Articles | Volume 21, issue 22
Atmos. Chem. Phys., 21, 16843–16868, 2021
https://doi.org/10.5194/acp-21-16843-2021
Atmos. Chem. Phys., 21, 16843–16868, 2021
https://doi.org/10.5194/acp-21-16843-2021

Research article 19 Nov 2021

Research article | 19 Nov 2021

Midlatitude mixed-phase stratocumulus clouds and their interactions with aerosols: how ice processes affect microphysical, dynamic, and thermodynamic development in those clouds and interactions?

Seoung Soo Lee et al.

Download

Interactive discussion

Status: closed

Comment types: AC – author | RC – referee | CC – community | EC – editor | CEC – chief editor | : Report abuse
  • RC1: 'Comment on acp-2020-1318', Anonymous Referee #1, 08 Apr 2021
    • AC1: 'Reply on RC1', Seoung Soo Lee, 11 Jul 2021
  • RC2: 'Comment on acp-2020-1318', Anonymous Referee #2, 12 May 2021
    • AC3: 'Reply on RC2', Seoung Soo Lee, 11 Jul 2021

Peer review completion

AR: Author's response | RR: Referee report | ED: Editor decision
AR by Seoung Soo Lee on behalf of the Authors (11 Jul 2021)  Author's response    Author's tracked changes    Manuscript
ED: Referee Nomination & Report Request started (16 Jul 2021) by Martina Krämer
RR by Anonymous Referee #2 (05 Aug 2021)
ED: Reconsider after major revisions (30 Aug 2021) by Martina Krämer
AR by Seoung Soo Lee on behalf of the Authors (26 Sep 2021)  Author's response    Author's tracked changes    Manuscript
ED: Publish as is (28 Sep 2021) by Martina Krämer
Download
Short summary
Using a modeling framework, a midlatitude stratocumulus cloud system is simulated. It is found that cloud mass in the system becomes very low due to interactions between ice and liquid particles compared to that in the absence of ice particles. It is also found that interactions between cloud mass and aerosols lead to a reduction in cloud mass in the system, and this is contrary to an aerosol-induced increase in cloud mass in the absence of ice particles.
Altmetrics
Final-revised paper
Preprint