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ENVIRONMENTAL SCIENCE 13e
CHAPTER 15:
Air Pollution,
Climate Change,
and Ozone Depletion
Fig. 15-1, p. 368
Asian Brown Cloud
• http://www.youtube.com/watch?v=qY
YK-2sDN4U
• http://www.youtube.com/watch?v=vSEJfpQLSI&NR=1&feature=fvwp
Core Case Study: South Asia’s
Massive Brown Cloud (1)
• Asian Brown Cloud
• India to Bangladesh to China’s Pacific
coast
• Pollutants from fires, cars, industry
• Skies permanently gray or brown
Core Case Study: South Asia’s
Massive Brown Cloud (2)
• Changing weather patterns
• 700,000 premature deaths per year
• Has traveled to the west coast of the
U.S.
• Made worse by global warming
15-1 What is the Nature of the
Atmosphere?
• Concept 15-1 The two innermost
layers of the atmosphere are the
troposphere, which supports life, and
the stratosphere, which contains the
protective ozone layer.
Earth’s Atmosphere
• Troposphere
– Extends upward 5-11 miles above
earth’s surface
– Makes up 75–80% earth’s air mass
– 78% N2, 21% O2
– Weather and climate
• Stratosphere
• Ozone layer
Stratosphere
• Stratosphere
– Extends from 11-30 miles above Earth’s
surface
– Volume of water vapor less than Troposphere
– Concentration of ozone much higher
• Ozone Layer
– Global sunscreen, keeps 95% of harmful UV
radiation from reaching Earth’s surface
Atmospheric pressure (millibars)
0
120
200
400
600
800
1,000
75
Temperature
110
65
100
Thermosphere
55
Mesopause
80
Mesosphere
70
60
Stratopause
45
35
50
Stratosphere
40
25
Tropopause
30
Ozone layer
20
Troposphere
10 Pressure
(Sea 0
–80
Level)
Altitude (miles)
Altitude (kilometers)
90
–40
0
40
80
Temperature (°C)
120
15
5
Pressure =
1,000
Millibars at
ground level
Fig. 15-2, p. 370
15-2 What Are the Major Air
Pollution Problems? (1)
• Concept 15-2A Three major outdoor
air pollution problems are industrial
smog from burning coal,
photochemical smog from motor
vehicle and industrial emissions, and
acid deposition from coal burning and
motor vehicle exhaust.
15-2 What Are the Major Air
Pollution Problems? (2)
• Concept 15-2B The most
threatening indoor air pollutants
are smoke and soot from wood and
coal fires (mostly in developing
countries) and chemicals used in
building materials and products.
Air pollution
• http://www.youtube.com/watch?v=Hx
_yWFQvJT4&feature=related
Outdoor Air Pollution
• What is air pollution?
– Presence of chemicals in atmosphere in
concentrations that are high enough to be harmful
– Stationary and mobile sources
• Primary pollutants-harmful chemicals
emitted directly into the air
• Secondary pollutants- formed when
primary pollutants react with one another and with
other components of air to form new harmful
chemicals
Types of Major Air Pollutants
• Carbon oxides (CO, CO2)
• Nitrogen oxides and nitric acid
(NO, NO2, HNO3)
• Sulfur dioxide and sulfuric acid
(SO2, H2SO4)
• Particulates (SPM)
• Ozone (O3)
• Volatile organic compounds (VOCs)
Carbon Oxides
Carbon monoxide (CO) colorless, odorless
and highly toxic gas that forms during
incomplete combustion of carbon-containing
materials
– Major sources: motor vehicle exhaust,
burning of forests and grasslands, tobacco
smoke, open fires/inefficient stoves for
cooking
– Reacts with Hb in RBCs to decrease ability
of blood to transport O2 to body cells and
tissues
• Carbon dioxide (CO2)
– Colorless, odorless gas
– 93% of atmospheric CO2 result of
natural carbon cycle
– Rest from burning fossil fuels, clearing
forests and grasslands
– Now classified as air pollutant due to
