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Ann. Geophys., 24, 415-426, 2006
www.ann-geophys.net/24/415/2006/
© European Geosciences Union 2006


Analysis of wind data in the low atmosphere from a RASS sodar

I. A. Pérez, M. A. García, M. L. Sánchez, and B. de Torre
Department of Applied Physics, Faculty of Sciences, University of Valladolid, Valladolid, Spain

Abstract. This paper focuses on the ability of a sodar to describe some characteristics of the atmospheric vertical structure and presents some techniques for meteorological data evaluation. The measuring campaign took place in April 2001 and consisted of 10-min averages covering the lower atmosphere from 40 to 500 m at 20-m levels. Three methods were considered, the first of which was a scalar analysis performed using a combination of wind and temperature median profiles. A noticeable contrast between day and night was obtained. Flat wind profiles during the day were a consequence of prevailing convective conditions that determined thermal turbulence. A stable layer above 260 m capped the unstable layer situated below and guaranteed the stability of the boundary layer. During the night, the presence of a low level jet was the most significant feature. The height of the core was 340 m and the higher vertical winds defined it clearly. The second method focused on the wind vector. In this analysis, the anti-cyclonic rotation of hourly averages was considered in the lower levels where it was observed. After a translation of the origin, an empirical, robust model with two parts was then proposed for the resulting vector. The angle was described linearly and the module by a second order model for cylindrical data. Finally, as a third method, three regression analyses were investigated: vectorial, taking every wind component separately and scalar. The two first seemed to be more complete due to their description of anti-cyclonic wind rotation when height increased. Correlation coefficients also proved to be more satisfactory. As a consequence, these techniques, although less frequently used, are more suitable to study wind in the low atmosphere.

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Citation: Pérez, I. A., García, M. A., Sánchez, M. L., and de Torre, B.: Analysis of wind data in the low atmosphere from a RASS sodar, Ann. Geophys., 24, 415-426, 2006.   Bibtex   EndNote   Reference Manager