Atmospheric Chemistry and Physics
Atmospheric Chemistry and Physics
ACP
Articles | Volume 19, issue 15
Articles | Volume 19, issue 15
https://doi.org/10.5194/acp-19-9833-2019
© Author(s) 2019. This work is distributed under
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/acp-19-9833-2019
© Author(s) 2019. This work is distributed under
the Creative Commons Attribution 4.0 License.
Articles | Volume 19, issue 15
Research article
 | 
02 Aug 2019
Research article |  | 02 Aug 2019

Separating the role of direct radiative heating and photolysis in modulating the atmospheric response to the amplitude of the 11-year solar cycle forcing

Ewa M. Bednarz, Amanda C. Maycock, Peter Braesicke, Paul J. Telford, N. Luke Abraham, and John A. Pyle

Viewed

Total article views: 2,284 (including HTML, PDF, and XML)
HTML PDF XML Total Supplement BibTeX EndNote
1,458 762 64 2,284 451 61 76
  • HTML: 1,458
  • PDF: 762
  • XML: 64
  • Total: 2,284
  • Supplement: 451
  • BibTeX: 61
  • EndNote: 76
Views and downloads (calculated since 04 Apr 2018)
Cumulative views and downloads (calculated since 04 Apr 2018)

Viewed (geographical distribution)

Total article views: 2,284 (including HTML, PDF, and XML) Thereof 2,301 with geography defined and -17 with unknown origin.
Country # Views %
  • 1
1
 
 
 
 

Cited

Latest update: 14 Dec 2024
Download
Short summary
The atmospheric response to the amplitude of 11-year solar cycle in UM-UKCA is separated into the contributions from changes in direct radiative heating and photolysis rates, and the results compared with a control case with both effects included. We find that while the tropical responses are largely additive, this is not necessarily the case in the high latitudes. We suggest that solar-induced changes in ozone are important for modulating the SH dynamical response to the 11-year solar cycle.
Read more
Altmetrics
Final-revised paper
Preprint