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Chapter 13 Atmospheric Science and Air Pollution

Chapter 13 Atmospheric Science and Air Pollution. This lecture will help you understand:. Earth ’ s atmosphere Weather, climate, and atmospheric conditions Outdoor pollution and solutions Stratospheric ozone depletion Acidic deposition and consequences

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Chapter 13 Atmospheric Science and Air Pollution

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  1. Chapter 13 Atmospheric Science and Air Pollution

  2. This lecture will help you understand: Earth’s atmosphere Weather, climate, and atmospheric conditions Outdoor pollution and solutions Stratospheric ozone depletion Acidic deposition and consequences Indoor air pollution and solutions

  3. Central Case Study: L.A. and Its Sister City, Tehran, Struggle for a Breath of Clean Air Vehicles caused smog in Los Angeles from 1970s to 1990s Policies and technologies improved its air qualities But its “sister cities”are not as clean Tehran, Iran, is very polluted Old cars use cheap gas Topography, immigration, etc., make things worse Air pollution kills 3,600/month in Tehran

  4. Section 1 The Structure and Components of the Atmosphere

  5. The atmosphere Atmosphere: the thin layer of gases around Earth Provides oxygen Absorbs radiation and moderates climate Transports and recycles water and nutrients 78% N2, 21% O2 Over history, the atmosphere has changed Human activity is now changing the amount of some gases CO2, methane (CH4), ozone (O3)

  6. The atmosphere’s composition

  7. The first layer of the atmosphere Earth’s four atmospheric layers have different Temperatures Densities Composition Troposphere: bottommost layer (11 km [7 miles]) Responsible for Earth’s weather The air gets colder with altitude Tropopause: the boundary that limits mixing between the troposphere and stratosphere

  8. The 3 higher levels of the atmosphere Stratosphere: 11–50 km (7–31 mi) above sea level Drier and less dense, with little vertical mixing Gets warmer with altitude Ozone layer: blocks UV radiation Mesosphere: low air pressure Gets colder with altitude Thermosphere: top layer

  9. Solar energy causes air to circulate An enormous amount of energy from the sun hits Earth 70% is absorbed by water, evaporating the water Air near Earth’s surface is warm and moist Convective circulation: less dense, warmer air rises Creating vertical currents Rising air expands and cools Cool air descends and becomes denser Replacing rising warm air Convection influences weather and climate

  10. The atmosphere drives weather and climate Weather and climate involve physical properties of the troposphere Temperature, pressure, humidity, cloudiness, wind Weather:atmospheric conditions within small geographic areas,over short time periods (hours, days) Climate:patterns of atmospheric conditions across large geographic regions over long periods of time Mark Twain said, “Climate is what we expect; weather is what we get”

  11. Circulation systems produce climate patterns Convective currents contribute to climatic patterns Hadley cells:convective cells near the equator Surface air warms, rises, and expands Causing heavy rainfall near the equator Giving rise to tropical rainforests Currents heading north and south are dry Giving rise to deserts at 30 degrees Ferrel cells andpolar cells: lift air and create precipitation at 60 degrees latitude north and south Conditions at the poles are dry

  12. Global wind patterns Atmospheric cells interact with Earth’s rotation to produce global wind patterns As Earth rotates, equatorial regions spin faster Some areas of the planet’s surface move more quickly than other areas Coriolis effect: the apparent north–south deflection of air currents of the convective cells Results in curving global wind patterns Global wind patterns helped ocean travel by wind-powered sailing ships

  13. Climate patterns and moisture distribution

  14. Storms pose hazards • Atmospheric conditions can produce dangerous storms • Hurricanes (typhoons, cyclones): form when winds rush into areas of low pressure • Warm, moist air over the topical oceans rises • Drawing up huge amounts of water vapor • Which falls as heavy rains • Tornadoes: form when warm air meets cold air • Quickly rising warm air forms a powerful convective current (spinning funnel)

  15. We need to understand the atmosphere • Understanding how the atmosphere works helps us to: • Predict violent storms and protect people • Comprehend how pollution affects climate, ecosystems, economies, and human health

  16. Section 2 Temperature Inversions and Air Quality

  17. Thermal (temperature) inversion Thermal inversion: a layer of cool air forms beneath warm air Inversion layer: the band of air where temperature rises with altitude Dense, cool air at the bottom of the layer resists mixing Inversions trap pollutants in cities surrounded by mountains • Tropospheric air temperature decreases with height • Warm air rises, causing vertical mixing

