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Ozone Hole FAQ
Frequently Asked Questions about the Ozone Hole

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Ozone Hole FAQ : Weather Underground

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What are the human health effects of increased UV-B light?
Has ozone loss contributed to an observed increase in sunburns and skin cancer in humans?
What is the effect of increased UV-B light on plants?
What is the effect of increased UV-B light on marine life?
Is the worldwide decline in amphibians due to ozone depletion?
Are sheep going blind in Chile?
What do the skeptics say about the ozone hole?
What are the costs and savings of the CFC phaseout?
What steps have been taken to save the ozone layer? Are they working?
What replacement chemicals for CFCs have been found? Are they safe?
When was the ozone hole discovered?
How do CFCs destroy ozone?
Are volcanos a major source of chlorine to the stratosphere?
What is ozone pollution?
Where can I go to learn more about the ozone hole?


What is the ozone hole?
The "ozone hole" is a loss of stratospheric ozone in springtime over Antarctica, peaking in September. The ozone hole area is defined as the size of the region with total ozone below 220 Dobson units (DU). Dobson Units are a unit of measurement that refer to the thickness of the ozone layer in a vertical column from the surface to the top of the atmosphere, a quantity called the "total column ozone amount." Prior to 1979, total column ozone values over Antarctica never fell below 220 DU. The hole has been proven to be a result of human activities--the release of huge quantities of chlorofluorocarbons (CFCs) and other ozone depleting substances into the atmosphere.

How big was the 2007 ozone hole, and is it getting bigger?
Every four years, a team of many of the top scientists researching ozone depletion put together a comprehensive summary of the scientific knowledge on the subject, under the auspices of the World Meteorological Organization (WMO). According to their most recent assessment, (WMO, 2006), monthly total column ozone amounts in September and October have continued to be 40 to 50% below pre-ozone-hole values, with up to 70% decreases for periods of a week or so. During the last decade, the average ozone hole area in the spring has increased in size, but not as rapidly as during the 1980s. It is not yet possible to say whether the area of the ozone hole has maximized. However, chlorine in the stratosphere has reached nearly constant levels and is expected to start declining, so the ozone hole may have seen its maximum size. Annual variations in temperature will probably be the dominant factor in determining differences in size of the ozone hole in the near future, due to the importance of cold-weather Polar Stratospheric Clouds (PSCs) that act as reactive surfaces to accelerate ozone destruction.

The 2007 hole was fairly average when compared to those of the past 15 years. On September 13, 2007, the hole reached it maximum size of 24 million square kilometers (9.3 million square miles), a full 18% smaller than the 2006 hole. The 2006 hole reached its maximum size of 29 million square kilometers (11.3 million square miles) on September 24, 2006, according to NASA. This is very close to the record ozone hole size of September 10, 2000, uOzone Hole FAQ : Weather Undergroundg m Dating Adult hOzone Hole FAQ : Weather Undergroundi b Free