Articles | Volume 17, issue 22
https://doi.org/10.5194/acp-17-13833-2017
https://doi.org/10.5194/acp-17-13833-2017
Research article
 | 
21 Nov 2017
Research article |  | 21 Nov 2017

Sensitivity of surface temperature to radiative forcing by contrail cirrus in a radiative-mixing model

Ulrich Schumann and Bernhard Mayer

Viewed

Total article views: 3,105 (including HTML, PDF, and XML)
HTML PDF XML Total BibTeX EndNote
1,931 1,048 126 3,105 70 97
  • HTML: 1,931
  • PDF: 1,048
  • XML: 126
  • Total: 3,105
  • BibTeX: 70
  • EndNote: 97
Views and downloads (calculated since 29 May 2017)
Cumulative views and downloads (calculated since 29 May 2017)

Viewed (geographical distribution)

Total article views: 3,105 (including HTML, PDF, and XML) Thereof 3,058 with geography defined and 47 with unknown origin.
Country # Views %
  • 1
1
 
 
 
 

Cited

Latest update: 20 Nov 2024
Download
Short summary
It is generally assumed that a positive radiative forcing of the atmosphere implies a warming of the Earth surface. This assumption is valid for well-mixed greenhouse gases but is not guaranteed for disturbances which cause a vertically variable radiative heating rate profile with warming in the upper troposphere and cooling near the surface. This conceptual study shows that the warming induced by contrail cirrus prevails only for fast vertical heat exchange by mixing within the troposphere.
Altmetrics
Final-revised paper
Preprint