::: Ozone Depletion :::

    NCCoPP Ozone Depletion
 
Ozone is an unstable form of molecular oxygen. About 90% of the ozone is found in the upper stratosphere. It forms a concentrated band, roughly between 19 and 23 km above the earth’s surface, and acts as a shield absorbing ultraviolet radiation, especially UV-B.
Man-made chemicals such as chlorofluorocarbons (CFCs) released into the atmosphere start chemical reactions that destroy the ozone layer.

The picture alongside shows the hole in the ozone layer (area marked grey) over the Antarctic. The affected area depicted is approximately 28 Mio km2 or 8.5 times the size of the Indian continent!! It will require many dozens of years (scientists say 50 years or more) to repair the damage, even with the Ozone Depleting Substances phased out.

Protecting the Ozone Layer
The first international agreement to protect the ozone layer was the Vienna Convention on the Protection of the Ozone layer. This was followed by the Montreal Protocol on Substances that Deplete the Ozone layer in 1987. The Montreal Protocol was substantially revised four times, the latest being in 1999 (Beijing). The Montreal Protocol stipulates that the production and consumption of compounds that deplete the ozone layer like, chlorofluorocarbons (CFCs), halons, and carbontetrachloride are to be phased out by 2010 while methyl chloroform by 2005.

Total ozone (DU)/ Ozone total (UD), 2006/09/25



DU - Dobson unit
Ozone Hole Antarctica
25 September 2006




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