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The stratosphere lies above the troposphere at 12 - 50 km. It is characterized by an increase of ozone with a maximum ozone concentration at ybout 30 km of height. Temperature also increases with height and reaches 0 °c at about 50 km. This increase is mainly caused by the ozone that absorbs the UV radiation of the sun. Doing this, the ozone layer is of essential important for the life on Earth. The stratosphere is almost without clouds because the transport of water vapour from the troposphere into the stratosphere is very limited because of the extremely low temperatures in the tropopause. The stratosphere may be devided into a lower stratosphere with a constant temperature of about -56 °C and a upper stratosphere above 20 km of height. In the upper stratosphere, temperature increases to about 0 °C from radiation absorption. Because of the increasing temperature with increasing height (like inversion weather condition) there is only very limited vertical movement. Almost 99 % of the mass of the atmosphere is located within the lower 30 km.

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