Articles | Volume 17, issue 5
https://doi.org/10.5194/gmd-17-2117-2024
https://doi.org/10.5194/gmd-17-2117-2024
Model description paper
 | 
13 Mar 2024
Model description paper |  | 13 Mar 2024

Modelling water isotopologues (1H2H16O, 1H217O) in the coupled numerical climate model iLOVECLIM (version 1.1.5)

Thomas Extier, Thibaut Caley, and Didier M. Roche

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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-2023-149', Anonymous Referee #1, 23 Jul 2023
  • RC2: 'Comment on gmd-2023-149', Anonymous Referee #2, 05 Aug 2023
  • CEC1: 'Comment on gmd-2023-149', Juan Antonio Añel, 06 Sep 2023

Peer review completion

AR: Author's response | RR: Referee report | ED: Editor decision | EF: Editorial file upload
AR by Thomas Extier on behalf of the Authors (01 Dec 2023)  Author's response   Author's tracked changes   Manuscript 
ED: Referee Nomination & Report Request started (05 Dec 2023) by Andy Wickert
RR by Anonymous Referee #2 (11 Dec 2023)
RR by Anonymous Referee #1 (14 Dec 2023)
ED: Publish subject to minor revisions (review by editor) (14 Dec 2023) by Andy Wickert
AR by Thomas Extier on behalf of the Authors (22 Dec 2023)  Author's response   Author's tracked changes   Manuscript 
ED: Publish subject to technical corrections (07 Jan 2024) by Andy Wickert
AR by Thomas Extier on behalf of the Authors (23 Jan 2024)  Manuscript 
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Short summary
Stable water isotopes are used to infer changes in the hydrological cycle for different time periods in climatic archive and climate models. We present the implementation of the δ2H and δ17O water isotopes in the coupled climate model iLOVECLIM and calculate the d- and 17O-excess. Results of a simulation under preindustrial conditions show that the model correctly reproduces the water isotope distribution in the atmosphere and ocean in comparison to data and other global circulation models.