Abstract
Fifteen hours of Sodar echoes, collected during the 4th Environmental CEC Campaign at Turbigo, Italy, in September 1979, have been analyzed. We discuss the vertical profiles and the time evolution of the second and third statistical moments of the vertical component of wind velocity, measured at a rate of one height-profile every 6 s for a height range of 1000 m and a vertical resolution of 29 m. We also analyze the power spectra of the vertical velocity.
Similar content being viewed by others
References
Berico, M., Mastrantonio, G., and Ricotta, A.: 1980, ‘Preliminary Analysis of the Measurements Obtained with the Triaxial Sodar System during the 4th Environmental CEC Campaign (in Italian)’,Internal Report, LPS-80-14.
Berico, M., Fiocco, G., Mastrantonio, G., and Ricotta, A.: 1981, ‘Spatial and Temporal Correlations of the Intensity and of the Vertical Velocity Field Obtained with a Tri-Axial Doppler Sodar’,Proc. 1st Intl. Symp. on Acoustic Remote Sensing of tha Atmosphere and Oceans, Calgary,IV, 98–106.
Berico, M. and Ricotta, A.: 1983, ‘Operation of two Monostatic Doppler Sodar Systems in the Thermo-electric Turbigo Power Plant (in italian)’,Internal Report, IFA-83-6.
Longhetto, A., Guillot, P., Anfossi, D., Bacci, P., Elisei, G., Frego, G., Sandroni, S., and Varey, R.: 1982, ‘Atmospheric-Dispersion Experiments in the Near and Medium Field’,Il Nuovo Cimento 3C, 299–331.
Melling, H. and List, R.: 1980, ‘Characteristics of Vertical Velocity Fluctuations in a Convective Urban Boundary Layer’,J. Appl. Meteorol. 19, 1184–1195.
Ricotta, A. and Berico, M.: 1980, ‘Triaxial Sodar System (in italian)’,Internal Report, LPS-80-6.
Weill, A., Baudin, F., Goutorbe, J. P., Van Grunderbeeck, P., and Lebere, P.: 1978, ‘Turbulence Structure in Temperature Inversions and in Convection Fields as Observed by Doppler Sodar’,Boundary-Layer Meteorol. 15, 375–390.
Weill, A., Klapisz, C., Strauss, B., Baudin, F., Jaupart, C., Van Grunderbeeck, P., and Goutorbe, J. P.: 1980, ‘Measuring Heat Flux and Structure Functions of Temperature Fluctuations with an Acoustic Doppler Sodar’,J. Appl. Meteorol. 19, 199–205.
Willis, G. E. and Deardorff, J. W.: 1974, ‘A Laboratory Model of the Unstable Planetary Boundary Layer’,J. Atmos. Sci. 31, 1297–1307.
Author information
Authors and Affiliations
Rights and permissions
About this article
Cite this article
Ricotta, A., Berico, M. & Mazzola, S. Structure of the vertical velocity field analyzed with a Doppler Sodar. Boundary-Layer Meteorol 27, 311–325 (1983). https://doi.org/10.1007/BF02033742
Accepted:
Issue Date:
DOI: https://doi.org/10.1007/BF02033742