Articles | Volume 16, issue 22
https://doi.org/10.5194/gmd-16-6899-2023
https://doi.org/10.5194/gmd-16-6899-2023
Development and technical paper
 | 
28 Nov 2023
Development and technical paper |  | 28 Nov 2023

A flexible z-layers approach for the accurate representation of free surface flows in a coastal ocean model (SHYFEM v. 7_5_71)

Luca Arpaia, Christian Ferrarin, Marco Bajo, and Georg Umgiesser

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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 gmd-2023-13', L. Bonaventura, 08 Mar 2023
    • AC1: 'Reply on RC1', Luca Arpaia, 04 Apr 2023
      • RC2: 'Reply on AC1', L. Bonaventura, 06 Apr 2023
        • AC2: 'Reply on RC2', Luca Arpaia, 06 Apr 2023
  • RC3: 'Comment on gmd-2023-13', Giacomo Capodaglio, 11 May 2023

Peer review completion

AR: Author's response | RR: Referee report | ED: Editor decision | EF: Editorial file upload
AR by Luca Arpaia on behalf of the Authors (14 Jul 2023)  Author's response   Author's tracked changes   Manuscript 
ED: Referee Nomination & Report Request started (18 Jul 2023) by Vassilios Vervatis
RR by L. Bonaventura (26 Jul 2023)
RR by Giacomo Capodaglio (14 Aug 2023)
ED: Publish subject to minor revisions (review by editor) (14 Aug 2023) by Vassilios Vervatis
AR by Luca Arpaia on behalf of the Authors (18 Sep 2023)  Author's response   Author's tracked changes   Manuscript 
ED: Publish as is (21 Sep 2023) by Vassilios Vervatis
AR by Luca Arpaia on behalf of the Authors (01 Oct 2023)  Manuscript 
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Short summary
We propose a discrete multilayer shallow water model based on z-layers which, thanks to the insertion and removal of surface layers, can deal with an arbitrarily large tidal oscillation independently of the vertical resolution. The algorithm is based on a two-step procedure used in numerical simulations with moving boundaries (grid movement followed by a grid topology change, that is, the insertion/removal of surface layers), which avoids the appearance of very thin surface layers.