Atmospheric Chemistry and Physics
Atmospheric Chemistry and Physics
ACP
Articles | Volume 19, issue 16
Articles | Volume 19, issue 16
https://doi.org/10.5194/acp-19-10739-2019
© Author(s) 2019. This work is distributed under
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/acp-19-10739-2019
© Author(s) 2019. This work is distributed under
the Creative Commons Attribution 4.0 License.
Articles | Volume 19, issue 16
Research article
 | 
26 Aug 2019
Research article |  | 26 Aug 2019

Core and margin in warm convective clouds – Part 2: Aerosol effects on core properties

Reuven H. Heiblum, Lital Pinto, Orit Altaratz, Guy Dagan, and Ilan Koren

Viewed

Total article views: 2,114 (including HTML, PDF, and XML)
HTML PDF XML Total BibTeX EndNote
1,309 761 44 2,114 62 58
  • HTML: 1,309
  • PDF: 761
  • XML: 44
  • Total: 2,114
  • BibTeX: 62
  • EndNote: 58
Views and downloads (calculated since 30 Aug 2018)
Cumulative views and downloads (calculated since 30 Aug 2018)

Viewed (geographical distribution)

Total article views: 2,114 (including HTML, PDF, and XML) Thereof 2,075 with geography defined and 39 with unknown origin.
Country # Views %
  • 1
1
 
 
 
 

Cited

Latest update: 09 May 2025
Download
Short summary
The effects of aerosol concentration on a cloud's partition to core and margin are examined. The main finding from Part I (i.e. Bcore ⊆ RHcore ⊆ Wcore) is seen for all aerosol concentrations. Clouds can produce positive buoyancy due to both saturated updrafts or unsaturated downdrafts; the latter are dependent on low aerosol concentrations. We show that a cloud's mass is mainly dependent on core processes (condensation), while its volume is mainly dependent on margin processes (evaporation).
Read more
Share
Altmetrics
Final-revised paper
Preprint