Articles | Volume 24, issue 20
https://doi.org/10.5194/acp-24-11653-2024
https://doi.org/10.5194/acp-24-11653-2024
Research article
 | 
18 Oct 2024
Research article |  | 18 Oct 2024

Evolution of cloud droplet temperature and lifetime in spatiotemporally varying subsaturated environments with implications for ice nucleation at cloud edges

Puja Roy, Robert M. Rauber, and Larry Di Girolamo

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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-2024-526', Anonymous Referee #1, 14 Mar 2024
  • RC2: 'Comment on egusphere-2024-526', Anonymous Referee #2, 24 Mar 2024

Peer review completion

AR: Author's response | RR: Referee report | ED: Editor decision | EF: Editorial file upload
AR by Puja Roy on behalf of the Authors (13 Jun 2024)  Author's response   Author's tracked changes   Manuscript 
ED: Referee Nomination & Report Request started (09 Jul 2024) by Thijs Heus
RR by Anonymous Referee #1 (16 Aug 2024)
ED: Publish subject to minor revisions (review by editor) (16 Aug 2024) by Thijs Heus
AR by Puja Roy on behalf of the Authors (18 Aug 2024)  Author's response   Author's tracked changes   Manuscript 
ED: Publish as is (20 Aug 2024) by Thijs Heus
AR by Puja Roy on behalf of the Authors (30 Aug 2024)  Manuscript 
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Short summary
Cloud droplet temperature and lifetime impact cloud microphysical processes such as the activation of ice-nucleating particles. We investigate the thermal and radial evolution of supercooled cloud droplets and their surrounding environments with an aim to better understand observed enhanced ice formation at supercooled cloud edges. This analysis shows that the magnitude of droplet cooling during evaporation is greater than estimated from past studies, especially for drier environments.

 
 
 
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