1 / 28

6.2 Stratospheric Ozone

6.2 Stratospheric Ozone. Atmosphere. Stratosphere. 12-50 km thick Temperature increases with altitude (gets warmer!) Horizontal winds ( jet stream ) Contains ozone layer. Ozone. 3 oxygen molecules. Ozone – O 3. Dynamic equilibria Balance between two ongoing processes

lindquist
Télécharger la présentation

6.2 Stratospheric Ozone

An Image/Link below is provided (as is) to download presentation Download Policy: Content on the Website is provided to you AS IS for your information and personal use and may not be sold / licensed / shared on other websites without getting consent from its author. Content is provided to you AS IS for your information and personal use only. Download presentation by click this link. While downloading, if for some reason you are not able to download a presentation, the publisher may have deleted the file from their server. During download, if you can't get a presentation, the file might be deleted by the publisher.

E N D

Presentation Transcript


  1. 6.2 Stratospheric Ozone

  2. Atmosphere

  3. Stratosphere • 12-50 km thick • Temperature increases with altitude (gets warmer!) • Horizontal winds (jet stream) • Contains ozone layer

  4. Ozone • 3 oxygen molecules

  5. Ozone – O3 • Dynamic equilibria • Balance between two ongoing processes • UV radiation passing through the Earth’s upper atmosphere is absorbed by the formation and destruction of ozone.

  6. Ozone • UV (ultraviolet) radiation is absorbed during the formation and destruction of ozone into oxygen (O2)

  7. Ozone and UV light • Allows UVa and UVb through, but blocks UVc waves • UVa - causes wrinkles • UVb - causes skin cancer • UVc - worst one because of damage to organisms/tissues

  8. UV radiation also affects other living organisms • Damage to photosynthetic organisms. • Especially phytoplankton – basis of many aquatic food webs.

  9. Beneficial Effects of UV • In animals stimulates the production of Vit D. • Treat psoriasis and vitiligo (skin diseases) • Steriliser, water purifier • Forensics, lighting, lasers

  10. Damage to the Ozone

  11. CFCs are usually very stable. However, in the high stratosphere the UV radiation breaks them down releasing free chlorine atoms (chlorine is very reactive)

  12. HOGS (Halogenated Organic Gases) • HOG’s are usually stable but break down into halogen atoms (F, Cl, Br, I, At) which are highly reactive • Ex. (CFC = chlorofluorocarbon • Cl and F are halogens • Organic = contains carbon

  13. Depletion of Ozone

  14. Damage to the ozone ODS (Ozone-depleting substance)

  15. Sources of CFC’s • fire extinguishers, refrigerators, AC units

  16. Sources of CFC’s • fire extinguishers, refrigerators, AC units

  17. Pollution Management Strategies

  18. Reducing ODS • Apply the “Replace, regulate and restore” model of pollution management to ODS.

  19. Pollution Management of CFC’s and HOGS • Reduce-Regulate-Restore model • Reduce: • Replace CFC’s with CO2, propane, or air • Replace aerosol propellants • Replace methylbromide pesticides with something other than GHG’s • Don’t use aerosol hair products or deodorant

  20. Pollution Management of CFC’s and HOGS • Regulate: • Require a switch to HCFC’s because they don’t persist as long in the atmosphere; • (They are still harmful to the ozone layer…just less so) • Create laws to require refrigerators returned to manufacturers to recover harmful materials inside • Capture CFC’s from scrap cars AC units

  21. Pollution Management of CFC’s and HOGS • Restore: • Remove chlorine from the stratosphere or add ozone (not exactly feasible!) • Ozone layer is slowly replenishing itself as long as we continue the ban

  22. National and International Organizations

  23. National and International Organizations • UNEP (United Nations Environmental Programme) • Montreal Protocol 1987

  24. National and International Organizations • UNEP (United Nations Environmental Programme) • Key role in: • Providing information • Creating and evaluating international agreements • Protection of stratospheric ozone

  25. National and International Organizations • Montreal Protocol 1987 • International agreements on the reduction of ODS use. • National laws and regulations aimed at reducing consumption of ODS (CFCs in particular)

  26. The Montreal Protocol 1987 • This protocol is very significant for a number of reasons: • Best example of international cooperation on an environmental issue. • An example of the precautionary principle in science-based decision making. • Experts from many different fields coming together to research a problem and find solutions. • The first to recognise that different countries could phase-out ODS chemicals at different times depending on their economic status. • The first with regulations that were carefully monitored. Precautionary principle - in environmental matters, the theory that if the effects of a product or action are unknown, then the product should not be used or the action should not be taken

  27. Hair Bands Ruined the Ozone Poison 1983… so much hairspray

More Related