Articles | Volume 19, issue 21
https://doi.org/10.5194/acp-19-13547-2019
https://doi.org/10.5194/acp-19-13547-2019
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, Gwenaël Berthet, Pasquale Sellitto, Felix Ploeger, Silvia Bucci, Sergey Khaykin, Fabrice Jégou, Ghassan Taha, Larry W. Thomason, Brice Barret, Eric Le Flochmoen, Marc von Hobe, Adriana Bossolasco, Nelson Bègue, and Bernard Legras

Download

Interactive discussion

Status: closed
Status: closed
AC: Author comment | RC: Referee comment | SC: Short comment | EC: Editor comment
Printer-friendly Version - Printer-friendly version Supplement - Supplement

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
AR by Corinna Kloss on behalf of the Authors (08 Oct 2019)  Manuscript 
Download
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.
Altmetrics
Final-revised paper
Preprint