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Published byAbel Haynes Modified over 9 years ago
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Ozone Depletion in the Stratosphere The other story Ch. 19
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APES Everything away except a writing utensil
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Altitude (kilometers) Ozone concentration (ppm) Altitude (miles) Stratospheric ozone Stratosphere Troposphere 40 35 30 25 20 15 10 5 0 05 1520 0 5 10 15 20 25 Photochemical ozone Beneficial Ozone Harmful Ozone *
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What does the ozone layer do? Protects Earth from dangerous UV
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What does the ozone layer do? Protects Earth from dangerous UV – Cause mutations Higher rate skin cancer, cataracts, and immune system problems – Essential for life: affect plants & marine ecosystems in unknown ways – Prevents tropospheric ozone Stratospheric Ozone Absorbs: ALL UV-C radiation (most energetic – most lethal) MOST UV-B radiation, but NO UV-A radiation
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Consequence: Increase UV (UVB) reaching Earth’s surface Human – Sunburn – Skin Cancer – Cataracts – Efficiency in immune system Ecosystem – Reducing of primary productivity in oceans – Disrupt food chains – Damage fish/amphibians/mammal s – Widespread effects on major food crops – Decrease plant productivity – Impair/destroy phytoplankton
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Class of Chemicals Primarily Responsible for Thinning of Stratospheric Ozone Layer
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Chlorofluorocarbons (CFCs) – Coolant/refrigerant/air conditioner – Aerosol or propellant – Foam-blowing plastics/insulation (styrofoam) – Solvent/Cleaners Halocarbons – Fire retardants (fire extinguishers) – Soil fumigant/pesticide – Solvents – Foam blowing insulation
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Class of Chemicals Primarily Responsible for Thinning of Stratospheric Ozone Layer Chlorofluorocarbons (CFCs) – AKA Freons – Wonder Chemical – Inexpensive – Stable in troposphere Chemically unreactive odorless nonflamable nontoxic, non corrosive
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Class of Chemicals Primarily Responsible for Thinning of Stratospheric Ozone Layer Others – Hydrobromoflurocarbons (HBFCs) Fire extinguishers – Methyl bromide fumigant – Hydrogen chloride Emitted by space shuttles – Carbon tetrachloride, methyl chloroform, n- propyl bromide, hexachlorobutadiene Cleaning solvents
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HOW do CFCs Break Down Ozone?* 1.CFCs & others released into troposphere 2.CFCs move/drift upward into stratosphere 3.UV radiation breaks apart CFCs releasing Chlorine (bromine/fluorine) 4.Sunlight causes chemical reaction allowing Cl to attack O 3 creating O 2 THUS reducing O 3 levels
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HOW do CFCs Break Down Ozone?* CCl 3 F+UV Cl+CCl 2 F Cl + O 3 ClO + O 2 ClO + O CL + O 2
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Sun Once free, the chlorine atom is off to attack another ozone molecule and begin the cycle again. A free oxygen atom pulls the oxygen atom off the chlorine monoxide molecule to form O2. The chlorine atom and the oxygen atom join to form a chlorine monoxide molecule (ClO). UV radiation Cl C F The chlorine atom attacks an ozone (O 3 ) molecule, pulling an oxygen atom off it and leaving an oxygen molecule (O 2 ). Cl O O O O O O O O O Ultraviolet light hits a chlorofluorocarbon (CFC) molecule, such as CFCl 3, breaking off a chlorine atom and leaving CFCl 2. O CLICK ME!
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How Do We Know This is Happening? Predicted by Mario Molina & Sherwood Rowland
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How Do We Know This is Happening? James Lovelock predicted haze came from human sources Presented at conference with meteorologists & chemists
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Original Hypothesis
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Nitrogen Dioxide Neutralizes Some Chlorine Still Significant (though lower) levels of ozone depletion
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Hypothesis Changes
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Seasonal Thinning of Ozone at the Poles During four months of each year up to half of the ozone in the stratosphere over Antarctica and a smaller amount over the Artic is depleted.
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Seasonal Thinning of Ozone at the Poles Polar stratospheric clouds - high-altitude clouds of ice particles in ozone layer Ice particles provide solid surface for reactions
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Seasonal Thinning at the Poles Ozone thinning (hole) Polar vortex
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Seasonal Thinning of Ozone at the Poles
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Final Hypothesis
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Additional Evidence Airplane flew through ozone hole
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Ozone Depletion Occurs Worldwide
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Montreal Protocol 1987 36 nations 50% reduction in CFC (not others) production by 1998 Phase out CFCs in developed countries by 1996 Phase out use of CFCs in developing countries by 2005
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Copenhagen Protocol Montreal Protocol Amendment 1992 93 countries Accelerated phase out – by 1996 PREVENTION!!
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International Cooperation Reach 1980 levels by 2068 1950 levels by 2108
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Ozone Depletion Projected worse over Antarctic and Arctic between 2010 & 2019
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Need Help? Good Ozone Link
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Characteristics of Global Warming and Ozone Depletion Global Warming CO 2, CH 4, NO x (greenhouse gases) Absorbs infrared (IR) radiation Raising the earth’s surface temperature Decrease burning of fossil fuels Ozone Depletion O 3, O 2, and CFCs Absorbs ultraviolet (UV) radiation Decreasing O 3 concentration in the stratosphere Eliminate CFCs
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