Abstract
Estimates of dissipation rate from remote-sensing techniques measuring the structure parameter Cn2 of density turbulent fluctuations assume a relationship between Cn2 and the dissipation rate ϵ. In order to obtain a precise test of this relation, in situ observations are of major importance. We present in this paper the first simultaneous in situ measurements of these parameters. The analysis of data shows that the models of turbulence used in the radar literature are not always fully justified and that the estimate of dissipation rate may be underestimated. However, we emphasize that UHF-VHF radars with high vertical resolution offer promising facilities for the observation of clear air turbulence.