Hostname: page-component-76fb5796d-vvkck Total loading time: 0 Render date: 2024-04-30T04:42:02.438Z Has data issue: false hasContentIssue false

On the atmosphere for astronomers above Dome C, Antarctica

Published online by Cambridge University Press:  24 August 2006

T. Sadibekova
Affiliation:
Laboratoire Universitaire d'Astrophysique de Nice, Université de Nice Sophia Antipolis, UMR 6525 Parc Valrose 06108 Nice France ESO (European Southern Observatory), Karl-Schwarzschild-Str. 2, D-85748 Garching, Germany
E. Fossat
Affiliation:
Laboratoire Universitaire d'Astrophysique de Nice, Université de Nice Sophia Antipolis, UMR 6525 Parc Valrose 06108 Nice France
C. Genthon
Affiliation:
Laboratoire de Glaciologie et Géophysique de l'Environnement (Université Joseph Fourier, Grenoble I et CNRS) 54 Rue Moliere, DU BP 96 F-38402 Saint Martin d'Heres Cedex, France
G. Krinner
Affiliation:
Laboratoire de Glaciologie et Géophysique de l'Environnement (Université Joseph Fourier, Grenoble I et CNRS) 54 Rue Moliere, DU BP 96 F-38402 Saint Martin d'Heres Cedex, France
E. Aristidi
Affiliation:
Laboratoire Universitaire d'Astrophysique de Nice, Université de Nice Sophia Antipolis, UMR 6525 Parc Valrose 06108 Nice France
K. Agabi
Affiliation:
Laboratoire Universitaire d'Astrophysique de Nice, Université de Nice Sophia Antipolis, UMR 6525 Parc Valrose 06108 Nice France
M. Azouit
Affiliation:
Laboratoire Universitaire d'Astrophysique de Nice, Université de Nice Sophia Antipolis, UMR 6525 Parc Valrose 06108 Nice France

Abstract

This paper describes a comparison between balloon radio-soundings made in summer at the Concordia station, Dome C, Antarctica and coincident model-based meteorological analyses. The comparison allows the assessment of the reliability of the analyses in summer. This allows the use of the winter analyses within an estimated range of uncertainty, while the first in situ measurements are just becoming available. The astronomical interest is to produce an estimate of atmospheric turbulence during the Antarctic winter at this very promising site. For this work the 6-hourly ECMWF operational analyses were used, concurrently with the data obtained in situ by the radio-sounding made at Concordia with standard meteorological balloons and sondes during four summer seasons (November–January), from December 2000 to the end of January 2004.

Type
PHYSICAL SCIENCES
Copyright
© Antarctic Science Ltd 2006

Access options

Get access to the full version of this content by using one of the access options below. (Log in options will check for institutional or personal access. Content may require purchase if you do not have access.)