Articles | Volume 15, issue 19
https://doi.org/10.5194/gmd-15-7449-2022
https://doi.org/10.5194/gmd-15-7449-2022
Development and technical paper
 | 
07 Oct 2022
Development and technical paper |  | 07 Oct 2022

The Moist Quasi-Geostrophic Coupled Model: MQ-GCM 2.0

Sergey Kravtsov, Ilijana Mastilovic, Andrew McC. Hogg, William K. Dewar, and Jeffrey R. Blundell

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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-2021-160', Anonymous Referee #1, 18 Jul 2021
    • AC1: 'Reply on RC1', Sergey Kravtsov, 12 Jun 2022
  • CEC1: 'Comment on gmd-2021-160', Juan Antonio Añel, 14 Aug 2021
    • CC1: 'Reply on CEC1', Ilijana Mastilovic, 26 Aug 2021
  • RC2: 'Comment on gmd-2021-160', Anonymous Referee #2, 06 Jun 2022
    • AC2: 'Reply on RC2', Sergey Kravtsov, 12 Jun 2022

Peer review completion

AR: Author's response | RR: Referee report | ED: Editor decision
AR by Sergey Kravtsov on behalf of the Authors (30 Jun 2022)  Author's response    Author's tracked changes    Manuscript
ED: Publish subject to minor revisions (review by editor) (11 Jul 2022) by Sophie Valcke
AR by Sergey Kravtsov on behalf of the Authors (11 Jul 2022)  Author's response    Author's tracked changes    Manuscript
ED: Publish subject to technical corrections (12 Jul 2022) by Sophie Valcke
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Short summary
Climate is a complex system whose behavior is shaped by multitudes of processes operating on widely different spatial scales and timescales. In hierarchical modeling, one goes back and forth between highly idealized process models and state-of-the-art models coupling the entire range of climate subsystems to identify specific phenomena and understand their dynamics. The present contribution highlights an intermediate climate model focussing on midlatitude ocean–atmosphere interactions.