depletion of ozone composition of atmosphere troposphere 0-12km thick; 75% of all gases in...

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5.6 Depletion of Stratospheric Ozone

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Page 1: Depletion of Ozone Composition of Atmosphere Troposphere 0-12km thick; 75% of all gases in atmosphere; All weather happens here; Temperature falls with

5.6 Depletion of Stratospheric Ozone

Page 2: Depletion of Ozone Composition of Atmosphere Troposphere 0-12km thick; 75% of all gases in atmosphere; All weather happens here; Temperature falls with

Depletion of Ozone

Page 3: Depletion of Ozone Composition of Atmosphere Troposphere 0-12km thick; 75% of all gases in atmosphere; All weather happens here; Temperature falls with

Composition of Atmosphere

Page 4: Depletion of Ozone Composition of Atmosphere Troposphere 0-12km thick; 75% of all gases in atmosphere; All weather happens here; Temperature falls with

Troposphere• 0-12km thick; • 75% of all gases in atmosphere; • All weather happens here; • Temperature falls with altitude

Page 5: Depletion of Ozone Composition of Atmosphere Troposphere 0-12km thick; 75% of all gases in atmosphere; All weather happens here; Temperature falls with

Stratosphere• 12-50 km thick• Temperature increases with altitude (gets warmer!)

• Horizontal winds (jet stream)

• Contains ozone layer

Page 6: Depletion of Ozone Composition of Atmosphere Troposphere 0-12km thick; 75% of all gases in atmosphere; All weather happens here; Temperature falls with

Mesosphere•50-80km thick• temperature falls with altitude •meteor showers happen here

Page 7: Depletion of Ozone Composition of Atmosphere Troposphere 0-12km thick; 75% of all gases in atmosphere; All weather happens here; Temperature falls with

Thermosphere• Aurora borealis and aurora australis

• Ionosphere here (reflects radio waves for communications)

• Very hot (2000 C+) !

Page 8: Depletion of Ozone Composition of Atmosphere Troposphere 0-12km thick; 75% of all gases in atmosphere; All weather happens here; Temperature falls with

Exosphere• Outermost layer of earth’s atmosphere

• 550km+ above earth’s surface• Satellites orbit here

Page 9: Depletion of Ozone Composition of Atmosphere Troposphere 0-12km thick; 75% of all gases in atmosphere; All weather happens here; Temperature falls with

Ozone3 oxygen moleculesUV (ultraviolet)

radiation is absorbed during the formation and destruction of ozone into oxygen (O2)

Page 10: Depletion of Ozone Composition of Atmosphere Troposphere 0-12km thick; 75% of all gases in atmosphere; All weather happens here; Temperature falls with

Ozone and UV light • Allows UVa and UVb through, but blocks

UVc wavesUVa - causes wrinklesUVb - causes skin cancerUVc - worst one because of damage to

organisms/tissues• O2 + O + UV → O3 • The energy provided by incoming UV light

changes O2 → O3

Page 11: Depletion of Ozone Composition of Atmosphere Troposphere 0-12km thick; 75% of all gases in atmosphere; All weather happens here; Temperature falls with

Atmosphere

Page 12: Depletion of Ozone Composition of Atmosphere Troposphere 0-12km thick; 75% of all gases in atmosphere; All weather happens here; Temperature falls with

Ozone and HOGS (Halogenated Organic Gases)

HOG’s are usually stable but break down into halogen atoms (F, Cl, Br, I, At) which are highly reactiveEx. (CFC = chlorofluorocarbon

Cl and F are halogens Organic = contains carbon

Page 13: Depletion of Ozone Composition of Atmosphere Troposphere 0-12km thick; 75% of all gases in atmosphere; All weather happens here; Temperature falls with

HOGS cont.How ozone is depleted by CFC’s:

UV radiation breaks off a chlorine atom from a CFC molecule. The chlorine atom attacks an ozone molecule (O3), breaking it

apart and destroying the ozone. The result is an ordinary oxygen molecule (O2) and a chlorine

monoxide molecule (ClO). The chlorine monoxide molecule (ClO) is attacked by a free

oxygen atom releasing the chlorine atom and forming an ordinary oxygen molecule (O2).

The chlorine atom is now free to attack and destroy another ozone molecule (O3). One chlorine atom can repeat this destructive cycle thousands of times.

sources of HOG’s - fire extinguishers, refrigerators, AC units

Page 14: Depletion of Ozone Composition of Atmosphere Troposphere 0-12km thick; 75% of all gases in atmosphere; All weather happens here; Temperature falls with

UV light and ozone

Page 15: Depletion of Ozone Composition of Atmosphere Troposphere 0-12km thick; 75% of all gases in atmosphere; All weather happens here; Temperature falls with

UV radiation on Life• Reacts with melanin

in skin to cause sunburn & skin cancer

• Overexposure degrades immune system (but how?)

Page 16: Depletion of Ozone Composition of Atmosphere Troposphere 0-12km thick; 75% of all gases in atmosphere; All weather happens here; Temperature falls with

UV radiation and life• Required for production of vitamin D (GOOD!)• Interferes with photosynthesis in producers (esp. phytoplankton)• Zooplankton then gain less energy from phytoplankton, and food chain suffers (i.e. productivity decreases)

Page 17: Depletion of Ozone Composition of Atmosphere Troposphere 0-12km thick; 75% of all gases in atmosphere; All weather happens here; Temperature falls with

Pollution Management of CFC’s and HOGS• Reduce-Regulate-Restore model

Reduce: Replace CFC’s with CO2, propane, or airReplace aerosol propellants Replace methylbromide pesticides with

something other than GHG’sDon’t use aerosol hair products or deodorant

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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

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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

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National and International Policies UNEP (United Nations Environment Program)

forges agreements on: ITIHC (International Trade in Harmful Chemicals) air pollution contamination of international waterways provide information to countries and public on

disadvantages of pollution

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Policies Continued1987 Montreal Protocol

international agreement on the emission of ozone-depleting substances

froze production and consumption of CFC’s with goal of zero production by year 2000

LEDC’s granted a longer time to implement the treaty

China and India have not met their quotas under the MP because of their rapid economic growth and high demand for refrigeration & AC’s

good example of a successful international cooperative effort to alter human impact on the environment

Page 22: Depletion of Ozone Composition of Atmosphere Troposphere 0-12km thick; 75% of all gases in atmosphere; All weather happens here; Temperature falls with

Hair Bands Ruined the Ozone

Poison 1983…so much hairspray