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About ninety p.c of the ozone resides in a layer between 10 and forty kilometers (6 and 25 miles) above the Earth’s surface in a area of the environment known as the stratosphere. However in the stratosphere, the problem is one in all depletion of the protecting ozone defend, making the earth’s environment increasingly more penetrable for dangerous extremely-violet radiation. The earlier returns are attributable to local weather change driven by rising ranges of greenhouse gases (GHGs), which influences complete ozone via adjustments in stratospheric transport and temperatures, as well as chemical effects of CH4 and N2O (see Figure Q20-three).

 

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