“…where T is the average air temperature, W is the average relative humidity, S is the average wind speed from the local weather station, and w is a scaling coefficient. The average values of 𝐶 using [67] were 3 × 10 −15 on a clear day, 1 × 10 A probability distribution function of the 𝐶 values from the experiment could be computed to determine if this adhered to relevant channel probability distribution functions for FSO spatial mode diversity and FSO aerial communications such as Malaga, log normal, Gamma-Gamma, Nagakami, and others [68][69][70][71][72]. Log normal and Gamma-Gamma channel models are considered as special cases of the Malaga channel model, for weak turbulence and moderate-strong turbulence, respectively [72].…”