role in climate change
Nitrogen oxides and nitric acid
– Nitric oxide (NO) colorless gas forms
when N and O react at high combustion
temps in auto engines and coal-burning
power/industrial plants
– In air NO reacts with O to form Nitrogen
dioxide (NO2), reddish brown gas
– Collectively NO and NO2 called Nitrogen oxides (NOx)
• Some NO2 reacts with water vapor to
form nitric acid (HNO3) and nitrate
salts (NO3-), components of acid
deposition
• Both NO and NO2 play role in formation of
photochemical smog: a mixture of chemicals
formed under influence of sunlight in cities
with heavy traffic
• Nitrous oxide (N2O) greenhouse gas,
emitted from fertilizers and animal
wastes and produced by burning
fossil fuels
• Nitrogen oxides can irritate eyes, nose, throat;
aggravate lung ailments, suppress plant growth,
and reduce visibility
Sulfur dioxide and sulfuric acid
• Sulfur dioxide (SO2) colorless gas with irritating odor
• 1/3 from natural sources, 2/3 from human sources such
as combustion of sulfur containing coal and oil refining
and smelting
• Can be converted to aerosols, microscopic suspended
droplets of sulfuric acid (H2SO4) and suspended
particles of sulfate (SO4) salts that return to Earth as
component of acid deposition
• SO2, H2SO4 droplets, and suspended particles of sulfate
reduce visibility; aggravate breathing problems; also damage
crops, trees, soils and aquatic life, corrode metals, damage
stone on buildings and statues
• Major component of Asian Brown Cloud
Particulates
• Suspended particulate matter (SPM)
• Variety of solid particles and liquid droplets small and
light enough to remain suspended in air for long periods
• 38% from human sources such as coal burning plants,
motor vehicles, road construction, and tobacco smoke
• Major component of Asian Brown Cloud
• These particles can irritate nose, throat; damage lungs;
aggravate asthma and bronchitis, and shorten life
• Also contains toxic particulates; can lead to mutations,
reproductive problems, cancer
• Reduce visibility, corrode metals, discolor clothes and
paints
Ozone
• Ozone (O3), colorless, highly reactive gas,
major ingredient of photochemical smog
• Can cause coughing, breathing problems,
aggravate lung and heart disease, reduce
resistance to colds/ pnuemonia, irritate
eyes, nose, throat
• damages plants, rubber in tires, fabrics,
paints
• Ozone in troposphere near ground
level “bad ozone”
• Ozone in stratosphere “good ozone”
b/c protects us from the sun’s harmful
UV radiation
• Same chemical
• Human activities decreasing “good
ozone” increasing “bad ozone”
Volatile organic compounds
(VOCs)
• VOC’s are organic compounds that exist as gases in the
atmosphere or that evaporate into the atmosphere
• Ex. hydrocarbons emitted by leaves of many plants and
methane (CH4) a greenhouse gas 20 times more
effective per molecule than CO2 is at warming
atmosphere
• 1/3 from natural sources, 2/3 human sources; rice
paddies, landfills, oil and natural gas wells, cows
• Other VOCs are liquids that evaporate into atmosphere
ex. Benzene and other industrial solvents, dry cleaning
fluids, components of gasoline, plastics, and other
products
Sources and types of air pollutants
Primary Pollutants
CO CO2
SO2 NO NO2
Most hydrocarbons
Most suspended particles
Secondary Pollutants
SO3
HNO3 H2SO4
H2O2 O3 PANs
Most NO3– and SO42– salts
Sources
Natural
Stationary
Mobile
Fig. 15-3, p. 371
In Class
• List the major outdoor air pollutants,
describe, and give their harmful effects.
