Quantification of the atmospheric turbulence by the method of the equivalent temperature gradient

The goal of the paper is in the presentation of the method of the equivalent temperature gradient, which can be adequatly used for the quantification of the volume of the atmospheric turbulence. The main advantage of the method is in its simple evaluation of the turbulence for particular time moments. The simplification of the method is presented in the paper, so only the basic parameters are required for evaluation of the volume of the turbulence.