Articles | Volume 16, issue 9
https://doi.org/10.5194/acp-16-5793-2016
https://doi.org/10.5194/acp-16-5793-2016
Research article
 | 
12 May 2016
Research article |  | 12 May 2016

The origin of midlatitude ice clouds and the resulting influence on their microphysical properties

Anna E. Luebke, Armin Afchine, Anja Costa, Jens-Uwe Grooß, Jessica Meyer, Christian Rolf, Nicole Spelten, Linnea M. Avallone, Darrel Baumgardner, and Martina Krämer

Viewed

Total article views: 4,299 (including HTML, PDF, and XML)
HTML PDF XML Total BibTeX EndNote
2,667 1,482 150 4,299 138 106
  • HTML: 2,667
  • PDF: 1,482
  • XML: 150
  • Total: 4,299
  • BibTeX: 138
  • EndNote: 106
Views and downloads (calculated since 07 Dec 2015)
Cumulative views and downloads (calculated since 07 Dec 2015)

Cited

Saved (preprint)

Latest update: 13 Nov 2024
Download

The requested paper has a corresponding corrigendum published. Please read the corrigendum first before downloading the article.

Short summary
In this study, we present observational evidence to show that two distinct types of cirrus clouds exist – in situ origin and liquid origin cirrus. These two types differ by their formation mechanism and other properties. Airborne, in-cloud measurements of cloud ice water content (IWC), ice crystal concentration (Nice), and ice crystal size from the 2014 ML-CIRRUS campaign provide cloud samples that have been divided and analyzed according to their origin type.
Altmetrics
Final-revised paper
Preprint