Industrial Smog
• Burning coal
– Sulfur dioxide, sulfuric acid, suspended particles (gray
air smog)
– Coal-burning a major contributor to Asian Brown
Cloud
• Developed versus developing
countries
– Air pollution control in the U.S. and Europe
– China, India, Ukraine
Photochemical Smog
• Photochemical reactions: chemical
rxn activated by sunlight
• Photochemical smog: mixture of primary
and secondary pollutants formed under the influence
of UV radiation from the sun
– Brown-air smog (contains NO2)
• Sources
• Health effects
• Urban areas
Photochemcial smog in Santiago, Chile
Fig. 15-4, p. 373
Natural Factors That Reduce Air
Pollution
•
•
•
•
•
Particles heavier than air
Rain and snow
Salty sea spray from oceans
Winds
Chemical reactions
Natural Factors That Increase
Air Pollution
•
•
•
•
Urban buildings
Hills and mountains
High temperatures
VOC emissions from certain trees
and plants
• Grasshopper effect
• Temperature inversions
http://www.lchs.wolfcreek.ab.ca/lcsweb/Staff/sschultz/Sci30/007DA42D
-000F810F.5/Grasshopper%20effect.jpg
http://www.airquality.utah.gov/Public-Interest/Current-Issues/cachevalley-PM/Images/Inversion.jpg
Acid Deposition
•
•
•
•
Sulfur dioxides and nitrogen oxides
Wet and dry deposition
Acid rain
Regional air pollution
– Midwest coal-burning power plants
– Prevailing winds
Acid deposition: consists of rain, snow, dust, or gas with pH less than 5.6
Wind
Transformation
to sulfuric acid
(H2SO4) and nitric
acid (HNO3)
Nitric oxide (NO)
Windborne ammonia gas
and some soil particles partially
neutralize acids and form dry
sulfate and nitrate salts
Sulfur dioxide
(SO2) and NO
Wet acid deposition
(droplets of H2SO4 and
HNO3 dissolved in rain
and snow)
Dry acid deposition
(sulfur dioxide gas
and particles of
sulfate and nitrate salts)
Acid fog
Lakes in deep
soil high in
limestone
are buffered
Lakes in shallow
soil low in
limestone
become acidic
Fig. 15-5, p. 374
Regions where acid deposition is now a problem and regions with the potential to
develop this problem
Potential problem areas because of sensitive soils
Potential problem areas because of air pollution:
emissions leading to acid deposition
Current problem areas (including lakes and rivers)
Fig. 15-6, p. 375
Harmful Effects of Acid
Deposition
•
•
•
•
•
•
Structural damage
Respiratory diseases in humans
Toxic metal leaching
Kills fish and other aquatic organisms
Leaches plant nutrients from soil
Acid clouds and fog at mountaintops
Solutions
Acid Deposition
Prevention
Cleanup
Reduce coal use
Add lime to
neutralize
acidified lakes
Burn low-sulfur coal
Increase natural gas use
Increase use of renewable
energy resources
Add phosphate
fertilizer to
neutralize
acidified lakes
Remove SO2 particulates
and NOx from smokestack
gases
Remove NOx from motor
vehicular exhaust
Tax emissions of SO2
Reduce air pollution by
improving energy efficiency
Fig. 15-7, p. 376
Indoor Air Pollution
• According to WHO indoor air pollution is
world’s most serious air pollution
problem especially for poor people
• Developing countries
– Indoor cooking and heating
• Often higher concentration in buildings and cars
• Most time is spent indoors or in cars
• EPA – top cancer risk
Major Indoor Air Pollutants
•
•
•
•
Tobacco smoke
Formaldehyde
Radioactive radon-222 gas
Very small particles
Chloroform
Source: Chlorine-treated water in
hot showers
Possible threat: Cancer
Para-dichlorobenzene
Source: Air fresheners,
mothball crystals
Threat: Cancer
1,1,1-Trichloroethane
Source: Aerosol sprays
Threat: Dizziness,
irregular breathing
Tetrachloroethylene
Source: Dry-cleaning
fluid fumes on clothes
Threat: Nerve disorders,
damage to liver and
kidneys, possible cancer
Formaldehyde
Source: Furniture stuffing,
paneling, particleboard,
foam insulation
Threat: Irritation of eyes,
throat, skin, and lungs;
nausea; dizziness
Styrene
Source: Carpets,
plastic products
Threat: Kidney and
liver damage
Nitrogen oxides
Source: Unvented gas
stoves and kerosene
heaters, woodstoves
Threat: Irritated lungs,
children's colds,
headaches
Benzo-α-pyrene
Source: Tobacco smoke,
woodstoves
Threat: Lung cancer
Particulates
Source: Pollen, pet
dander, dust mites,
cooking smoke particles
Threat: Irritated lungs,
asthma attacks, itchy
eyes, runny nose,
lung disease
Radon-222
Source: Radioactive soil
and rock surrounding
foundation, water supply
Threat: Lung cancer
Tobacco smoke
Source: Cigarettes
Threat: Lung cancer, respiratory
ailments, heart disease
Asbestos
