Articles | Volume 17, issue 16
https://doi.org/10.5194/acp-17-9917-2017
https://doi.org/10.5194/acp-17-9917-2017
Research article
 | 
23 Aug 2017
Research article |  | 23 Aug 2017

Modeling the inorganic bromine partitioning in the tropical tropopause layer over the eastern and western Pacific Ocean

Maria A. Navarro, Alfonso Saiz-Lopez, Carlos A. Cuevas, Rafael P. Fernandez, Elliot Atlas, Xavier Rodriguez-Lloveras, Douglas Kinnison, Jean-Francois Lamarque, Simone Tilmes, Troy Thornberry, Andrew Rollins, James W. Elkins, Eric J. Hintsa, and Fred L. Moore

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AR: Author's response | RR: Referee report | ED: Editor decision
AR by Maria A. Navarro (deceased) on behalf of the Authors (16 Mar 2017)  Author's response   Manuscript 
ED: Referee Nomination & Report Request started (08 Apr 2017) by Martyn Chipperfield
RR by Klaus Pfeilsticker (21 Apr 2017)
RR by Anonymous Referee #2 (24 Apr 2017)
ED: Reconsider after major revisions (09 May 2017) by Martyn Chipperfield
AR by Maria A. Navarro (deceased) on behalf of the Authors (20 Jun 2017)  Author's response   Manuscript 
ED: Publish as is (18 Jul 2017) by Martyn Chipperfield
AR by Maria A. Navarro (deceased) on behalf of the Authors (18 Jul 2017)  Author's response   Manuscript 
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Short summary
Inorganic bromine (Bry) plays an important role in ozone layer depletion. Based on aircraft observations of organic bromine species and chemistry simulations, we model the Bry abundances over the Pacific tropical tropopause. Our results show BrO and Br as the dominant species during daytime hours, and BrCl and BrONO2 as the nighttime dominant species over the western and eastern Pacific, respectively. The difference in the partitioning is due to changes in the abundance of O3, NO2, and Cly.
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