On the atmospheric ozone
1951 Volume 60 Issue 2 Pages 49-52
Details
1951 Volume 60 Issue 2 Pages 49-52
The atmospheric ozone is produced by the photochemical reaction in the air and it is mainly distributed in the stratosphere. The ultra-violet solar, radiation shorter than 2850 Å is absorbed by the ozone layer which. has the thickness of only 0.3 cm when reduced to the normal state. The warm layer in the stratosphere is formed by the light absorption of ozone.
A review on the relation between the ozone and the, weather is made.
