The
distribution of ozone in the stratosphere is a function of altitude, latitude
and season. It is determined by photochemical and transport processes. The
ozone layer is located between 10 and 50 km above the Earth's surface and
contains 90% of all stratospheric ozone. Under normal conditions, stratospheric
ozone is formed by a photochemical reaction between oxygen molecules, oxygen
atoms and solar radiation. Read more here.
Courtesy: http://esl.jrc.it
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