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-19-10717-2019
© Author(s) 2019. This work is distributed under
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/acp-19-10717-2019
© 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 1: Core types and evolution during a cloud's lifetime

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

Viewed

Total article views: 3,608 (including HTML, PDF, and XML)
HTML PDF XML Total BibTeX EndNote
2,152 1,298 158 3,608 196 222
  • HTML: 2,152
  • PDF: 1,298
  • XML: 158
  • Total: 3,608
  • BibTeX: 196
  • EndNote: 222
Views and downloads (calculated since 30 Aug 2018)
Cumulative views and downloads (calculated since 30 Aug 2018)

Viewed (geographical distribution)

Total article views: 3,608 (including HTML, PDF, and XML) Thereof 3,539 with geography defined and 69 with unknown origin.
Country # Views %
  • 1
1
 
 
 
 

Cited

Saved (final revised paper)

Latest update: 10 Sep 2026
Download
Short summary
It is useful to divide a cloud into two regions: core and margin. Three parameters used to define a core are compared: buoyancy (B), relative humidity (RH), and vertical velocity (W). Using theoretical arguments and simulations, we show that during most of a cloud's lifetime, the cores are subsets of one another: Bcore ⊆ RHcore ⊆ Wcore. Moreover, the core–shell cloud model applies to all core definitions. Our findings can serve as a benchmark in the partition the core and margin.
Read more
Share
Altmetrics
Final-revised paper
Preprint