The climate of Kazakhstan is on most of the territory is sharply continental, with large amplitudes of temperatures; relatively dry. The average annual rainfall in most parts of the territory of small — 100-500 mm stand mid-mountain areas of the South of the country, where temperature mountain-valley inversions are large areas with relatively mild winter conditions and high rainfall, as exemplified by the climate of Almaty. K the South of parallel 43° (in Kazakhstan it is the areas to the South line Aktau—Shymkent) climate scientists are isolated in a special Iranian subtropical region[1], which in General dominate the heated mass of dry air of tropical origin. Although winter weather in this southern subzone is very unstable due to the periodic intrusion of cold Northern mass and local mountain-valley phenomena, it has a positive average temperatures in each month and high average temperatures overall for the year (from +10 and above).