The Earth’s atmosphere acts as a source of O2 and a repository of CO2, but its also acts as a shield for life. First, nearly all meteorites burn up on entry because of the high temperatures generated by the friction of the atmosphere. Second, the atmosphere acts as a shield for high energy UV radiation.
Although UV radiation converts 7-dehydrocholesterol into vitamin D3 in the skin (Figure 2), and is therefore useful, high energy UV destroys living cells. In fact the darkening we call a suntan is actually the body’s mechanism for preventing further UV damage. Sun burn and skin cancer are caused by relatively weak UV light that reaches the Earth’s surface, without the atmosphere we would be exposed to high energy UV that would be a hazard to all life on Earth. The Earth’s “sun screen” is ozone (O3). And without ozone in the upper atmosphere there would be no life on Earth.
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The ozone layer is located in the lower portion of the stratosphere from approximately 10 km to 50 km above Earth, though the thickness varies seasonally and geographically. This layer contains over 91% of the ozone in Earth’s atmosphere and absorbs 93-99% of the sun's high frequency ultraviolet light. The ozone decomposes photolytically to O2 and molecular oxygen, Equation 10, and it is this reaction that accounts for the UV protection of the atmosphere. Ozone is naturally regenerated by the exothermic reaction of the molecular oxygen with O2, Equation 11.


The balance between ozone formation and destruction is thus an important mechanism for the protection of living organisms on the planet. While the ozone layer had been relatively constant on Earth for millions of years, the last 70 have seen a dramatic change including the increase in the polar hole in the ozone layer. The ozone hole is defined geographically as the area where the total ozone concentration is less than 220 Dobson Units.
Note:
The ozone hole has steadily grown in size and length of existence over the past two and half decades. At present the size of ozone hole over Antarctica is estimated to be about 30 million sq.km (Figure 3).
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