Introduction to Ozone Depletion
Ozone is both beneficial and harmful to us. Near the ground, ozone forming as a result of chemical reactions involving traffic pollution and sunlight may cause a number of respiratory problems, particularly for young children. However, high up in the atmosphere in a region known as the stratosphere, ozone filters out incoming radiation from the Sun in the cell-damaging ultraviolet (UV) part of the spectrum. Without this ozone layer, life on earth would not have evolved in the way it has.
Concentrations of ozone in the stratosphere fluctuate naturally in response to variations in weather conditions and amounts of energy being released from the Sun, and to major volcanic eruptions. Nevertheless, during the 1970s it was realised that man-made emissions of CFCs and other chemicals used in refrigeration, aerosols and cleansing agents may cause a significant destruction of ozone in the stratosphere, thereby letting through more of the harmful ultraviolet radiation. Then in 1985 evidence of a large "ozone hole" was discovered above the continent of Antarctica during the springtime. This has reappeared annually, generally growing larger and deeper each year. More recently, fears have emerged about significant ozone depletion over the Arctic, closer to the more populous regions of the Northern Hemisphere.
In response to this and additional fears about more widespread global ozone depletion, the Montreal Protocol on Substances that Deplete the Ozone Layer was implemented in 1987. This legally binding international treaty called for participating developed nations to reduce the use of CFCs and other ozone depleting substances. In 1990 and again in 1992, subsequent Amendments to the Protocol brought forward the phase out date for CFCs for developed countries to 1995.
Protecting the ozone layer is essential. Ultraviolet radiation from the Sun can cause a variety of health problems in humans, including skin cancers, eye cataracts and a reduction in the body's immunity to disease. Furthermore, ultraviolet radiation can be damaging to microscopic life in the surface oceans which forms the basis of the world’s marine food chain, certain varieties of crops including rice and soya, and polymers used in paints and clothing. A loss of ozone in the stratosphere may even affect the global climate.
International agreements and other legislation have gone a long way to safeguarding this life-supporting shield. Nevertheless, for there to be real and long-lasting success, everyone must become part of the solution. Individual efforts taken together can be powerful forces for environmental change. There are a number of things that we, as individuals, can do to both protect the ozone layer. These include proper disposal of old refrigerators, the use of halon-free fire extinguishers and the recycling of foam and other non-disposable packaging. Finally, we should all be aware that whilst emissions of ozone depleters are now being controlled, the ozone layer is not likely to fully repair itself for several decades. Consequently, we should take precautions when exposing ourselves to the Sun.
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Websites
• ARIC
• British Antarctic Survey
• Environment Canada
• US EPA
• World Meteorological Org.
• Environment Canada
• Environment Canada
• Scientific Assessment 1994
• Scientific Assessment 1998
• OzonAction
• DETR
• Concerned Scientists
Other topics
• Introduction
• Antarctica
• Arctic
• Causes
• CFCs
• Doing Our Bit
• Evidence
• Eye Disorders
• Global Climate
• Human Health
• Immune System
• Impacts
• Land Plants
• Legislation
• Materials Damage
• Measuring
• Monitoring
• Montreal Protocol
• ODCs
• Ozone
• Ozone Hole
• Ozone Layer
• Polar Vortex
• Protection
• PSCs
• Sea Life
• Skin Cancer
• Stratosphere
• Sun
• UV Radiation
• Volcanoes