Articles | Volume 15, issue 14
https://doi.org/10.5194/gmd-15-5689-2022
https://doi.org/10.5194/gmd-15-5689-2022
Development and technical paper
 | 
22 Jul 2022
Development and technical paper |  | 22 Jul 2022

Embedding a one-column ocean model in the Community Atmosphere Model 5.3 to improve Madden–Julian Oscillation simulation in boreal winter

Yung-Yao Lan, Huang-Hsiung Hsu, Wan-Ling Tseng, and Li-Chiang Jiang

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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-2021-346', Anonymous Referee #1, 02 Jan 2022
    • AC1: 'Reply on RC1', Yung-Yao Lan, 09 Feb 2022
  • RC2: 'Comment on gmd-2021-346', Anonymous Referee #2, 13 Jan 2022
    • AC2: 'Reply on RC2', Yung-Yao Lan, 09 Feb 2022

Peer review completion

AR: Author's response | RR: Referee report | ED: Editor decision | EF: Editorial file upload
AR by Yung-Yao Lan on behalf of the Authors (09 Feb 2022)
EF by Polina Shvedko (10 Feb 2022)  Author's tracked changes 
EF by Polina Shvedko (10 Feb 2022)  Author's response 
EF by Polina Shvedko (10 Feb 2022)  Supplement 
EF by Polina Shvedko (10 Feb 2022)  Manuscript 
ED: Referee Nomination & Report Request started (28 Apr 2022) by Richard Neale
RR by Anonymous Referee #1 (10 May 2022)
ED: Publish subject to minor revisions (review by editor) (09 Jun 2022) by Richard Neale
AR by Yung-Yao Lan on behalf of the Authors (19 Jun 2022)  Author's response   Author's tracked changes   Manuscript 
ED: Publish as is (26 Jun 2022) by Richard Neale
AR by Yung-Yao Lan on behalf of the Authors (01 Jul 2022)  Manuscript 
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Short summary
This study has shown that coupling a high-resolution 1-D ocean model (SIT 1.06) with the Community Atmosphere Model 5.3 (CAM5.3) significantly improves the simulation of the Madden–Julian Oscillation (MJO) over the standalone CAM5.3. Systematic sensitivity experiments resulted in more realistic simulations of the tropical MJO because they had better upper-ocean resolution, adequate upper-ocean thickness, coupling regions including the eastern Pacific and southern tropics, and a diurnal cycle.