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The stratosphere is a region of intense interactions among radiative, dynamical, and chemical processes, in which the horizontal mixing of gaseous components proceeds much more rapidly than does vertical mixing.
The stratosphere is a layer of extremely stratified air that rises 40 kilometres above the tropopause and comprises about 20% of the atmosphere’s mass. A two-step reactive mechanism produces ozone in the stratosphere naturally.
The stratosphere is the layer of air that extends approximately 40 km above the tropopause and contains about 20% of the atmosphere's mass. It plays an active role in the Earth's climate system, influenced by solar and infrared radiation, ozone chemistry, and transport of waves from the troposphere. From: Sub-Seasonal to Seasonal Prediction, 2019
The stratosphere is a layer of Earth's atmosphere. It is the second layer of the atmosphere as you go upward. The troposphere, the lowest layer, is right below the stratosphere. The next higher layer above the stratosphere is the mesosphere.
19 Οκτ 2024 · Stratosphere, layer of Earth’s atmosphere lying between the troposphere and the mesosphere. The lower portion of the stratosphere is nearly isothermal (a layer of constant temperature), whereas temperatures in its upper levels increase with altitude.
6 Σεπ 2014 · The stratosphere layer is a region of intense interactions between the radiative, dynamic, and chemical processes, in which the horizontal mixing of gaseous components proceeds much more rapidly than the vertical mixing.
Stratosphere is the region where about 90 % of ozone is formed. Ozone (chemical formula: O 3 ) is a gas that is formed by the action of the sun’s rays on oxygen present in the stratosphere. Ozone is important as it absorbs harmful ultraviolet rays of the sun.