan


Interactive discussion

Status: closed

Comment types: AC – author | RC – referee | CC – community | EC – editor | CEC – chief editor | : Report abuse
  • RC1: 'Comment on gmd-2022-204', Anonymous Referee #1, 22 Oct 2022
    • RC2: 'Reply on RC1', Anonymous Referee #2, 02 Nov 2022
      • AC2: 'Reply on RC2', David Gwyther, 14 Nov 2022
    • AC1: 'Reply on RC1', David Gwyther, 14 Nov 2022

Peer review completion

AR: Author's response | RR: Referee report | ED: Editor decision
AR by David Gwyther on behalf of the Authors (14 Nov 2022)  Author's response    Author's tracked changes    Manuscript
ED: Referee Nomination & Report Request started (14 Nov 2022) by Riccardo Farneti
RR by Anonymous Referee #1 (14 Nov 2022)
RR by Anonymous Referee #2 (23 Nov 2022)
ED: Publish as is (23 Nov 2022) by Riccardo Farneti
Short summary
Ocean eddies are important for weather, climate, biology, navigation, and search and rescue. Since eddies change rapidly, models that incorporate or assimilate observations are required to produce accurate eddy timings and locations, yet the model accuracy is rarely assessed below the surface. We use a unique type of ocean model experiment to assess three-dimensional eddy structure in the East Australian Current and explore two pathways in which this subsurface structure is being degraded.