“…A safe, non-contact remote method of measuring the snow cover height in the avalanche centre, which does not require large material and time costs, is the method of georadiolocation. In addition, there are currently theoretical developments that make it possible to consider the radiolocation method for studying snow cover properties [9][10][11]. The relative simplicity and speed of obtaining such information would help to cover a large area of avalanche-prone territories, study the regularities of snow cover distribution, as well as the peculiarities of spatial occurrence of snow layers in avalanche formation, their structure, density, and water content.…”