Articles | Volume 22, issue 5
https://doi.org/10.5194/acp-22-3169-2022
https://doi.org/10.5194/acp-22-3169-2022
Research article
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10 Mar 2022
Research article | Highlight paper |  | 10 Mar 2022

Persistence of moist plumes from overshooting convection in the Asian monsoon anticyclone

Sergey M. Khaykin, Elizabeth Moyer, Martina Krämer, Benjamin Clouser, Silvia Bucci, Bernard Legras, Alexey Lykov, Armin Afchine, Francesco Cairo, Ivan Formanyuk, Valentin Mitev, Renaud Matthey, Christian Rolf, Clare E. Singer, Nicole Spelten, Vasiliy Volkov, Vladimir Yushkov, and Fred Stroh

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Interactive discussion

Status: closed

Comment types: AC – author | RC – referee | CC – community | EC – editor | CEC – chief editor | : Report abuse
  • RC1: 'Review of “Persistence of moist plumes from overshooting convection in the Asian monsoon anticyclone” by Sergey M. Khaykin et al.', Anonymous Referee #1, 27 Sep 2021
  • RC2: 'Comment on acp-2021-653', Anonymous Referee #2, 05 Oct 2021
  • RC3: 'Comment on acp-2021-653', Anonymous Referee #3, 05 Oct 2021

Peer review completion

AR: Author's response | RR: Referee report | ED: Editor decision
AR by Sergey Khaykin on behalf of the Authors (09 Jan 2022)  Author's response    Author's tracked changes    Manuscript
ED: Publish subject to technical corrections (29 Jan 2022) by Corinna Hoose
AR by Sergey Khaykin on behalf of the Authors (31 Jan 2022)  Author's response    Manuscript
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Short summary
The Asian monsoon anticyclone is the key contributor to the global annual maximum in lower stratospheric water vapour. We investigate the impact of deep convection on the lower stratospheric water using a unique set of observations aboard the high-altitude M55-Geophysica aircraft deployed in Nepal in summer 2017 within the EU StratoClim project. We find that convective plumes of wet air can persist within the Asian anticyclone for weeks, thereby enhancing the occurrence of high-level clouds.
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