Articles | Volume 18, issue 10
https://doi.org/10.5194/tc-18-4589-2024
https://doi.org/10.5194/tc-18-4589-2024
Research article
 | 
08 Oct 2024
Research article |  | 08 Oct 2024

Simulating lake ice phenology using a coupled atmosphere–lake model at Nam Co, a typical deep alpine lake on the Tibetan Plateau

Xu Zhou, Binbin Wang, Xiaogang Ma, Zhu La, and Kun Yang

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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-2023-2455', Anonymous Referee #1, 25 Mar 2024
    • AC1: 'Reply on RC1', xu zhou, 23 May 2024
  • RC2: 'Comment on egusphere-2023-2455', Laura Rontu, 14 Apr 2024
    • AC2: 'Reply on RC2', xu zhou, 23 May 2024

Peer review completion

AR: Author's response | RR: Referee report | ED: Editor decision | EF: Editorial file upload
ED: Publish subject to minor revisions (review by editor) (25 Jun 2024) by Homa Kheyrollah Pour
AR by xu zhou on behalf of the Authors (25 Jul 2024)  Author's response   Author's tracked changes   Manuscript 
ED: Publish as is (30 Jul 2024) by Homa Kheyrollah Pour
AR by xu zhou on behalf of the Authors (05 Aug 2024)
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Short summary
The simulation of the ice phenology of Nam Co by WRF is investigated. Compared with the default model, improving the key lake schemes, such as water surface roughness length for heat fluxes and the shortwave radiation transfer for lake ice, can better simulate the lake ice phenology. The still existing errors in the spatial patterns of lake ice phenology imply that challenges still exist in modelling key lake and non-lake physics such as grid-scale water circulation and snow-related processes.