Preprints
https://doi.org/10.5194/egusphere-2022-740
https://doi.org/10.5194/egusphere-2022-740
23 Aug 2022
 | 23 Aug 2022

Temperature and CCN sensitivity of orographic precipitation enhanced by a mixed-phase seeder-feeder mechanism

Julia Thomas, Andrew Barrett, and Corinna Hoose

Abstract. Orographic precipitation is a key driver of flooding in mountainous areas. This article investigates the microphysical response of orographic rainfall to perturbations of temperature and cloud condensation nuclei (CCN) concentration. The study is motivated by the increased water vapour capacity of the atmosphere in a warming climate and the increasing frequency of extreme rainfall events. A case study for the Cumbria flood in December 2015 is performed with sensitivities using a realization of the `piggybacking' method implemented into a limited-area setup of the ICON model. A 6 % K-1 enhancement of rainfall results for the highest altitudes, caused by a `mixed-phase seeder-feeder mechanism', i.e. the interplay of melting and accretion. Total 24 h rainfall is found to increase by only 2 % K-1, significantly less than the 7 % K-1 increase in atmospheric water vapour. A rain budget analysis reveals that the negative temperature sensitivity of the condensation ratio and the increase of rain evaporation dampen the rainfall enhancement. Decreasing the CCN concentration speeds up the microphysical processing, which leads to an increase in total rainfall. At low CCN concentration the rainfall sensitivity to temperature is systematically smaller. It is shown that the CCN and temperature sensitivities are to a large extent independent (with a ±3 % relative error) and additive.

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Journal article(s) based on this preprint

08 Feb 2023
Temperature and cloud condensation nuclei (CCN) sensitivity of orographic precipitation enhanced by a mixed-phase seeder–feeder mechanism: a case study for the 2015 Cumbria flood
Julia Thomas, Andrew Barrett, and Corinna Hoose
Atmos. Chem. Phys., 23, 1987–2002, https://doi.org/10.5194/acp-23-1987-2023,https://doi.org/10.5194/acp-23-1987-2023, 2023
Short summary
Julia Thomas, Andrew Barrett, and Corinna Hoose

Interactive discussion

Status: closed

Comment types: AC – author | RC – referee | CC – community | EC – editor | CEC – chief editor | : Report abuse
  • RC1: 'Comment on egusphere-2022-740', Anonymous Referee #1, 26 Sep 2022
  • RC2: 'Comment on egusphere-2022-740', Anonymous Referee #2, 29 Sep 2022
  • RC3: 'Comment on egusphere-2022-740', Anonymous Referee #3, 02 Oct 2022
  • AC1: 'Replies', Corinna Hoose, 30 Nov 2022

Interactive discussion

Status: closed

Comment types: AC – author | RC – referee | CC – community | EC – editor | CEC – chief editor | : Report abuse
  • RC1: 'Comment on egusphere-2022-740', Anonymous Referee #1, 26 Sep 2022
  • RC2: 'Comment on egusphere-2022-740', Anonymous Referee #2, 29 Sep 2022
  • RC3: 'Comment on egusphere-2022-740', Anonymous Referee #3, 02 Oct 2022
  • AC1: 'Replies', Corinna Hoose, 30 Nov 2022

Peer review completion

AR: Author's response | RR: Referee report | ED: Editor decision | EF: Editorial file upload
AR by Corinna Hoose on behalf of the Authors (01 Dec 2022)  Author's response   Author's tracked changes   Manuscript 
ED: Referee Nomination & Report Request started (04 Dec 2022) by Hailong Wang
RR by Omid Alizadeh (05 Dec 2022)
RR by Anonymous Referee #4 (07 Jan 2023)
ED: Publish as is (07 Jan 2023) by Hailong Wang
AR by Corinna Hoose on behalf of the Authors (11 Jan 2023)  Author's response   Manuscript 

Journal article(s) based on this preprint

08 Feb 2023
Temperature and cloud condensation nuclei (CCN) sensitivity of orographic precipitation enhanced by a mixed-phase seeder–feeder mechanism: a case study for the 2015 Cumbria flood
Julia Thomas, Andrew Barrett, and Corinna Hoose
Atmos. Chem. Phys., 23, 1987–2002, https://doi.org/10.5194/acp-23-1987-2023,https://doi.org/10.5194/acp-23-1987-2023, 2023
Short summary
Julia Thomas, Andrew Barrett, and Corinna Hoose
Julia Thomas, Andrew Barrett, and Corinna Hoose

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Latest update: 19 Sep 2024
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Short summary
We study the sensitivity of rain formation processes during a heavy rainfall event over mountains to changes in temperature and pollution. Total rainfall increases by 2 % K-1, while a 6 % K-1 rainfall increase is found at the highest altitudes, caused by a mixed-phase seeder-feeder mechanism (frozen cloud particles melt and grow further as they fall through a liquid cloud layer). In a cleaner atmosphere, this process is enhanced. Thus, the risk for severe rainfall in mountains may increase in future.