Articles | Volume 20, issue 3
https://doi.org/10.5194/os-20-711-2024
https://doi.org/10.5194/os-20-711-2024
Research article
 | 
11 Jun 2024
Research article |  | 11 Jun 2024

Exploring the tidal response to bathymetry evolution and present-day sea level rise in a channel–shoal environment

Robert Lepper, Leon Jänicke, Ingo Hache, Christian Jordan, and Frank Kösters

Download

Interactive discussion

Status: closed

Comment types: AC – author | RC – referee | CC – community | EC – editor | CEC – chief editor | : Report abuse
  • RC1: 'Comment on egusphere-2024-283', Anonymous Referee #1, 03 Mar 2024
    • AC1: 'Reply on RC1', Robert Lepper, 19 Apr 2024
  • RC2: 'Comment on egusphere-2024-283', Anonymous Referee #2, 06 Apr 2024
    • AC2: 'Reply on RC2', Robert Lepper, 19 Apr 2024

Peer review completion

AR: Author's response | RR: Referee report | ED: Editor decision | EF: Editorial file upload
AR by Robert Lepper on behalf of the Authors (19 Apr 2024)  Author's response   Author's tracked changes   Manuscript 
ED: Publish subject to technical corrections (24 Apr 2024) by John M. Huthnance
AR by Robert Lepper on behalf of the Authors (25 Apr 2024)  Manuscript 
Download
Short summary
Most coastal environments are sheltered by tidal flats and salt marshes. These habitats are threatened from drowning under sea level rise. Contrary to expectation, recent analyses in the Wadden Sea showed that tidal flats can accrete faster than sea level rise. We found that this phenomenon was facilitated by the nonlinear link between tidal characteristics and coastal bathymetry evolution. This link caused local and regional tidal adaptation with sharp increase–decrease edges at the coast.