Articles | Volume 18, issue 23
Atmos. Chem. Phys., 18, 17325–17354, 2018
https://doi.org/10.5194/acp-18-17325-2018
Atmos. Chem. Phys., 18, 17325–17354, 2018
https://doi.org/10.5194/acp-18-17325-2018
Research article
06 Dec 2018
Research article | 06 Dec 2018

CALIPSO (IIR–CALIOP) retrievals of cirrus cloud ice-particle concentrations

David L. Mitchell et al.

Viewed

Total article views: 2,245 (including HTML, PDF, and XML)
HTML PDF XML Total Supplement BibTeX EndNote
1,420 791 34 2,245 123 42 36
  • HTML: 1,420
  • PDF: 791
  • XML: 34
  • Total: 2,245
  • Supplement: 123
  • BibTeX: 42
  • EndNote: 36
Views and downloads (calculated since 19 Jun 2018)
Cumulative views and downloads (calculated since 19 Jun 2018)

Viewed (geographical distribution)

Total article views: 2,153 (including HTML, PDF, and XML) Thereof 2,142 with geography defined and 11 with unknown origin.
Country # Views %
  • 1
1
 
 
 
 

Cited

Latest update: 24 May 2022
Download
Short summary
To realistically model a changing climate, global measurements of cirrus cloud ice-particle number concentration (N) and size (De) are needed, through which one may infer the general mechanism of ice formation. A satellite remote sensing method was developed to measure N and De. It was found that N was highest and De lowest at high latitudes. In the Arctic, cirrus clouds occurred much more often during winter, which may have an impact on mid-latitude winter weather.
Altmetrics
Final-revised paper
Preprint