Quantifying uncertainties of climate signals in chemistry climate models related to the 11-year solar cycle – Part 1: Annual mean response in heating rates, temperature, and ozone
Markus Kunze et al.
Viewed
Total article views: 1,547 (including HTML, PDF, and XML)
HTML
PDF
XML
Total
Supplement
BibTeX
EndNote
1,125
404
18
1,547
300
21
19
HTML: 1,125
PDF: 404
XML: 18
Total: 1,547
Supplement: 300
BibTeX: 21
EndNote: 19
Views and downloads (calculated since 31 Jan 2020)
Cumulative views and downloads
(calculated since 31 Jan 2020)
Total article views: 1,008 (including HTML, PDF, and XML)
HTML
PDF
XML
Total
Supplement
BibTeX
EndNote
746
249
13
1,008
208
15
13
HTML: 746
PDF: 249
XML: 13
Total: 1,008
Supplement: 208
BibTeX: 15
EndNote: 13
Views and downloads (calculated since 12 Jun 2020)
Cumulative views and downloads
(calculated since 12 Jun 2020)
Total article views: 539 (including HTML, PDF, and XML)
HTML
PDF
XML
Total
Supplement
BibTeX
EndNote
379
155
5
539
92
6
6
HTML: 379
PDF: 155
XML: 5
Total: 539
Supplement: 92
BibTeX: 6
EndNote: 6
Views and downloads (calculated since 31 Jan 2020)
Cumulative views and downloads
(calculated since 31 Jan 2020)
Viewed (geographical distribution)
Total article views: 1,547 (including HTML, PDF, and XML)
Thereof 1,625 with geography defined
and -78 with unknown origin.
Total article views: 1,008 (including HTML, PDF, and XML)
Thereof 1,152 with geography defined
and -144 with unknown origin.
Total article views: 539 (including HTML, PDF, and XML)
Thereof 473 with geography defined
and 66 with unknown origin.
Modelling the response of the atmosphere and its constituents to 11-year solar variations is subject to a certain uncertainty arising from the solar irradiance data set used in the chemistry–climate model (CCM) and the applied CCM itself.
This study reveals significant influences from both sources on the variations in the solar response in the stratosphere and mesosphere.
However, there are also regions where the random, unexplained part of the variations in the solar response is largest.
Modelling the response of the atmosphere and its constituents to 11-year solar variations is...