Source: Pipe insulation, vinyl
ceiling and floor tiles
Threat: Lung disease, lung cancer
Carbon monoxide
Source: Faulty furnaces,
unvented gas stoves and
kerosene heaters,
woodstoves
Threat: Headaches,
drowsiness, irregular
heartbeat, death
Methylene chloride
Source: Paint strippers and thinners
Threat: Nerve disorders, diabetes
Fig. 15-8, p. 377
Air Pollution and the Human
Respiratory System
• Natural protective system; hairs in nose
filter out large particles, mucus captures
particles, cilia (tiny mucus coated, hair-like
structures) transport pollutants they trap
• Lung cancer, chronic bronchitis,
emphysema, asthma
• Premature deaths
• Air pollution kills 2.4 million people
prematurely every year worldwide
Major components of respiratory system
Epithelial cell
Cilia
Nasal cavity
Oral cavity
Goblet cell
(secreting
mucus)
Pharynx (throat)
Mucus
Trachea (windpipe)
Bronchioles
Bronchus
Alveolar duct
Right lung
Bronchioles
Alveoli
Alveolar sac
(sectioned)
Fig. 15-9, p. 378
Premature deaths from
air pollution in US
Deaths per 100,000 adults per year
<1
1–5
5–10 10–20 20–30 30+
Fig. 15-10, p. 378
15-3 How Should We Deal with
Air Pollution?
• Concept 15-3 Legal, economic, and
technological tools can help clean up
air pollution, but the best solution is to
prevent it.
U.S. Outdoor Air Pollution
Control Laws
• Clean Air Acts 1970, 1977, 1990
• Air-quality standards for 6 major
outdoor pollutants
– Carbon monoxide (CO), nitrogen dioxide
(NO2), sulfur dioxide (SO2), SPM, ozone
(O3), and lead
• Levels of these 6 pollutants have fallen
dramatically between 1980 and 2008
*Improving Air Pollution Laws (1)
• Emphasize pollution prevention
• Increase fuel economy standards
• Regulate emissions from two-cycle
engines
• Regulate ultra-fine particles
*Improving Air Pollution Laws (2)
• Increase regulations at airports
• Decrease urban ozone
• Increase regulations for indoor air
pollution
• Better enforcement of Clean Air Act
*Using the Marketplace to
Reduce Air Pollution
• Clean Air Act of 1990 authorized
emissions trading (cap and trade) program
– Enables 110 most polluting coal burning
power plants in 21 states to buy and sell SO2
pollution rights
• Proponents – cheaper and more efficient
• Critics – companies buy their way out
• Success depends on cap being gradually
lowered
Solutions
Stationary Source Air Pollution
Prevention
Dispersion or
Burn low-sulfur coal
Disperse emissions above
thermal inversion layer with
tall smokestacks
Cleanup
Remove sulfur from coal
Convert coal to a liquid
or gaseous fuel
Shift to less polluting
energy sources
Remove pollutants after
combustion
Tax each unit of pollution
produced
Fig. 15-11, p. 380
Solutions
Motor Vehicle Air Pollution
Prevention
Cleanup
Use mass transit
Require
emission
control devices
Walk or bike
Use less polluting
fuels
Get older, polluting
cars off the road
Inspect car
exhaust
systems
twice a year
Give large tax
write-offs or rebates
for buying lowpolluting, energy
efficient vehicles
Set strict
emission
standards
Improve fuel efficiency
Fig. 15-12, p. 381
Solutions
Indoor Air Pollution
Prevention
Clean ceiling tiles
and line AC
ducts to
prevent release
of mineral fibers
Ban smoking
or limit it to
well-ventilated
areas
Set stricter
formaldehyde
emissions
standards
for carpet,
furniture, and
building
materials
Prevent radon
infiltration
Use office
machines
in wellventilated areas
Use less
polluting
substitutes for
harmful cleaning
agents, paints,
and other products
Cleanup or
Dilution
Use adjustable
fresh air vents
for work spaces
Increase
intake of
outside air
Change air
more
frequently
Circulate a
building’s air
through rooftop
greenhouses
Use efficient
venting systems
for woodburning
stoves
Use exhaust
hoods
for stoves and
appliances
burning
natural gas
Fig. 15-13, p. 381
Fig. 15-14, p. 381
Solutions
Air Pollution
Outdoor
Indoor
Improve energy
efficiency to
reduce fossil fuel
use
Reduce poverty
Rely more on
lower-polluting
natural gas
Rely more on
renewable energy
(especially solar
cells, wind,
geothermal and
solar-produced
hydrogen)
Transfer energy
efficiency,
renewable energy,
and pollution
prevention
technologies
to developing
countries
Distribute cheap
and efficient
cookstoves or
solar cookers to
poor families in
developing
countries
Reduce or ban
indoor smoking
Develop simple
and cheap tests
for indoor
pollutants such
as particulates,
radon, and
formaldehyde
Fig. 15-15, p. 382
15-4 How Might the Earth’s
Climate Change in the Future?
