Articles | Volume 16, issue 4
Research article
03 Mar 2016
Research article |  | 03 Mar 2016

Transport pathways from the Asian monsoon anticyclone to the stratosphere

Hella Garny and William J. Randel


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 Hella Garny on behalf of the Authors (02 Jan 2016)  Author's response
ED: Referee Nomination & Report Request started (20 Jan 2016) by Gabriele Stiller
RR by Anonymous Referee #2 (27 Jan 2016)
ED: Publish subject to technical corrections (17 Feb 2016) by Gabriele Stiller
AR by Hella Garny on behalf of the Authors (22 Feb 2016)  Author's response    Manuscript
Short summary
We investigate the fate of air that originates in the monsoon region in the upper troposphere, where it was transported to by convection. We find that almost half of the air parcels released in the monsoon region in the upper troposphere reach the stratosphere within 60 days, and most ascend to the tropical lower stratosphere. This suggests that trace gases, including pollutants, that are transported into the stratosphere via the Asian monsoon are in a position to enter the deep stratosphere.
Final-revised paper