Articles | Volume 22, issue 6
Atmos. Chem. Phys., 22, 4129–4147, 2022
https://doi.org/10.5194/acp-22-4129-2022
Atmos. Chem. Phys., 22, 4129–4147, 2022
https://doi.org/10.5194/acp-22-4129-2022
Research article
31 Mar 2022
Research article | 31 Mar 2022

Radiative and microphysical responses of clouds to an anomalous increase in fire particles over the Maritime Continent in 2015

Azusa Takeishi and Chien Wang

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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-2021-674', Anonymous Referee #1, 19 Oct 2021
    • AC1: 'Reply on RC1', Azusa Takeishi, 09 Nov 2021
      • RC3: 'Reply on AC1', Anonymous Referee #1, 16 Nov 2021
  • RC2: 'Comment on acp-2021-674', Anonymous Referee #2, 16 Nov 2021

Peer review completion

AR: Author's response | RR: Referee report | ED: Editor decision
AR by Azusa Takeishi on behalf of the Authors (14 Jan 2022)  Author's response    Author's tracked changes    Manuscript
ED: Referee Nomination & Report Request started (21 Jan 2022) by Toshihiko Takemura
RR by Anonymous Referee #2 (12 Feb 2022)
ED: Publish subject to minor revisions (review by editor) (12 Feb 2022) by Toshihiko Takemura
AR by Azusa Takeishi on behalf of the Authors (21 Feb 2022)  Author's response    Author's tracked changes    Manuscript
ED: Publish as is (23 Feb 2022) by Toshihiko Takemura
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Short summary
Nanometer- to micrometer-sized particles in the atmosphere, namely aerosols, play a crucial role in cloud formation as cloud droplets form on aerosols. This study uses a weather forecasting model to examine the impacts of a large emission of aerosol particles from biomass burning activities over Southeast Asia. We find that additional cloud droplets brought by fire-emitted particles can lead to taller and more reflective convective clouds with increased rainfall.
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