• Concept 15-4 Considerable scientific
evidence indicates that emissions of
greenhouse gases into the earth’s
atmosphere from human activities will
lead to significant climate change
during this century.
Climate Change
• http://www.youtube.com/watch?v=oJ
AbATJCugs
Past Climate Changes
• Glacial and interglacial periods over past
900,000 yrs
• Global cooling and global warming
• Measurement of past temperature changes
– Radioisotopes in rocks and fossils
– Tiny bubbles of ancient air found in ice cores
from glaciers
– Tree rings
– Historical measurements since 1861
AVERAGE TEMPERATURE (over past 900,000 years
TEMPERATURE CHANGE (over past 22,000 years
AVERAGE TEMPERATURE (over past 130 years
TEMPERATURE CHANGE (over past 1,000 years
Stepped Art
Fig. 15-16, p. 383
Ice cores are extracted by drilling deep holes into ancient glaciers at various sites like
this one in Antarctica. .
Fig. 15-17, p. 383
The Greenhouse Effect
• Life on Earth is totally dependent on natural
greenhouse effect
• Without this greenhouse effect, the world would
be too cold to support the forms of life we find
today
• Natural greenhouse gases
– Water vapor (H2O)
– Carbon dioxide (CO2)
– Methane (CH4)
– Nitrous Oxide (N2O)
List the 4 natural greenhouse gasses.
What is the importance of the
greenhouse effect?
• http://earthguide.ucsd.edu/earthguide/
diagrams/greenhouse/
Evidence to Support Global
Warming (1)
• Intergovernmental Panel on Climate
Change
• 2007 IPCC report
• Rise in average global surface
temperature
• 10 warmest years on record since
1970
Evidence to Support Global
Warming (2)
• Annual greenhouse gas emissions up
70% between 1970 and 2008
• Changes in glaciers, rainfall patterns,
hurricanes
• Sea level rise in this century 4–8
inches
Melting of Alaska’s Muir Glacier in Glacier Bay National Park and Preserve between
1948 and 2004. Mountain glaciers are now melting everywhere in the world.
The big melt. Each summer, some of the floating sea ice in the Arctic Sea melts and
Then refreezes during winter. But in recent years, rising atmospheric and ocean temps
have caused more and more ice to melt. Satellite data show a 39% drop in the average
Cover of summer Arctic ice between 1979 and 2007. Such summer ice may be gone by
2037, and perhaps earlier.
Sept. 1979
Sept. 2008
Russia
Russia
*
North
pole
*
North
pole
Greenland
Alaska (U.S.)
Greenland
Alaska (U.S.)
Canada
Canada
Fig. 15-19, p. 385
CO2 Emissions Are the Major Culprit
• 1850: 285 ppm (Start of the Industrial Revolution)
• 2009: 388 ppm
• Over 450 ppm is tipping point (could set into
motion large-scale climate changes for hundreds to thousands of
years)
• 350 ppm as intermediate goal
Science Focus: Scientific Consensus about
Future Global Temperature Changes?
• Temperature as a function of
greenhouse gases
• Mathematical models
• Model data and assumptions
• Predictions and model reliability
• Recent warming due to human
activities
Simplified model of some major processes that interact to determine the average
temperature and greenhouse gas content of the lower atmosphere and thus the Earth’s
climate. Red arrows show processes resulting in warming; blue cooling.
