Articles | Volume 11, issue 3
https://doi.org/10.5194/gmd-11-1161-2018
https://doi.org/10.5194/gmd-11-1161-2018
Development and technical paper
 | 
29 Mar 2018
Development and technical paper |  | 29 Mar 2018

A fully consistent and conservative vertically adaptive coordinate system for SLIM 3D v0.4 with an application to the thermocline oscillations of Lake Tanganyika

Philippe Delandmeter, Jonathan Lambrechts, Vincent Legat, Valentin Vallaeys, Jaya Naithani, Wim Thiery, Jean-François Remacle, and Eric Deleersnijder

Download

Interactive discussion

Status: closed
Status: closed
AC: Author comment | RC: Referee comment | SC: Short comment | EC: Editor comment
Printer-friendly Version - Printer-friendly version Supplement - Supplement

Peer-review completion

AR: Author's response | RR: Referee report | ED: Editor decision
AR by Philippe Delandmeter on behalf of the Authors (19 Jan 2018)  Author's response   Manuscript 
ED: Publish subject to minor revisions (review by editor) (07 Feb 2018) by James Maddison
AR by Philippe Delandmeter on behalf of the Authors (16 Feb 2018)  Author's response   Manuscript 
ED: Publish subject to technical corrections (04 Mar 2018) by James Maddison
AR by Philippe Delandmeter on behalf of the Authors (05 Mar 2018)  Author's response   Manuscript 
Download
Short summary
The discontinuous Galerkin (DG) finite element method is well suited for the modelling of three-dimensional flows exhibiting strong density gradients. Here, a vertical adaptive mesh method is developed for DG finite element methods and implemented into SLIM 3D. This technique increases drastically the accuracy of simulations including strong stratification, without affecting the simulation cost. SLIM 3D is then used to simulate the thermocline oscillations of Lake Tanganyika.