Articles | Volume 17, issue 9
https://doi.org/10.5194/gmd-17-3765-2024
https://doi.org/10.5194/gmd-17-3765-2024
Model evaluation paper
 | 
13 May 2024
Model evaluation paper |  | 13 May 2024

Investigating the impact of coupling HARMONIE-WINS50 (cy43) meteorology to LOTOS-EUROS (v2.2.002) on a simulation of NO2 concentrations over the Netherlands

Andrés Yarce Botero, Michiel van Weele, Arjo Segers, Pier Siebesma, and Henk Eskes

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Interactive discussion

Status: closed

Comment types: AC – author | RC – referee | CC – community | EC – editor | CEC – chief editor | : Report abuse
  • CEC1: 'Comment on egusphere-2023-1418', Juan Antonio Añel, 06 Oct 2023
    • AC1: 'Reply on CEC1', Andres Yarce Botero, 11 Oct 2023
      • CEC2: 'Reply on AC1', Juan Antonio Añel, 11 Oct 2023
        • AC2: 'Reply on CEC2', Andres Yarce Botero, 11 Oct 2023
          • CEC3: 'Reply on AC2', Juan Antonio Añel, 11 Oct 2023
            • AC3: 'Reply on CEC3', Andres Yarce Botero, 12 Oct 2023
  • RC1: 'Comment on egusphere-2023-1418', Anonymous Referee #1, 31 Oct 2023
    • AC4: 'Reply on RC1', Andres Yarce Botero, 20 Nov 2023
    • AC5: 'Reply on RC1', Andres Yarce Botero, 20 Nov 2023
  • RC2: 'Comment on egusphere-2023-1418', Anonymous Referee #2, 17 Nov 2023
    • AC7: 'Reply on RC2', Andres Yarce Botero, 16 Jan 2024

Peer review completion

AR: Author's response | RR: Referee report | ED: Editor decision | EF: Editorial file upload
AR by Andres Yarce Botero on behalf of the Authors (19 Feb 2024)  Author's response   Author's tracked changes   Manuscript 
ED: Referee Nomination & Report Request started (28 Feb 2024) by Slimane Bekki
RR by Anonymous Referee #1 (13 Mar 2024)
ED: Publish subject to technical corrections (14 Mar 2024) by Slimane Bekki
AR by Andres Yarce Botero on behalf of the Authors (19 Mar 2024)  Author's response   Manuscript 
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Short summary
HARMONIE WINS50 reanalysis data with 0.025° × 0.025° resolution from 2019 to 2021 were coupled with the LOTOS-EUROS Chemical Transport Model. HARMONIE and ECMWF meteorology configurations against Cabauw observations (52.0° N, 4.9° W) were evaluated as simulated NO2 concentrations with ground-level sensors. Differences in crucial meteorological input parameters (boundary layer height, vertical diffusion coefficient) between the hydrostatic and non-hydrostatic models were analysed.