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Environmental Science: Toward a Sustainable Future Richard T. Wright. Chapter 20. The Atmosphere: Climate, Climate Change, and Ozone Depletion PPT by Clark E. Adams. El Niño: What Happened?. Jet streams shifted from normal course Cause unknown. April. May. June. El Niño: What Happened?.
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Environmental Science: Toward a Sustainable FutureRichard T. Wright Chapter 20 The Atmosphere: Climate, Climate Change, and Ozone DepletionPPT by Clark E. Adams
El Niño: What Happened? • Jet streams shifted from normal course • Cause unknown April May June
El Niño: What Happened? • Development of warm water in the eastern Pacific over time • Reversal in trade winds that normally blow from an easterly direction
El Niño: What Happened? • Warm water spread to the east • Global patterns in moisture and evaporation changed = climate shifts
The El Niño Effects: Fig. 20-1 • Landslides on the California coast • Mildest hurricane season in many years • Rain five times normal in an East Africa drought region • Record crop harvests in India, Australia, and Argentina
La Niña: What Happened? • Easterly trade winds reestablished with greater intensity • Upwelling of colder water from ocean depths • Jet streams are weakened • Global patterns in moisture and evaporation return to “normal”
The Atmosphere: Climate, Climate Change, and Ozone Depletion • Atmosphere and weather • Climate • Global climate change • Response to climate change • Depletion of the ozone layer
Atmosphere and Weather • Atmospheric structure • Weather
Weather: Solar Energy Balance Most solar energy absorbed by atmosphere, oceans, and land
Tornadoes • Cold low-pressure air mass collides with a warm high-pressure air mass http://www.photolib.noaa.gov/nssl/nssl0065.htm
Fujita Scale Measures the Intensity of Tornadoes • F-0: 40–72 mph, chimney damage, tree branches broken • F-1: 73–112 mph, mobile homes pushed off foundations or overturned • F-2: 113–157 mph, considerable damage, mobile homes demolished, trees uprooted
Fujita Scale Measures the Intensity of Tornadoes • F-3: 158–205 mph, roofs and walls torn down, trains overturned, cars thrown • F-4: 207–260 mph, well-constructed walls leveled • F-5: 261–318 mph, homes lifted off foundation and carried considerable distances, autos thrown as far as 100 meters
Climate • Ocean and atmosphere • Climates in the past
Climate • Defined as the average trend in temperature and rainfall that produces a unique assemblage of plants and animals • On the next slide identify climates A to E, e.g., low average rainfall and high average temperature = hot desert
High A D C Temperature B E Low High Identify Climates A to E Precipitation
Ocean and Atmosphere • Covers 75% of the Earth’s surface • Major source of water to hydrologic cycle • Major source of heat to atmosphere • Stores and conveys heat
The Ocean Conveyor System • Thermohaline circulation: effects that temperature and salinity have on density of water • Conveyor system moves water masses from the surface to deep oceans and back again • Cool northern waters more dense and sink to depths of 4,000 m = North Atlantic Deep Water (NADW)
The Ocean Conveyor System • Deep water spreads southward to south Africa and joined by cold Antarctic waters • Spread northward into Indian and Pacific oceans as deep currents • Current slows down, warms up, becomes less dense, rises to the surface, and moves back to North Atlantic • Produces a warm climate in Europe
The Ocean Conveyor System • Factors that could alter the conveyor system • Appearance of unusually large quantities of freshwater – melting icebergs • Global warming
Global Climate Change • The Earth as a greenhouse • The greenhouse gases • Evidence of climate change
Factors Affecting Global Temperatures • Cloud cover: cooling • Changes in Sun’s intensity: cooling or warming • Volcanic activity: cooling • Sulfate aerosols: cooling
Greenhouse Gases: CO2 Emissions from Fossil Fuel Burning • 35% higher than before industrial revolution • Oceans = CO2 sink • Forests = CO2 source • 24 billion metric tons CO2 added each year
Water vapor Methane Nitrous oxide CFCs and other halocarbons Hydrologic cycle Animal husbandry Chemical fertilizers* Refrigerants* Other Greenhouse Gases and Sources * = Long residence times and contribute to ozone depletion
Impacts of Global Warming • Melting of polar ice caps • Flooding of coastal areas • Massive migrations of people inland
Impacts of Global Warming • Alteration of rainfall patterns • Deserts becoming farmland and farmland becoming deserts • Significant losses in crop yields
Evidences of Climatic Change • 17 of the hottest years on record have occurred since 1980 (Fig. 20-5) • Wide-scale recession of glaciers • Sea level rising Predicted mean global temperature change by 2100 is between 1.5 and 4.5oC
Reducing CO2 Emissions (True or False) • Reducing use of fossil fuels • Adopt a wait-and-see attitude • Develop alternative energy sources • Plant trees • Examine other possible causes of global warming
Reducing CO2 Emissions (True or False) • Make and enforce energy conservation rules • Rely on the government • Adopt the precautionary principle • Raise the minimum driving age to 18 years
Key Findings of the 2000 U.S. Climate Change Assessment (Table 20-3) • Increased warming • Differing regional impacts • Vulnerable ecosystems • Widespread water concerns • Agriculture largely unaffected • Forest growth to increase • Coastlines – rising sea levels
Responses to Climate Change • Response 1: mitigation = reduce CO2 emissions • Response 2: adaptation = accepting and learning to live with the consequences of climate change
Framework Convention on Climate Change (FCC) • Relied on voluntary approach to reduce CO2 emissions • Developing countries continue toward developed nation status using fossil fuels
Framework Convention on Climate Change (FCC) • To achieve a 7% reduction by 2010 requires a 25% reduction of present use • By 2010 CO2 emissions will have increased by 30%
Framework Convention on Climate Change (FCC) • Bottom line: need 60% reduction (144 ppm) in CO2 emission worldwide NOW to stabilize greenhouse gas concentrations at today’s levels
Depletion of Ozone Layer • Radiation and importance of the shield • Formation and breakdown of the shield • Coming to grips with ozone depletion
Good Ozone! Bad Ozone!
Radiation and Importance of the Shield • Skin cancer (700,000 new cases each year) • Premature skin aging • Eye damage • Cataracts • Blindness
Reaction #1: UV light + O2 O + O Reaction #2: Free O + O2 O3 Reaction #3: Free O + O3 O2 + O2 O + O2 Reaction #4: UV light + O3 Formation of the Ozone Shield
Chlorofluorocarbons (CFCs) • Organic molecules in which both chlorine and fluorine atoms replace some of the hydrogen atoms • Sources: • refrigerators and air conditioners • production of plastic foam • cleaner for electronic parts • pressurizing agent in aerosol cans