  18. Temperature Inversions • Trap air pollutants such as smog • Can cause freezing rain • Will result in poor air quality and Ozone Alert Days • http://www.airnow.gov

  19. Section 3 Atmospheric Pollutants

  20. Outdoor air pollution Air pollutants: gases and particulate material added to the atmosphere Can affect climate or harm people or other organisms Air pollution: the release of pollutants Outdoor (ambient) air pollution: pollution outside Has recently decreased due to government policy and improved technologies in developed countries Developing countries and urban areas still have significant problems Greenhouse gas emissions may be our worst problem

  21. Natural sources can pollute Humans make impacts worse Farming, grazing cause erosion, desertification Fire suppression leads to worse fires(dead trees,etc build up on forest floor) • Fires generate soot and gases • Winds send huge amounts of dust aloft • Even across oceans • Volcanoes release particulate matter, sulfur dioxide

  22. We create outdoor air pollution Humans generate many types of air pollution Point sources: specific spots where large quantities of pollutants are discharged (power plants) Non-point sources: more diffuse, consisting of many small, widely spread sources (automobiles) Primary pollutants: directly harmful or can react to form harmful substances (soot and carbon monoxide) Secondary pollutants: form when primary pollutants react with constituents of the atmosphere

  23. Pollutants exert local and global effects • Residence time: the time a pollutant stays in the atmosphere • Pollutants with brief residence times exert localized impacts over short time periods • Particulate matter, automobile exhaust • Pollutants with long residence times exert regional or global impacts • Greenhouse gases • Ozone destroyers

  24. Legislation addresses pollution The Clean Air Act (1963, amended in 1970, 1990) Funds research for pollution control Sets standards for air quality, limits on emissions Allows citizens to sue parties violating the standards Introduced a cap-and-trade program for sulfur dioxide The EPA sets standards for emissions and pollutants States monitor air quality They develop, implement, and enforce regulations They submit plans to the EPA for approval The EPA takes over enforcement if plans are inadequate

  25. Wrap UP: • What is a temperature inversion? • How can this affect air quality? • Why do the pollutants stay trapped and close to the ground during an inversion? • What is the difference between a point and non-point pollutant? • Give an example of an air pollutant with a short residence time? • Does the residence time affect how we monitor the pollutant?

  26. Section 5 Criteria Pollutants

  27. Criteria pollutants: carbon monoxide Criteria pollutants: especially great threats to humans Carbon monoxide, sulfur dioxide, nitrogen dioxide, tropospheric ozone, particulate matter, lead 127 million Americans live in areas that violate standards for at least one criteria pollutant Carbon monoxide(CO): colorless, odorless gas Produced primarily by incomplete combustion of fuel From vehicles and engines, industry, waste combustion, residential wood burning Prevents blood hemoglobin from binding with oxygen

  28. Criteria pollutants: SO2 and NOx Sulfur dioxide (SO2): colorless gas with a strong odor Coal emissions from electricity generation, industry Can form acid deposition Nitrogen dioxide (NO2):foul-smelling red-brown gas Contributes to smog and acid deposition Nitrogen oxides (NOx): formed when nitrogen and oxygen react at high temperatures in engines Vehicles, electrical utilities, industrial combustion

  29. Criteria pollutants: tropospheric ozone Tropospheric ozone (O3): a colorless gas A secondary pollutant created from sunlight, heat, nitrogen oxides, volatile carbon-containing chemicals A major component of smog Participates in reactions that harm tissues and cause respiratory problems The pollutant that most frequently exceeds EPA standards

  30. Criteria pollutants: particulate matter andlead Particulate matter: suspended solid or liquid particles Damages respiratory tissue when inhaled Primary pollutants: dust and soot Secondary pollutants: sulfates and nitrates From dust and combustion processes Lead: in gasoline and industrial metal smelting Bioaccumulates and damages the nervous system Banned in gasoline in developed, but not in developing, countries

  31. Agencies monitor emissions State and local agencies monitor and report to the EPA emissions of: Carbon monoxide, sulfur dioxide, particulate matter, lead, and all nitrogen oxides Tropospheric ozone, a secondary pollutant, has no emissions to monitor Agencies monitor volatile organic compounds (VOCs): Emitted by engines and industrial processes VOCs can react to produce ozone

