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What is ozone layer destruction?


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Advancing destruction of the ozone layer

The ozone layer, situated in the stratosphere about 15 to 30 km above the earth's surface, plays the important role of "space suit" that protects us living beings by absorbing harmful ultraviolet radiation (UVB) from the sun.


The ozone layer is currently being destroyed by CFCs and other substances, its depletion progressing globally except in the tropical zone.

The ozone layer is disappearing at a particularly high rate in high-latitude areas.
In the Antarctic Circle, a large ozone hole has been observed for eight consecutive years from 1989 through 1996.


NB: m atm-cm, milli-atmosphere centimeter indicates total ozone amount, i.e., the amount of ozone contained in a vertical air column in the atmosphere; 300 atm-cm has a thickness of 3 mm when ozone in the air column is entirely compressed at 0 and 1 atmospheric pressure.
Annual Change in Three Ozone Hole Factors
(Meteorological Agency: Ozone Layer Observation Report, 1996)


Impact of ozone layer destruction

Destruction of the ozone layer increases the amount of harmful ultraviolet radiation (UVB), which in turn can result in increased cases of skin cancer, and visual impediments such as cataract. It can also hinder the growth of plants and negatively impact small living organisms, such as zooplankton, phytoplankton, shrimp larvae and the young of fish.


What is CFC?

CFC, chlorofluorocarbon, is the collective name for compounds made of carbon, fluorine, chlorine and hydrogen. Because of their stable, harmless and non-combustible properties, they are widely used in everyday applications such as cleansing agents for electronic components, coolants for air conditioners, foaming agents for the manufacture of insulating materials and so on. CFC variations include HCFC and HFC.
  • CFC (Chlorofluorocarbon)
    Because of CFC's strong ozone layer-destroying effect, its production was totally banned at the end of 1995.
    It is necessary to ensure proper handling of CFC in appliances currently in use.

  • HCFC (Hydrochlorofluorocarbon)
    Although less powerful than CFC in destroying the ozone layer, HCFC must be also contained.


Mechanism of ozone layer destruction by CFCs

Since CFCs are chemically stable, when released into the atmosphere they pass through the troposphere at about 20 km altitude without decomposing, reaching the stratosphere, where they are chemically decomposed by short-wavelength ultraviolet rays, releasing chlorine atoms. In a chain reaction, the chlorine atoms destroy the ozone layer in the stratosphere.

Mechanism of Ozone Layer Destruction by CFC in Stratosphere



Prediction of future ozone layer destruction

The 1994 general report of the scientific, environmental impact and technological economic assessment panel of the UNEP predicted that the amount of chlorine and bromine would peak in 1994 in the troposphere, while in the stratosphere it would reach peak 3 - 5 years later and begin to decrease, provided that all the signatory countries observe the revised Montreal Protocol of 1992.
From this, it is predicted that the global ozone decrease will continue during the remaining years of the 20th century, but that if other factors remain unchanged, the ozone layer will begin to be restored in the early 21st century and the Antarctic ozone hole will disappear around the year 2045.


Effective Straospheric Chlorine Concentration

(1994 UNEP report)


 
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