Articles | Volume 16, issue 10
https://doi.org/10.5194/acp-16-6595-2016
https://doi.org/10.5194/acp-16-6595-2016
Research article
 | 
31 May 2016
Research article |  | 31 May 2016

Limitations of passive remote sensing to constrain global cloud condensation nuclei

Philip Stier

Viewed

Total article views: 5,904 (including HTML, PDF, and XML)
HTML PDF XML Total BibTeX EndNote
3,695 1,956 253 5,904 217 340
  • HTML: 3,695
  • PDF: 1,956
  • XML: 253
  • Total: 5,904
  • BibTeX: 217
  • EndNote: 340
Views and downloads (calculated since 19 Nov 2015)
Cumulative views and downloads (calculated since 19 Nov 2015)
Latest update: 16 Mar 2026
Download
Short summary
Cloud droplets form on suitable nuclei from aerosol emissions. Clouds with more droplets have higher reflectance so that aerosol emissions have a cooling climate effect. Numerous publications of these effects rely on passive satellite remote sensing. In this work I use a self consistent global aerosol model to show that a commonly used assumption (passively retrieved aerosol extinction is a suitable proxy for cloud condensation nuclei) is violated for a significant fraction of the Earth.
Share
Altmetrics
Final-revised paper
Preprint