  32. U.S. air pollution In 2008, the U.S. emitted 123 million tons of the six monitored pollutants

  33. We have reduced U.S. air pollution Total emissions of the six monitored pollutants have declined 60% since the Clean Air Act of 1970 Despite increased population, energy consumption, miles traveled, and gross domestic product

  34. We have reduced emissions Federal policies and technology Cleaner-burning engines and catalytic converters Reduced SO2 emissions Permit trading programs and clean coal technologies Scrubbers: chemically convert or physically remove pollutants before they leave smokestacks Phaseout of leaded gasoline

  35. We still have more to do… • The reduction in outdoor air pollution since 1970 is one of our greatest accomplishments! • Saving the lives of 200,000 Americans since 1970 • There is room for improvement: • Concerns over new pollutants and greenhouse gas emissions • U.S. carbon dioxide emissions increased 44% (1970–2008) • The Supreme Court ruled that the EPA could regulate carbon dioxide as a pollutant • There is formidable political opposition to this

  36. Toxic substances pose health risks Toxic air pollutants: substances that cause … Cancer, reproductive defects, or neurological, immune system, developmental, or respiratory problems The EPA regulates 188 toxic air pollutants Including mercury, VOCs, methylene chloride Toxic air pollutants cause 36 cancer cases per 1 million people Clean Air Act regulations helped reduce emissions by more than 35% since 1990

  37. Industrializing nations suffer increasing pollution Outdoor pollution is getting worse in developing nations Polluting factories and power plants, increasing numbers of cars Emphasize economic growth, not pollution control People burn traditional fuels (wood and charcoal) China has the world’s worst air pollution Coal burning, more cars, power plants, factories Causing over 300,000 premature deaths/year China is reducing pollution (closing factories, cleaner fuels, raising efficiency standards, cleaner energy, etc.)

  38. Pollution in developing nations is high In Tehran, vehicles emit 5,000 tons of pollutants each day!

  39. Section 6 Smog

  40. Smog: our most common air quality problem Smog: an unhealthy mixture of air pollutants over urban areas Industrial smog: burning coal or oil releases CO2, CO, soot, mercury, sulfur Sulfuric acid is formed Regulations in developed countries reduced smog Coal-burning industrializing countries faces health risks Due to lax pollution control Smog in Donora, PA, killed 21 people and sickened 6,000

  41. Photochemical (brown air) smog Sunlight drives a chemical reactions between primary pollutants and atmospheric compounds Forming ozone, NO2, and many other compounds Appears as a brownish haze Formed in hot, sunny cities surrounded by mountains Morning traffic releases NO and VOCs Irritates eyes, noses, and throats In 1996, photochemical smog killed 300 and sickened 400,000 in 5 days

  42. Creation of smog Industrial smog Photochemical smog

  43. We can reduce smog But…increased population and cars can wipe out advances • Pollution control technology • Vehicle inspection programs • Financial incentives to replace aging vehicles • Restricting driving • Cleaner burning fuels • Cleaner industrial facilities • Close those that can’t improve • Pollution indicator boards

  44. Wrap up: • Which compound is the primary component of photochemical smog? • How does smog form? • How can we reduce this type of air pollution? • Why are some areas, such as Mexico City, more susceptible to smog?

  45. Section 7 Stratospheric OZONE

  46. Do Now: 1. Which color represents 2013? 2.How does 2013 compare with the last 10 years? 3.When is the Ozone hole the biggest? 4. Why isn’t January to June on the chart?

  47. Taken with the OMI instrument on the AURA Satellite How does the ozone hole change?

  48. Synthetic chemicals deplete stratospheric ozone Ozone in the lower stratosphere absorbs the sun’s ultraviolet (UV) radiation UV radiation can damage tissues and DNA Ozone-depleting substances(ODS): human-made chemicals that destroy ozone Halocarbons: human-made compounds made from hydrocarbons with added chlorine, bromine, or fluorine Chlorofluorocarbons (CFCs): halocarbons used as refrigerants, in fire extinguishers, in aerosol cans, etc. They stay in the stratosphere for a century

  49. CFCs destroy ozone One chlorine atom can destroy 100,000 ozone molecules Sunlight releases chlorine atoms that split ozone Ozone hole: decreased ozone levels over Antarctica Discovered in 1985 Measured in Dobson Units

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