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

Viewed

Total article views: 2,572 (including HTML, PDF, and XML)
HTML PDF XML Total BibTeX EndNote
1,642 816 114 2,572 64 92
  • HTML: 1,642
  • PDF: 816
  • XML: 114
  • Total: 2,572
  • BibTeX: 64
  • EndNote: 92
Views and downloads (calculated since 05 Dec 2016)
Cumulative views and downloads (calculated since 05 Dec 2016)

Viewed (geographical distribution)

Total article views: 2,572 (including HTML, PDF, and XML) Thereof 2,554 with geography defined and 18 with unknown origin.
Country # Views %
  • 1
1
 
 
 
 

Cited

Saved (preprint)

Discussed (final revised paper)

Latest update: 23 Apr 2024
Download
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.
Altmetrics
Final-revised paper
Preprint