Chp. 8: “Air and Air Pollution”
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Transcript Chp. 8: “Air and Air Pollution”
Chapter 10
The Atmospheric Environment
Air Pollution: Long Distance
Traveler
Winds distribute pollutants
Developing countries lack regulations
Global distillation effect
Canadian Arctic accumulates
high levels of toxins
Inuit people
High levels of PCBs
Why?
The Atmosphere
Gaseous envelope surrounding Earth
Mostly oxygen & nitrogen (99%)
Four layers
Troposphere
Stratosphere
Mesosphere
Thermosphere
The Atmosphere
The Atmosphere
What’s In Our Atmosphere
Nitrogen
Oxygen
Argon
Carbon dioxide
Other Gases
78%
21%
0.93%
0.04%
0.03%
The Atmosphere
Ecosystem services
Protects Earth from UV radiation
Allows visible light and some infrared
to penetrate
We depend on
the atmosphere
Oxygen balance
The sun makes life on Earth possible:
Primary determinant of climate: amount
of sunlight received
Solar radiation powers
Earth’s cycles
Solar Radiation and
Atmospheric Circulation
Electromagnetic spectrum
Entire range of electromagnetic radiation
Includes gamma, x-ray, ultraviolet, visible, infrared,
microwave, and radio
43% of incoming solar radiation peaks in visible light
wavelengths
Gamma, x-rays and most UV rays are absorbed by the
stratosphere
Plants use portions of visible light for photosynthesis
Sun does not
reach all places
uniformly:
why?
Temperature
varies locally
Inclination on its axis determines Earth’s
seasons
N. and S. hemispheres are opposite
The Atmosphere
Temperature differences drive circulation
Continuous circulation moderates surface
temperature on the Earth
Atmospheric Circulation
Winds
Small-scale, horizontal movements
Result of atmospheric pressure and Earth’s
rotation
Prevailing winds
Major surface winds; blow continuously
Polar easterlies, westerlies, trade winds
Atmospheric Circulation
Coriolis effect
Earth’s rotation
from west to east
Moving air or
water is
deflected
N. hemisphere:
deflected right
S. hemisphere:
deflected left
Influences wind
direction
Oceanic Conveyor Belt
Transfer of warm water from Pacific ocean to the
Atlantic as a surface current
Cold dense water sinks and slowly flows from
Atlantic to the Pacific Ocean as a deep water
current
Weather
Atmospheric conditions at a specific place
and time
Rapid changes
Climate
Average weather conditions
Changes over hundreds/thousands of
years
Important factors: temperature and
precipitation
Air Quality &
Air Pollution
Various chemicals present in the
atmosphere in levels high enough to cause
harm
Natural & human sources
Seven important types
Two categories
Primary: enter directly into atmosphere
Secondary: form in the atmosphere
Primary and Secondary Air Pollution
Carbon Oxides
Gases
Carbon monoxide
Colorless, odorless, tasteless
Reduces blood’s ability to transport
oxygen
Carbon dioxide
Produced in very large quantities
Major greenhouse gas
Sulfer Oxides
Gases
Acid deposition
Corrode metals, damage stone
Damage plants, respiratory irritant
Nitrogen Oxides
Gases
Inhibit plant growth
Aggravate health problems
Photochemical smog
Nitrous oxide: greenhouse gas, depletes
ozone
Nitrogen oxides: corrode metals &
textiles
Particulate Matter
Different solid and liquid particles
Suspended in the atmosphere
Soil particles, soot, lead, etc…
Corrodes metal, erodes buildings, soils
clothing
Can be microscopic!
Inhaling can be hazardous
Hydrocarbons
Contain only carbon and hydrogen
Methane, benzene, paraffin
Many different kinds!
Varying effects
Some have no effect
Some cause respiratory damage
Some cause cancer
Sources of Sulphur and
Nitrogen Oxide Emissions
Volatile Organic Compounds
VOC’s: unburned hydrocarbons and
vapors that evaporate easily in the
atmosphere
VOC concentration may be 10 times
higher indoors, why?
Toxic effect on humans
Ozone
Essential component of stratosphere
Filters out harmful UV radiation
Pollutant in the troposphere
Most harmful component of photochemical smog
Reduces visibility,
causes health problems
Reduces plant vigor
Sources of Air Pollutants
Natural:
Erupting volcanoes
Forest fires (lightening)
Ocean spray and salt particulates
Volatile organic compounds from coniferous
forests
Natural process from other vegetation
Air Pollution
Human Activities:
Fossil fuels (coal, natural gas)
Transportation (mobile)
Industrial (stationary)
Human Health Effects
Eye and respiratory tract problems
Suppresses immune system
Chronic respiratory disease
Cancer
Birth defects
Neurological damage
Effects of Air Pollution
Injures organisms
Reduces visibility
Corrodes metals, plastics,
textiles
Harms respiratory tracts
Reduces plant production
Ozone depletion, climate
change
Managing Air Pollution
Difficult due to long-range transport
Nations have to work together
Emissions trading – “cap and trade”
EU ETS – one of the largest programs
Kyoto Protocol uses emissions trading system
for six major greenhouse gases
Carbon credit trading – two types
COC’s
CRC’s
Canada’s Response
Clean Air Act
Includes air pollutants and greenhouse gases
Controversial
Federal and provincial governments need to
work together
Incentive-based regulation
Kyoto Protocol
Signed in 1997
Conservative government dropped it in 2006
Second Clean Air Act introduced
Urban Air Pollution
Smog
Industrial smog
Sulphur oxides, particulate matter
Worst in winter…why?
