Spectral results from a vertical sounding of temperature and wind velo
city performed with an open stratospheric balloon in Argentina near th
e Andes mountains between 12 and 25 km of altitude, are reported. The
use of sonic anemometers allows for a higher resolution than in previo
us experiments. The data records are studied in successive subinterval
s, yielding a good spectral correlation between the ascent and the des
cent around and below the tropopause. The possibilities of an orograph
ic origin for large amplitude modes observed in the spectra and of wav
e generation by non linear interactions between them are discussed.