Articles | Volume 16, issue 11
https://doi.org/10.5194/gmd-16-3263-2023
https://doi.org/10.5194/gmd-16-3263-2023
Development and technical paper
 | 
12 Jun 2023
Development and technical paper |  | 12 Jun 2023

A model instability issue in the National Centers for Environmental Prediction Global Forecast System version 16 and potential solutions

Xiaqiong Zhou and Hann-Ming Henry Juang

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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 egusphere-2022-1235', Anonymous Referee #1, 28 Feb 2023
    • AC1: 'Reply on RC1', Xiaqiong Zhou, 07 Mar 2023
  • RC2: 'Comment on egusphere-2022-1235', Anonymous Referee #2, 04 Apr 2023
    • AC2: 'Reply on RC2', Xiaqiong Zhou, 13 Apr 2023
  • EC1: 'Comment on egusphere-2022-1235', Simon Unterstrasser, 11 Apr 2023
    • AC3: 'Reply on EC1', Xiaqiong Zhou, 13 Apr 2023

Peer review completion

AR: Author's response | RR: Referee report | ED: Editor decision | EF: Editorial file upload
AR by Xiaqiong Zhou on behalf of the Authors (13 Apr 2023)  Author's response   Author's tracked changes   Manuscript 
ED: Publish subject to minor revisions (review by editor) (23 Apr 2023) by Simon Unterstrasser
AR by Xiaqiong Zhou on behalf of the Authors (30 Apr 2023)  Author's response   Author's tracked changes   Manuscript 
ED: Publish as is (15 May 2023) by Simon Unterstrasser
AR by Xiaqiong Zhou on behalf of the Authors (16 May 2023)  Manuscript 
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Short summary
The National Centers for Environmental Prediction Global Forecast System version 16 experienced model instability failures in real-time runs resolved by increasing the minimum thickness depth parameter. Further investigation revealed that the issue was caused by the advection of geopotential heights at the model's layer interfaces. By replacing high-order boundary conditions with zero-gradient boundary conditions for interface-wind reconstruction, the instability was effectively addressed.