Articles | Volume 20, issue 21
https://doi.org/10.5194/acp-20-12655-2020
https://doi.org/10.5194/acp-20-12655-2020
Research article
 | 
03 Nov 2020
Research article |  | 03 Nov 2020

Impact of the South Asian monsoon outflow on atmospheric hydroperoxides in the upper troposphere

Bettina Hottmann, Sascha Hafermann, Laura Tomsche, Daniel Marno, Monica Martinez, Hartwig Harder, Andrea Pozzer, Marco Neumaier, Andreas Zahn, Birger Bohn, Greta Stratmann, Helmut Ziereis, Jos Lelieveld, and Horst Fischer

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AC: Author comment | RC: Referee comment | SC: Short comment | EC: Editor comment
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AR: Author's response | RR: Referee report | ED: Editor decision
AR by Bettina Hottmann on behalf of the Authors (20 May 2020)  Author's response    Manuscript
ED: Referee Nomination & Report Request started (05 Jun 2020) by Barbara Ervens
RR by Anonymous Referee #2 (19 Jun 2020)
RR by Anonymous Referee #1 (23 Jun 2020)
ED: Reconsider after major revisions (26 Jun 2020) by Barbara Ervens
AR by Bettina Hottmann on behalf of the Authors (04 Aug 2020)  Author's response    Manuscript
ED: Reconsider after major revisions (10 Aug 2020) by Barbara Ervens
AR by Bettina Hottmann on behalf of the Authors (17 Aug 2020)  Author's response    Manuscript
ED: Publish as is (20 Aug 2020) by Barbara Ervens
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Short summary
During OMO we observed enhanced mixing ratios of hydroperoxides (ROOH) in the Asian monsoon anticyclone (AMA) relative to the background. The observed mixing ratios are higher than steady-state calculations and EMAC simulations, especially in the AMA, indicating atmospheric transport of ROOH. Uncertainties in the scavenging efficiencies likely cause deviations from EMAC. Longitudinal gradients indicate a pool of ROOH towards the center of the AMA associated with upwind convection over India.
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