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Issue A&A
Volume 430, Number 2, February I 2005
Page(s) 739 - 746
Section Instruments, observational techniques, and data processing
DOI http://dx.doi.org/10.1051/0004-6361:20041876



A&A 430, 739-746 (2005)
DOI: 10.1051/0004-6361:20041876

An analysis of temperatures and wind speeds above Dome C, Antarctica

E. Aristidi1, K. Agabi1, M. Azouit1, E. Fossat1, J. Vernin1, T. Travouillon2, J. S. Lawrence2, C. Meyer2, J. W. V. Storey2, B. Halter3, W. L. Roth3 and V. Walden3

1  Laboratoire Universitaire d'Astrophysique de Nice, Université de Nice Sophia Antipolis, Parc Valrose, 06108 Nice Cedex 2, France
    e-mail: aristidi@unice.fr
2  School of Physics, University of New South Wales, Sydney, NSW 2052, Australia
    e-mail: tonyt@phys.unsw.edu.au
3  Department of Geography, University of Idaho, Moscow, Idaho, USA

(Received 21 August 2004 / Accepted 24 September 2004)

Abstract
A good astronomical site must fulfill several criteria including low atmospheric turbulence and low wind speeds. It is therefore important to have a detailed knowledge of the temperature and wind conditions of a location considered for future astronomical research. Antarctica has unique atmospheric conditions that have already been exploited at the South Pole station. Dome C, a site located on a local maximum of the Antarctic plateau, is likely to have even better conditions. In this paper we present the analysis of two decades of wind speed measurements taken at Dome C by an automated weather station (AWS). We also present temperature and wind speed profiles taken over four Antarctic summers using balloon-borne weather sondes. We will show that as well as having one of the lowest average wind speed ever recorded at an existing or potential observatory, Dome C also has an extremely stable upper atmosphere and a very low inversion layer.


Key words: site testing -- atmospheric effects -- balloons




© ESO 2005

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