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

Grazioli, J.; Lloyd, G.; Panziera, L.; Hoyle, C. R.; Connolly, P. J.; Henneberger, J.; Berne, A.

doi:https://doi.org/10.5194/acp-15-13787-2015

Articles | Volume 15, issue 23

https://doi.org/10.5194/acp-15-13787-2015

© Author(s) 2015. This work is distributed under
the Creative Commons Attribution 3.0 License.

https://doi.org/10.5194/acp-15-13787-2015

© Author(s) 2015. This work is distributed under
the Creative Commons Attribution 3.0 License.

Articles | Volume 15, issue 23

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, G. Lloyd, L. Panziera, C. R. Hoyle, P. J. Connolly, J. Henneberger, and A. Berne

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Final revised paper (published on 15 Dec 2015)
Preprint (discussion started on 02 Jul 2015)

Interactive discussion

Status: closed

AC: Author comment | RC: Referee comment | SC: Short comment | EC: Editor comment

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- Supplement

RC C5950: 'Review of ACP-2015-416', Anonymous Referee #1, 15 Aug 2015
- AC C8118: 'Responses to Reviewers', Alexis Berne, 16 Oct 2015
- AC C8120: 'REvised version with changes highlighted', Alexis Berne, 16 Oct 2015
RC C6599: 'Review: Grazioli et al., Riming in winter alpine snowfall during CLACE 2014: polarimetric radar and in-situ observations.', Anonymous Referee #2, 06 Sep 2015
- AC C8119: 'Responses to Reviewers', Alexis Berne, 16 Oct 2015

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.