Articles | Volume 20, issue 15
Atmos. Chem. Phys., 20, 9393–9417, 2020
Atmos. Chem. Phys., 20, 9393–9417, 2020

Research article 11 Aug 2020

Research article | 11 Aug 2020

The impact of biomass burning on upper tropospheric carbon monoxide: a study using MOCAGE global model and IAGOS airborne data

Martin Cussac et al.


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 Martin Cussac on behalf of the Authors (10 Jun 2020)  Author's response    Manuscript
ED: Publish as is (30 Jun 2020) by Andreas Hofzumahaus
Short summary
Biomass burning emissions are a major source of carbon monoxide in the atmosphere. Here, the vertical transport that these emissions can undergo until the upper troposphere is investigated, as well as their contribution to carbon monoxide concentrations. It was found that boreal forest emissions were specific to the occurrence of pyroconvection directly above the fires, whereas biomass burning emissions from other regions of the globe relied more on the occurrence of deep convection.
Final-revised paper