Troposphere
Cooling
from
increase
Aerosols
Greenhouse
gases
Warming
from
decrease
CO2 removal
by plants and
soil organisms
CO2 emissions from
land clearing,
fires, and decay
Heat and
CO2 removal
Heat and
CO2 emissions
Ice and snow cover
Shallow ocean
Land and soil biota
Natural and human emissions
Long-term
storage
Deep ocean
Fig. 15-A, p. 386
Fig. 15-B, p. 387
What Role for Oceans in
Climate Change?
• Oceans help to moderate earth’s avg surface
temp and thus climate by removing about 2530% of CO2 pumped into lower atmosphere by
human activities
• Absorb heat from lower atmoshere and slowly
transfer some CO2 to deep ocean
• CO2 solubility decreases with increasing
temperature
• Upper ocean getting warmer
• Acidity of ocean increasing
15-5 What Are Some Possible Effects
of a Projected Climate Change?
• Concept 15-5 The projected change
in the earth’s climate during this
century could have severe and longlasting consequences, including
increased drought and flooding, rising
sea levels, and shifts in locations of
agriculture and wildlife habitats.
Potential Severe Consequences
•
•
•
•
Rapid projected temperature increase
2 Cº inevitable
4 Cº possible
Effects will last for at least 1,000
years
Fig. 15-20, p. 389
Harmful Effects of Global
Warming (1)
•
•
•
•
•
Excessive heat
Drought
Ice and snow melt
Rising sea levels
Extreme weather
Harmful Effects of Global
Warming (2)
•
•
•
•
Threat to biodiversity
Food production may decline
Change location of agricultural crops
Threats to human health
Glaciers covering about 80% of Greenland, the world’s largest island, contain about 10%
of the world’s freshwater. This is enough water to raise global sea level by 23 ft if they all
melt. Complete melting unlikely, but partial summer melting of some of its glacial ice
increased dramatically between 1982 and 2007.
Fig. 15-21, p. 390
Areas of Florida that will be flooded (red) if the average sea level rises by 1 meter
(3.3 ft).
Fig. 15-22, p. 391
S45
15-6 What Can We Do to Slow
Projected Climate Change?
• Concept 15-6 To slow the rate of
projected climate change, we can
increase energy efficiency, sharply
reduce greenhouse gas emissions,
rely more on renewable energy
resources, and slow population
growth.
Options to Deal with Climate
Change
• Two approaches:
1. Drastically reduce greenhouse gas
emissions
2. Develop strategies to reduce its
harmful effects
• Mix both approaches
• Governments beginning to act
Solutions
Slowing Climate Change
Prevention
Cleanup
Cut fossil fuel
use (especially
coal)
Remove CO2 from
smokestack and
vehicle emissions
Shift from coal
to natural gas
Improve energy
efficiency
Store (sequester)
CO2 by planting
trees
Sequester CO2 in
soil by using notill cultivation and
taking cropland
out of production
Shift to
renewable
energy resources
Transfer energy
efficiency and
renewable energy
technologies to
developing
countries
Reduce
deforestation
Use more
sustainable
agriculture and
forestry
Limit urban
sprawl
Reduce poverty
Slow population
growth
Sequester CO2
deep
underground
(with no leaks
allowed)
Sequester CO2 in
the deep ocean
(with no leaks
allowed)
Repair leaky
natural gas
pipelines and
facilities
Use animal feeds
that reduce CH4
emissions from
cows (belching)
Fig. 15-23, p. 393
Reducing the Threat of Climate
Change (1)
• Improve energy efficiency to reduce
fossil fuel use
• Shift from coal to natural gas
• Improve energy efficiency
• Shift to renewable energy sources
Reducing the Threat of Climate
Change (2)
• Transfer appropriate technology to
developing countries
• Reduce deforestation
• Sustainable agriculture and forestry
• Reduce poverty
• Slow population growth
Reducing the Threat of Climate
Change (3)
• Decrease CO2 emissions
• Sequester CO2
– Plant trees
– Agriculture
– Underground
– Deep ocean
• Repair leaking natural gas lines
• Reduce methane emissions from
animals
Science Focus: Is Capturing and
Storing CO2 the Answer? (1)
• Global tree planting
• Restore wetlands
• Plant fast-growing perennials
Science Focus: Is Capturing and
Storing CO2 the Answer? (2)
• Preserve natural forests
• Seed oceans with iron to promote
growth of phytoplankton
• Sequester carbon dioxide
underground and under the ocean
floor
Oil rig
Tanker delivers
CO2 from plant
to rig
CO2 is pumped
down from rig for
disposal in deep
ocean or under
seafloor sediments
Coal power
plant
Tree plantation
Abandoned
oil field
Switchgrass
Crop field
CO2 is pumped
underground
Spent oil or
natural gas
reservoir
Spent coal
bed cavern
Deep, saltwater-filled cavern
= CO2 pumping
= CO2 deposit
Fig. 15-C, p. 394
• What are the limitations to carbon capture
and storage?
