Articles | Volume 21, issue 1
https://doi.org/10.5194/os-21-473-2025
https://doi.org/10.5194/os-21-473-2025
Research article
 | 
13 Feb 2025
Research article |  | 13 Feb 2025

Application of wave–current coupled sediment transport models with variable grain properties for coastal morphodynamics: a case study of the Changhua River, Hainan

Yuxi Wu, Enjin Zhao, Xiwen Li, and Shiyou Zhang

Download

Interactive discussion

Status: closed

Comment types: AC – author | RC – referee | CC – community | EC – editor | CEC – chief editor | : Report abuse
  • RC1: 'Comment on egusphere-2024-2154', Anonymous Referee #1, 02 Sep 2024
  • RC2: 'Comment on egusphere-2024-2154', Anonymous Referee #2, 20 Oct 2024

Peer review completion

AR: Author's response | RR: Referee report | ED: Editor decision | EF: Editorial file upload
AR by Yuxi Wu on behalf of the Authors (20 Oct 2024)  Author's response   Author's tracked changes   Manuscript 
ED: Reconsider after major revisions (25 Oct 2024) by John M. Huthnance
AR by Yuxi Wu on behalf of the Authors (07 Nov 2024)  Author's response   Author's tracked changes   Manuscript 
ED: Referee Nomination & Report Request started (12 Nov 2024) by John M. Huthnance
RR by Anonymous Referee #2 (20 Nov 2024)
RR by Anonymous Referee #1 (24 Nov 2024)
ED: Publish subject to minor revisions (review by editor) (25 Nov 2024) by John M. Huthnance
AR by Yuxi Wu on behalf of the Authors (30 Nov 2024)  Author's response   Author's tracked changes   Manuscript 
ED: Publish subject to technical corrections (10 Dec 2024) by John M. Huthnance
AR by Yuxi Wu on behalf of the Authors (11 Dec 2024)  Author's response   Manuscript 
Download
Short summary
A comprehensive sand transfer model is proposed to study sediment dynamics in the lower reaches of the Changhua River on the island of Hainan. It captures the complex relationship between wave action, ocean currents, and sediment transport. Validated on the basis of on-site measurements, the model reveals significant sediment deposits which are significantly affected by coastal ocean currents and geological structures.
Share