Abstract
An experimental set-up developed for the measurement of path-averaged atmospheric refractive index structure parameter (C2n) is described followed by a brief summary of the theory involved in the generation and amplification of refractive index inhomogeneities. The results of the experiments conducted in the surface layer using a Helium-Neon laser source over an optical path length of 61.5 m at a height of 1.1 m above uniform surface are presented. The observed C2n ranges from 0.97 × 10−12 to 1.3 × 10−14 m−2/3. The diurnal variation of C2n shows rapid increase during morning hours, peaking around noon and slow decrease during evening hours. The observed relationship between the variations of C2n and temperature is explained and further studies to support and extend the present findings are indicated.