METHOD OF CALCULATION OF THE MAXIMUM DEEP INFLUENCING THE SOIL AND THE MIDDLE VISIT OF THE SNOW COVERING IN THE GIRLS OF THE LVIV REGION AND AT THE PLACE OF THE TERRITORY OF POLAND BY RENDERED FORMULA
The maximum depth of freezing of the soil and the average height of snow cover mountain regions of Lviv region and the adjoining territory of Poland have not been studied enough. The calculation of climatic parameters data was carried out for the first time in the methodology of the directions between the initial and final meteorological stations or the transition station, the formulas of high-altitude coefficients using correction coefficients at the distance between stations. To calculate the maximum depths of freezing of the soil and average snow cover heights, simplified formulas are proposed and the heights of the horizontals of topographic maps are used. Freezing of the soil is the spread of winter in the soil of negative temperature. The depth of freezing depends on the type and cultivation of the soil, which determine its heat and thermal conductivity, moisture, which prevents freezing as a result of the hidden heat when freezing water, the thickness of the snow cover and the available vegetation, which protects the soil from strong cooling. In the calculations of the depth of freezing of soil, the average height of the snow cover, which was at the time of maximum freezing of the soil in the meteorological stations, was taken into account
