green house effect and orone layer depletion optional
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the trapping of the sun's warmth in a planet's lower atmosphere, due to the greater transparency of the atmosphere to visible radiation from the sun than to infrared radiation emitted from the planet's surface.
on the stratospheric ozone layer. ... Gaseous CFCs can deplete theozone layer when they slowly rise into the stratosphere, are broken down by strong ultraviolet radiation, release chlorine atoms, and then react with ozonemolecules.
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