Articles | Volume 18, issue 21
Research article
07 Nov 2018
Research article |  | 07 Nov 2018

Balloon-borne measurements of temperature, water vapor, ozone and aerosol backscatter on the southern slopes of the Himalayas during StratoClim 2016–2017

Simone Brunamonti, Teresa Jorge, Peter Oelsner, Sreeharsha Hanumanthu, Bhupendra B. Singh, K. Ravi Kumar, Sunil Sonbawne, Susanne Meier, Deepak Singh, Frank G. Wienhold, Bei Ping Luo, Maxi Boettcher, Yann Poltera, Hannu Jauhiainen, Rijan Kayastha, Jagadishwor Karmacharya, Ruud Dirksen, Manish Naja, Markus Rex, Suvarna Fadnavis, and Thomas Peter


Interactive discussion

Status: closed
Status: closed
AC: Author comment | RC: Referee comment | SC: Short comment | EC: Editor comment
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Peer-review completion

AR: Author's response | RR: Referee report | ED: Editor decision
AR by Simone Brunamonti on behalf of the Authors (01 Sep 2018)  Author's response    Manuscript
ED: Referee Nomination & Report Request started (03 Sep 2018) by Farahnaz Khosrawi
RR by Anonymous Referee #2 (21 Sep 2018)
ED: Publish subject to minor revisions (review by editor) (24 Sep 2018) by Farahnaz Khosrawi
AR by Simone Brunamonti on behalf of the Authors (04 Oct 2018)  Author's response    Manuscript
ED: Publish as is (09 Oct 2018) by Farahnaz Khosrawi
Short summary
Based on balloon-borne measurements performed in India and Nepal in 2016–2017, we infer the vertical distributions of water vapor, ozone and aerosols in the atmosphere, from the surface to 30 km altitude. Our measurements show that the atmospheric dynamics of the Asian summer monsoon system over the polluted Indian subcontinent lead to increased concentrations of water vapor and aerosols in the high atmosphere (approximately 14–20 km altitude), which can have an important effect on climate.
Final-revised paper