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The Ozone Layer

By: Desiree Collins. The Ozone Layer. History of the Ozone Discovery. Dramatic loss of ozone in the lower stratosphere over Antarctica was first noticed in the 1970s by a research group from the British Antarctic Survey were monitoring the atmosphere above Antarctica.

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The Ozone Layer

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  1. By: Desiree Collins The Ozone Layer

  2. History of the Ozone Discovery • Dramatic loss of ozone in the lower stratosphere over Antarctica was first noticed in the 1970s by a research group from the British Antarctic Survey were monitoring the atmosphere above Antarctica.

  3. What is the ozone hole? • News media confuses it with the problem of global warming • Ozone contributes to the greenhouse effect • Over Antarctica (and the Arctic), stratospheric ozone depleted over past 15 years at certain times of the year • Hole presently size Antarctica, 10km altitude - lower stratosphere

  4. What is ozone? • Ozone forms a layer in the stratosphere, thinnest in the tropics (around the equator) and denser towards the poles

  5. How is ozone formed? • UV radiation strikes the O2 molecule and splits it, atomic oxygen associates itself with another O2 molecule .

  6. Hole Formation Based on Two different mechanisms: • Meteorological mechanism • Movement of air from one place to another in the upper stratosphere • Cold temperature in the upper atmosphere causes nitric acid to freeze into crystals forming wispy pink clouds • Forms a vortex of tightly twisted winds thus forming a hole in the upper atmosphere

  7. Chemical Mechanism • Different chemicals are responsible for the destruction of the ozone layer • Topping the list : • chlorofluorocarbons (CFC’s) • man-made, non-toxic and inert in the troposphere • In the stratosphere are photolysed, releasing reactive chlorine atoms that catalytically destroy ozone

  8. UV light & DNA • UV-B has a direct effect on DNA • DNA absorbs UV light of 260nm • The action of UV forms thymine dimers • This can cause a gene mutation when the DNA replicates

  9. Specific damage by UV light • Sunburn • Clouding of the cornea and formation of cataract • Skin cancer (melanoma) • Reduced rates of photosynthesis

  10. What are CFCs? • Used as propellants in aerosol spray cans • Used as refrigerants in fridges, freezers and air conditioning units

  11. What can be done? • Reduce the use of CFCs • They are already banned in aerosols (1987) • BUT they are still used as refrigerants • Recycle fridges and air conditioning plants

  12. The current situation • The holes developing over the pole suggest that they may be show an improvement • BUT CFC molecules take 30 years to rise up to the stratosphere • The chlorine radicals last a long time • The peak ozone damage was supposed to be in 2000 • Damage could go on another 50 years

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