Articles | Volume 17, issue 8
https://doi.org/10.5194/acp-17-5221-2017
https://doi.org/10.5194/acp-17-5221-2017
Research article
 | 
21 Apr 2017
Research article |  | 21 Apr 2017

Genesis of diamond dust, ice fog and thick cloud episodes observed and modelled above Dome C, Antarctica

Philippe Ricaud, Eric Bazile, Massimo del Guasta, Christian Lanconelli, Paolo Grigioni, and Achraf Mahjoub

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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 Philippe Ricaud on behalf of the Authors (06 Feb 2017)  Author's response   Manuscript 
ED: Referee Nomination & Report Request started (06 Feb 2017) by Markus Petters
RR by Anonymous Referee #1 (17 Feb 2017)
RR by Anonymous Referee #2 (03 Mar 2017)
RR by Anonymous Referee #3 (20 Mar 2017)
ED: Reconsider after minor revisions (Editor review) (26 Mar 2017) by Markus Petters
AR by Philippe Ricaud on behalf of the Authors (31 Mar 2017)  Author's response   Manuscript 
ED: Publish as is (31 Mar 2017) by Markus Petters
AR by Philippe Ricaud on behalf of the Authors (03 Apr 2017)
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Short summary
The novelty of the paper is to combine a large set of measurements and meteorological models to study the genesis of thick cloud and diamond dust/ice fog (ice crystals) episodes above Dome C, Antarctica. The originality of the work is to attribute the presence of thick cloud and diamond dust/ice fog to advection and microphysical processes with oceanic and continental origin of air masses, respectively. Thick cloud episodes are reproduced by the models but not diamond dust/ice fog episode.
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