Ozone layer formation and deplation animation ppt

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OZONE DEPLATION •Ozone is a triatomic form of oxygen (O3) found in Earth’s upper and lower atmosphere. •It is unstable gas, only few cm thick . •If the rate of breakdown is faster then the rate of formation then the ozone layer thins •This could develop into Ozone hole. •An ozone hole was first observed over he Antarctic in 1985

Transcript of Ozone layer formation and deplation animation ppt

Page 1: Ozone layer formation and deplation animation ppt

OZONE DEPLATION

•Ozone is a triatomic form of oxygen (O3) found in Earth’s upper and lower atmosphere. •It is unstable gas, only few cm thick .•If the rate of breakdown is faster then the rate of formation then the ozone layer thins•This could develop into Ozone hole. •An ozone hole was first observed over he Antarctic in 1985

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Evolution of the Ozone Layer

Early planet history:– no ozone present

– UV light directly hit planet’s surface

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Oxygen in the Atmosphere

+O2

O

O

+

O +O2 O3 (ozone)

Evolution of the Ozone Layer

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UV O3 (ozone)

O +O2

O +O3 (ozone) O2 O2+

O + O2O3 (ozone)

+

heat

+

Evolution of the Ozone Layer

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Depletion of Ozone Layer

•The ozone layer is being destroyed by CFCs and other substances.• The mechanisms Responsible for Ozone depletion

1)Meteorological mechanism 2)Chemical mechanism

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Original Research1974: Rowland and Molina

+

SUN

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Cl FreeRadicals O3 (ozone) O2ClO

+

ClO+

O Cl- “free radical”

+O2

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Dynamic Equilibrium

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A combination of low temperatures and elevated chlorine and bromine concentrations are responsible for the destruction of ozone in the upper stratosphere thus forming a “hole”. (Kerr, 1987)

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Location of Ozone Losses

Ozone loss extends beyond Antarctica and Arctic Polar regions

Ozone loss over US currently 5% below normal rates

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Current Rate of Ozone Depletion

• Decrease in rate of ozone depletion (since 1997)• Slowing of buildup of harmful Cl- from CFCs• Ozone hole is still growing.• Ozone layer recovery expected by 2050

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Images of Antarctica Taken Indicate A Slow Recovery

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Too much ultra-violet light can result in:• Skin cancer• Eye damage such as cataracts• Immune system damage• Damage to the DNA in various life-forms – this has been as observed  in Antarctic ice-fish that lack

pigments to shield them from the ultra-violet light (they've never needed them before)

• UV radiation can alter both the time of flowering as well as the number of flowers in certain species.

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What Is Being Done to Counter the Effects of Ozone Depletion?

• Montreal Protocol (adopted in 1987) – panel of experts was formed to investigate substances responsible for Ozone hole formation

– Established policies that prevent future use of certain types of chemicals

– Stipulated that the production and consumption of compounds contributing towards depletion of ozone in the stratosphere were to be phased out by the year 2000 (2005 for methylchloroform)

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The Environmental Protection Agency (EPA)

• Responsible for enforcing the Montreal Protocol within the U.S.– The EPA has several programs in place;• Regulating and enforcing on-road car and truck air-

conditioning systems

• Regulating most air-conditioning and refrigeration appliances

• Technician certification

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Efforts Need to Be Continued• Create reliable models– To gain a better understanding of the effects ozone

depletion has on organisms living within different ecosystems

• Enforcement of Montreal Protocol– To reduce concentrations of chemicals responsible for

ozone depletion

• Monitoring chemicals being emitted

• Gain a better overall understanding on just how ozone depletion is affecting our planet

...