Articles | Volume 25, issue 13
https://doi.org/10.5194/acp-25-6679-2025
https://doi.org/10.5194/acp-25-6679-2025
Research article
 | 
02 Jul 2025
Research article |  | 02 Jul 2025

In-cloud characteristics observed in northeastern and midwestern US non-orographic winter storms with implications for ice particle mass growth and residence time

Luke R. Allen, Sandra E. Yuter, Declan M. Crowe, Matthew A. Miller, and K. Lee Thornhill

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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-2024-3808', Anonymous Referee #1, 23 Dec 2024
    • AC1: 'Comment on egusphere-2024-3808', Luke R. Allen, 20 Mar 2025
  • RC2: 'Comment on egusphere-2024-3808', Anonymous Referee #2, 18 Jan 2025
    • RC3: 'Reply on RC2', Anonymous Referee #2, 18 Jan 2025
    • AC1: 'Comment on egusphere-2024-3808', Luke R. Allen, 20 Mar 2025
  • RC4: 'Comment on egusphere-2024-3808', Anonymous Referee #3, 27 Jan 2025
    • AC1: 'Comment on egusphere-2024-3808', Luke R. Allen, 20 Mar 2025
  • AC1: 'Comment on egusphere-2024-3808', Luke R. Allen, 20 Mar 2025

Peer review completion

AR: Author's response | RR: Referee report | ED: Editor decision | EF: Editorial file upload
AR by Luke R. Allen on behalf of the Authors (20 Mar 2025)  Author's response   Author's tracked changes   Manuscript 
ED: Referee Nomination & Report Request started (20 Mar 2025) by Greg McFarquhar
RR by Anonymous Referee #2 (30 Mar 2025)
RR by Anonymous Referee #1 (05 Apr 2025)
RR by Anonymous Referee #3 (08 Apr 2025)
ED: Publish subject to technical corrections (08 Apr 2025) by Greg McFarquhar
AR by Luke R. Allen on behalf of the Authors (09 Apr 2025)  Manuscript 
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Short summary
We analyzed in-cloud characteristics using in situ measurements from 42 research flights across two field campaigns into non-orographic, non-lake-effect winter storms. Much of the storm volume contains weak vertical motions (a few centimeters per second), and most updrafts ≥ 0.5 m s-1 are small (< 1 km). Within 2 km of cloud radar echo top, stronger vertical motions and conditions for ice particle growth are more common. Overturning air motions near cloud top appear important for the production of snow particles.
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