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ACP | Articles | Volume 19, issue 21
Atmos. Chem. Phys., 19, 13547–13567, 2019
https://doi.org/10.5194/acp-19-13547-2019
© Author(s) 2019. This work is distributed under
the Creative Commons Attribution 4.0 License.
Atmos. Chem. Phys., 19, 13547–13567, 2019
https://doi.org/10.5194/acp-19-13547-2019
© Author(s) 2019. This work is distributed under
the Creative Commons Attribution 4.0 License.

Research article 07 Nov 2019

Research article | 07 Nov 2019

Transport of the 2017 Canadian wildfire plume to the tropics via the Asian monsoon circulation

Corinna Kloss et al.

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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 Corinna Kloss on behalf of the Authors (18 Jun 2019)  Author's response    Manuscript
ED: Referee Nomination & Report Request started (21 Jun 2019) by Hang Su
RR by Michael Fromm (03 Jul 2019)
RR by Anonymous Referee #2 (24 Jul 2019)
ED: Reconsider after major revisions (01 Aug 2019) by Hang Su
AR by Corinna Kloss on behalf of the Authors (22 Sep 2019)  Author's response    Manuscript
ED: Publish as is (07 Oct 2019) by Hang Su
Publications Copernicus
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Short summary
With satellite measurements and transport models, we show that a plume resulting from strong Canadian fires in July/August 2017 was not only distributed throughout the northern/higher latitudes, but also reached the faraway tropics, aided by the circulation of Asian monsoon anticyclone. The regional climate impact in the wider Asian monsoon area in September exceeds the impact of the Asian tropopause aerosol layer by a factor of ~ 3 and compares to that of an advected moderate volcanic eruption.
With satellite measurements and transport models, we show that a plume resulting from strong...
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