Articles | Volume 20, issue 8
https://doi.org/10.5194/acp-20-5035-2020
https://doi.org/10.5194/acp-20-5035-2020
Research article
 | 
28 Apr 2020
Research article |  | 28 Apr 2020

Supercooled drizzle development in response to semi-coherent vertical velocity fluctuations within an orographic-layer cloud

Adam Majewski and Jeffrey R. French

Viewed

Total article views: 1,775 (including HTML, PDF, and XML)
HTML PDF XML Total BibTeX EndNote
1,158 567 50 1,775 54 48
  • HTML: 1,158
  • PDF: 567
  • XML: 50
  • Total: 1,775
  • BibTeX: 54
  • EndNote: 48
Views and downloads (calculated since 07 Oct 2019)
Cumulative views and downloads (calculated since 07 Oct 2019)

Viewed (geographical distribution)

Total article views: 1,775 (including HTML, PDF, and XML) Thereof 1,668 with geography defined and 107 with unknown origin.
Country # Views %
  • 1
1
 
 
 
 

Cited

Latest update: 05 Jul 2024
Download
Short summary
The study reports formation of supercooled drizzle drops in response to repeating kilometer-wide updrafts and downdrafts within a mixed-phase, mountain-layer cloud containing very little ice despite cold cloud top temperatures (T ~ -30°C). The discrete, embedded hydrometeor growth layers and downwind transition to drizzle production at cloud top indicates the relative importance of kinematic mechanisms in determining the location of precipitation development in cloud.
Altmetrics
Final-revised paper
Preprint