Rise in temperature in stratosphere caused by the absorption of
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Unlike the troposphere, the temperature within the stratosphere increases with altitude, primarily as a result of the absorption of UV radiation by ozone. The mesosphere is the layer of the atmosphere between 50-80 km above the Earth's surface. It is within this layer that satellites orbit the Earth.
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The stratosphere is stratified (layered) in temperature, with warmer layers higher and cooler layers closer to the Earth; this increase of temperature with altitude is a result of the absorption of the Sun's ultraviolet radiation by the ozone layer.
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