Articles | Volume 15, issue 11
Atmos. Chem. Phys., 15, 6225–6236, 2015
https://doi.org/10.5194/acp-15-6225-2015

Special issue: Oxidant Production over Antarctic Land and its Export...

Atmos. Chem. Phys., 15, 6225–6236, 2015
https://doi.org/10.5194/acp-15-6225-2015

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 et al.

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Cited articles

Andreas, E. L.: Physically based model of the form drag associated with sastrugi. US Army Cold Regions Research and Engineering Laboratory, Hanover, NH, CRREL Report No CR 95–16, 12 pp., 1995.
Argentini, S. and Pietroni, I.: An Integrated Observing System for Boundary Layer Monitoring at Concordia Station, Antarctica, in: Integrated Ground-Based Observing Systems, edited by: Cimini, D., Marzano, F., and Visconti, G., Springer-Verlag, Berlin Heidelberg, 199–208, 2010.
Argentini, S., Pietroni, I., Mastrantonio, G., Petenko, I., and Viola, A.: Use of a high-resolution sodar to study surface-layer turbulence at night, Bound.-Lay. Meteorol., 143, 177–188, 2011.
Argentini, S., Petenko, I., Viola, A., Mastrantonio, G., Pietroni, I., Casasanta, G., Aristidi, E., and Genthon, C.: The surface layer observed by a high-resolution sodar at DOME C, Antarctica, Ann. Geophys.-Italy, 56, F0557, https://doi.org/10.4401/ag-6347, 2013.
Bintanja, R.: Snowdrift suspension and atmospheric turbulence. Part I: Theoretical background and model description, Bound.-Lay. Meteorol., 95, 343–368, 2000.
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.
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