Characterization of the boundary layer at Dome C (East Antarctica) during the OPALE summer campaign

Gallée, H.; Preunkert, S.; Argentini, S.; Frey, M. M.; Genthon, C.; Jourdain, B.; Pietroni, I.; Casasanta, G.; Barral, H.; Vignon, E.; Amory, C.; Legrand, M.

doi:https://doi.org/10.5194/acp-15-6225-2015

Articles | Volume 15, issue 11

https://doi.org/10.5194/acp-15-6225-2015

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

Special issue:

Oxidant Production over Antarctic Land and its Export...

https://doi.org/10.5194/acp-15-6225-2015

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

Articles | Volume 15, issue 11

Research article

|

08 Jun 2015

Research article |

| 08 Jun 2015

Characterization of the boundary layer at Dome C (East Antarctica) during the OPALE summer campaign

H. Gallée, S. Preunkert, S. Argentini, M. M. Frey, C. Genthon, B. Jourdain, I. Pietroni, G. Casasanta, H. Barral, E. Vignon, C. Amory, and M. Legrand

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Final revised paper (published on 08 Jun 2015)
Preprint (discussion started on 23 Dec 2014)

Interactive discussion

Status: closed

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

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RC C11100: 'Characterization of the boundary layer at Dome C (East Antarctica) during the OPALE summer campaign', Anonymous Referee #1, 11 Jan 2015
RC C11555: 'Review', Anonymous Referee #2, 25 Jan 2015
AC C12755: 'Response to the reviewers', Hubert Gallée, 25 Mar 2015

Peer-review completion

AR: Author's response | RR: Referee report | ED: Editor decision

AR by Hubert Gallée on behalf of the Authors (17 Apr 2015) Manuscript

ED: Publish as is (08 May 2015) by Thorsten Bartels-Rausch

AR by Hubert Gallée on behalf of the Authors (13 May 2015) Author's response Manuscript

Short summary

Regional climate model MAR was run for the region of Dome C located on the East Antarctic plateau, during summer 2011–2012, with a high vertical resolution in the lower troposphere. MAR is generally in very good agreement with the observations and provides sufficiently reliable information about surface turbulent fluxes and vertical profiles of vertical diffusion coefficients when discussing the representativeness of chemical measurements made nearby the ground surface at Dome C.