Articles | Volume 22, issue 2
Atmos. Chem. Phys., 22, 881–901, 2022
https://doi.org/10.5194/acp-22-881-2022
Atmos. Chem. Phys., 22, 881–901, 2022
https://doi.org/10.5194/acp-22-881-2022

Research article 19 Jan 2022

Research article | 19 Jan 2022

On the cross-tropopause transport of water by tropical convective overshoots: a mesoscale modelling study constrained by in situ observations during the TRO-Pico field campaign in Brazil

Abhinna K. Behera et al.

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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 acp-2021-543', Anonymous Referee #1, 26 Jul 2021
    • AC1: 'Reply on RC1', Abhinna Behera, 14 Nov 2021
  • RC2: 'Comment on acp-2021-543', Anonymous Referee #2, 27 Jul 2021
    • AC2: 'Reply on RC2', Abhinna Behera, 14 Nov 2021
  • RC3: 'Comment on acp-2021-543', Anonymous Referee #3, 03 Sep 2021
    • AC3: 'Reply on RC3', Abhinna Behera, 14 Nov 2021

Peer review completion

AR: Author's response | RR: Referee report | ED: Editor decision
AR by Abhinna Behera on behalf of the Authors (14 Nov 2021)  Author's response    Author's tracked changes    Manuscript
ED: Publish as is (11 Dec 2021) by Timothy J. Dunkerton
AR by Abhinna Behera on behalf of the Authors (17 Dec 2021)  Author's response    Manuscript
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Short summary
Deep convection overshooting the stratosphere's contribution to the global stratospheric water budget is still being quantified. We ran three different cloud-resolving simulations of an observed case of overshoots in Bauru during the TRO-Pico balloon campaign in the context of upscaling the impact of overshoots at a large scale. These simulations, which have been validated with balloon-borne and S-band radar measurements, shed light on the local-scale variability and composition of overshoots.
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