Government Roles in Reducing the
Threat of Climate Change (1)
• Regulate carbon dioxide and
methane as pollutants
• Carbon taxes
• Cap total CO2 emissions
• Subsidize energy-efficient
technologies
• Technology transfers
Government Roles in Reducing the
Threat of Climate Change (2)
• International climate negotiations
• Kyoto Protocol (US withdrew in 2001)
• Act locally
– Costa Rica, aims to be first country to be carbon
neutral
– U.S. states; 30 US states had greenhouse gas
reduction programs by 2009
– Large corporations such as Alcoa, DuPont, IBM,
Toyota, General Electric have set goals for reducing
greenhouse gas emissions
– Colleges and universities; such as Oberlin College
Fig. 15-24, p. 396
Ways to prepare for possible long term harmful effects of climate change.
Develop crops that
need less water
Waste less water
Connect wildlife
reserves with corridors
Move hazardous material storage
tanks away from coast
Move people away
from low-lying
coastal areas
Stockpile 1- to 5-year
supply of key foods
Prohibit new construction
on low-lying coastal areas
or build houses on stilts
Expand existing
wildlife reserves
toward poles
Fig. 15-25, p. 396
15-7 How Have We Depleted Ozone in the
Stratosphere and What Can We Do about It?
• Concept 15-7A Widespread use of
certain chemicals has reduced ozone
levels in the stratosphere and allowed
more harmful ultraviolet radiation to reach
the earth’s surface.
• Concept 15-7B To reverse ozone
depletion, we need to stop producing
ozone-depleting chemicals and adhere to
the international treaties that ban such
chemicals.
Human Impact on
the Ozone Layer
• Location and purpose of the ozone
layer
– Blocks UV-A and UV-B radiation
• Seasonal and long-term depletion of
ozone
• Threat to humans, animals, plants
• Causes – chlorofluorocarbons (CFCs)
Individuals Matter: Banning of
Chlorofluorocarbons (CFCs)
• Chemists Rowland and Molina –
– Nobel Prize in 1995
• Called for ban
– Remain in atmosphere
– Rise into stratosphere
– Break down into atoms that accelerate
ozone depletion
– Stay in stratosphere for long periods
• Defended research against big industry
Former Uses of CFCs
• Coolants in air conditioners and
refrigerators
• Propellants in aerosol cans
• Cleaning solutions for electronic parts
• Fumigants
• Bubbles in plastic packing foam
Fig. 15-26, p. 398
Fig. 15-27, p. 398
Reversing Ozone Depletion
• Stop producing ozone-depleting
chemicals
• Slow recovery
• Montreal Protocol
• Copenhagen Protocol
• International cooperation
Three Big Ideas from This
Chapter - #1
All countries need to step up efforts to
control and prevent outdoor and
indoor air pollution.
Three Big Ideas from This
Chapter - #2
Reducing the possible harmful effects
of projected rapid climate change
during this century requires
emergency action to cut energy
waste, sharply reduce greenhouse
gas emissions, rely more on
renewable energy resources, and
slow population growth.
Three Big Ideas from This
Chapter - #3
We need to continue phasing out the
use of chemicals that have reduced
ozone levels in the stratosphere and
allowed more harmful ultraviolet
radiation to reach the earth’s surface.
Teacher’s Guide to Climate Change
• http://hdgc.epp.cmu.edu/teachersguid
e/teachersguide.htm
• http://education.usgs.gov/secondary.h
tml