The stratosphere begins at lower latitudes with an average height of 12 km and extends up to 80 km.
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On the distribution of temperature and other physical characteristics of the heterogeneity of the stratosphere is divided into three layers:
1) the lower isothermal, which extends to an altitude of 30-35 km. The constancy of temperature in this layer due to radiative equilibrium: the radiant heat flux is equal to the outflow;
2) medium, or hot, the layer extending from 35 to 55 km. This layer is characterized by a temperature rise of the strong absorption by ozone of ultraviolet radiation of the sun. (From the height of 5-10 km ozone concentrations in the atmosphere increases significantly and reaches a maximum at an altitude of 20-25 km. Above the ozone concentration decreases, and at an altitude of 56-60 km of winding down);
3) the upper, or cold, a layer of length - from 55 to 80 km. In this layer, with increasing altitude the temperature decreases rapidly.
The ionosphere extends to a height of more than 80 miles directly above the stratosphere. A characteristic feature of this area is substantial ionization and conductivity. The ionosphere extends to an altitude of about 2000-3000 km. Next is the sphere scattering.
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In the troposphere, from the Earth's surface and to an altitude of 11 km (in the temperate latitudes) - the temperature is lowered by 6,5 ° C per kilometer.
In the stratosphere at an altitude of 11 to 32 km the temperature range from -25 up to -85 ° C, with an average temperature for this altitude can be considered -56,5 ° C (standard atmosphere).
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Then the temperature rises and at a height of 50-65 km in the range from + 25 to +150 ° C. The mean temperature for this altitude can be considered as +75 ° C. Further, up to a height of 80 km the temperature is lowered to -105 ° C. The new , is a regular increase in the temperature starts from a height of about 85 km