Articles | Volume 15, issue 23
Atmos. Chem. Phys., 15, 13787–13802, 2015
Atmos. Chem. Phys., 15, 13787–13802, 2015

Research article 15 Dec 2015

Research article | 15 Dec 2015

Polarimetric radar and in situ observations of riming and snowfall microphysics during CLACE 2014

J. Grazioli et al.


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 Alexis Berne on behalf of the Authors (16 Oct 2015)  Author's response    Manuscript
ED: Publish as is (10 Nov 2015) by Timothy Garrett
Short summary
This study investigates the microphysics of winter alpine snowfall occurring in mixed-phase clouds in an inner-Alpine valley during CLACE2014. From polarimetric radar and in situ observations, riming is shown to be an important process leading to more intense snowfall. Riming is usually associated with more intense turbulence providing supercooled liquid water. Distinct features are identified in the vertical structure of polarimetric radar variables.
Final-revised paper