Articles | Volume 21, issue 17
Atmos. Chem. Phys., 21, 13099–13117, 2021
https://doi.org/10.5194/acp-21-13099-2021
Atmos. Chem. Phys., 21, 13099–13117, 2021
https://doi.org/10.5194/acp-21-13099-2021

Research article 03 Sep 2021

Research article | 03 Sep 2021

A new conceptual model for adiabatic fog

Felipe Toledo et al.

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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 acp-2020-1314', Anonymous Referee #1, 29 Mar 2021
    • RC2: 'Reply on RC1', Anonymous Referee #2, 21 Apr 2021
      • AC2: 'Reply on RC2', Felipe Toledo, 17 Jun 2021
    • AC1: 'Reply on RC1', Felipe Toledo, 17 Jun 2021

Peer review completion

AR: Author's response | RR: Referee report | ED: Editor decision
AR by Felipe Toledo on behalf of the Authors (17 Jun 2021)  Author's response    Author's tracked changes    Manuscript
ED: Referee Nomination & Report Request started (05 Jul 2021) by Barbara Ervens
RR by Anonymous Referee #2 (20 Jul 2021)
ED: Publish subject to minor revisions (review by editor) (23 Jul 2021) by Barbara Ervens
AR by Felipe Toledo on behalf of the Authors (26 Jul 2021)  Author's response    Author's tracked changes    Manuscript
ED: Publish as is (27 Jul 2021) by Barbara Ervens
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Short summary
The article presents a new conceptual model to describe the temporal evolution of continental fog layers, developed based on 7 years of fog measurements performed at the SIRTA observatory, France. This new paradigm relates the visibility reduction caused by fog to its vertical thickness and liquid water path and provides diagnostic variables that could substantially improve the reliability of fog dissipation nowcasting at a local scale, based on real-time profiling observation.
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