Articles | Volume 16, issue 3
Research article
17 Feb 2016
Research article |  | 17 Feb 2016

Drizzle formation in stratocumulus clouds: effects of turbulent mixing

L. Magaritz-Ronen, M. Pinsky, and A. Khain


Interactive discussion

Status: closed
Status: closed
AC: Author comment | RC: Referee comment | SC: Short comment | EC: Editor comment
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Peer-review completion

AR: Author's response | RR: Referee report | ED: Editor decision
AR by Leehi Magaritz Ronen on behalf of the Authors (11 Jan 2016)  Author's response    Manuscript
ED: Referee Nomination & Report Request started (13 Jan 2016) by Markus Petters
RR by Anonymous Referee #2 (28 Jan 2016)
ED: Publish subject to technical corrections (28 Jan 2016) by Markus Petters
Short summary
The mechanism of drizzle formation in shallow stratocumulus clouds and the effect of turbulent mixing on this process are investigated using a Lagrangian-Eularian model of the cloud-topped boundary layer. It was found that first large drops form in volumes that are closest to adiabatic with extended residence near cloud top, and maximum values of LWC. Turbulent mixing was found able to delay the process of drizzle initiation but is essential for the further development of drizzle in the cloud.
Final-revised paper