Composition and Chemistry
Formation of stratospheric nitric acid by a hydrated ion cluster reaction: Implications for the effect of energetic particle precipitation on the middle atmosphere
Version of Record online: 17 AUG 2012
©2012. American Geophysical Union. All Rights Reserved.
Journal of Geophysical Research: Atmospheres (1984–2012)
Volume 117, Issue D16, 27 August 2012
How to Cite
2012), Formation of stratospheric nitric acid by a hydrated ion cluster reaction: Implications for the effect of energetic particle precipitation on the middle atmosphere, J. Geophys. Res., 117, D16301, doi:10.1029/2011JD017257., , , , and (
- Issue online: 17 AUG 2012
- Version of Record online: 17 AUG 2012
- Manuscript Revised: 2 JUL 2012
- Manuscript Accepted: 2 JUL 2012
- Manuscript Received: 1 DEC 2011
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|jgrd17856-sup-0002-fs01a.eps||PS document||91216K||Figure S1a. Climatological annual cycle of the ensemble-mean difference (perturbed minus control, colour shaded) for N2O (ppbv), NOx (ppbv), O3 (ppmv) and the NOx/NOy-ratio at 10 hPa. Corresponds toFigure 6a.|
|jgrd17856-sup-0003-fs01b.eps||PS document||89539K||Figure S1b. Same as in Figure S1a but for southern hemisphere (40°-90° S). Corresponds toFigure 6b|
|jgrd17856-sup-0004-fs02.eps||PS document||12172K||Figure S2. Climatological annual cycle of O3(ppmv) vs. pressure, based on monthly-mean MLS data from 2004 to 2011 (upper row: panels a,b), ensemble mean from the WACCM perturbed simulation (middle row: panels c,d) and control simulation (bottom row: panels e,f). Corresponds toFigure 4.|
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