6.2 Stratospheric ozone

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7 Terms

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Ozone

molecules that protect the Earth from harsh UV rays. They are mainly found in the strartosphere

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Ozone thickness

  • Thicker in the spring / thinner in the summer

  • Thinner in the equator / thicker near the poles

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Ozone's dynamic equilibrium

The UV rays from the sun causes the ozone molecules to break apart in order to absorb the UV rays. However, they later reform under normal conditions.

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Halogen atoms

cause chemical depletion of stratospheric ozone over the globe by slowing down the rate of ozone production

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CFCs

Destroys the straspheric ozone layer

Ex: Chlorofluorocarbons (CFCs or freons) - propellants in spray cans, foam, refrigerants

  • Hydrochlorofluorocarbons (HCFCs) - replacements for CFCs

  • Halon - fire extinguishers

  • Methyl bromide - pesticides

  • Nitrogen oxides - bacterial breakdown of nitrites and nitrates in the soil, supersonic aircraft

  • Carbon tetrachloride - cleaning substance

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Effects of UV rays

  • Increase in mutation rates in DNA causing cancer

  • Can cause eye cataracts

  • Can damage the ability to carry out photosynthesis in plants and phytoplankton

  • Reduces primary production and therefore total productivity

  • Damage to immune system

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Solutions to helping ozone

  • recycling refrigerants

  • developing alternatives to gas-blown plastics, halogenated pesticides, propellants and aerosols

  • developing non-propellant alternatives.