More problematic in developing
countries…why?
Urban Air Pollution
Photochemical smog
Brownish-orange haze
Chemical reactions
Worst in
summer…why?
Sources?
Urban Air Pollution
Weather and Topography
Temperature change air circulates
pollutants dispersed
Temperature inversion
Cold air layer trapped near the ground
by warm layer
Traps pollutants close to ground
Cities in valleys: more temperature
inversions
Temperature Inversion
Commitments to
Reduce Smog
Smog has serious impacts on Canadian
economy
1990, Canadian Council of Ministers of
the Environment developed
regulations, guidelines and education
initiatives
Targeted automobile emissions and
commercial emission restrictions
Los Angeles
Very bad
smog…why?
1969: California is
first state to enforce
vehicle emission
standards
Every pollutant
regulated today
Should meet federal
standards by 2010
Sulphur and nitric acids in precipitation
Dry acid particles in air
Around since Industrial Revolution
Causes much damage
Kills fish, damages structures
Affects forest ecosystems
Sulphur dioxide and nitrogen oxides
released
Where do these pollutants come from?
Wind carries these pollutants
React with water in atmosphere
Form dilute acids
Sulphuric
Nitric, nitrous
How Acid Deposition Develops
Ph Scale runs from zero (most acidic) to
fourteen (most alkaline)
A one unit change on the Ph scale
represents a 10 fold unit change in
acidity
Corrodes metals and building materials
Decline in some fish species
Birds lay eggs with thinner shells
Damaging to forests
Research at ELA on lake 223
Reduction in Ph
Reduction in biodiversity
Ph lower than 4.0 may mean no fish at all
Damage to forests
Overall tree weakening
Increase in UV radiation
Insect infestation
Changes in soil chemistry
Difficult to control
Who should pay for the pollution?
Acids are released in one place
Returned to Earth’s surface hundreds
of miles from source
Over past 15 years, Canada has committed to
reducing sulphur dioxide
1985, Eastern Canadian Acid Rain Program
1991, Canada-United States Air Quality
Agreement
Canada Wide Acid Rain Strategy for Post-2000
Reduction achieved by:
Scrubbers installed in smoke stacks
Low sulphur coal (but other problems arise)
Acid Neutralizing Capacity
Ability of water or soil to neutralize
acids
Critical Loads
Maximum amount of pollution an
ecosystem can tolerate before it
becomes damaged
Indoor Air Pollution
May be more pollution inside than out!
We spend a lot of time indoors
Radon, cigarette smoke, cleaners, etc…
Viruses, bacteria, fungi, dust mites
Sick building syndrome
Eye irritations, nausea, headaches, fatigue
Caused by indoor air pollution
Lost work time
Indoor Air Pollution
Radon
Most serious indoor air pollutant
Radioactive gas produced by decay of radium
in Earth’s crust
Seeps into homes
Dangerous when inhaled
Can cause cancer
Energy efficient homes,
radon can’t disperse
Test your home!
Temperature is increasing
Spring arriving earlier; autumn later
more heat waves
Radiative forcing – the imbalance in
the Earth’s energy budget that results
when the amount of energy radiated to
outer space is changed through either
natural or human influences
Positive forcing results in warming
Negative forcing leads to cooling
Greenhouse gases
absorb infrared
radiation
warms
atmosphere
We are increasing
concentrations of
these gases
Two important factors: amount of gas
emitted and properties of the gas
Average residence time: length of time gas
resides in the atmosphere
Global warming potential: how much given
mass of greenhouse gas contributes to global
warming over a period of time compared to
the same mass of carbon dioxide
CO2, CH4, N2O, CFCs,
O3 accumulate
Where do these gases
come from?
Concentrations of
these gases are
increasing
Carbon Footprint
What is a Carbon
footprint?
Calculate your
carbon footprint
Think about what
steps you can take
to reduce your
carbon footprint
Some pollutants cool the atmosphere
Atmospheric aerosols
Natural human sources
Reflect sunlight into space
Cools atmosphere
Sulphur haze, volcanic
eruptions
Most nations
trying to reduce
Precipitation patterns will change
More droughts, floods
Impact on freshwater supplies
Agricultural changes
Some areas will flood
Pests could increase their ranges
Polar amplification
More extinctions
Melting sea ice
Rise in sea level, devastating impacts on
coastal communities
Increasing coastal erosion rates
Changing salt levels in ocean
Rise in sea level with flood some agricultural
lands
Agricultural pests and disease causing
organisms will reduce crop yields
Increased frequency of drought (occurrence
and duration) – more drought resistant crops
Changing length of growing season
New areas suitable for agricultural production
Every species on earth affects
Some will expand and thrive – example
Mountain Pine Beetle
Inter-related ecosystem changes
At greatest risks are
polar seas
coral reefs
mountain ecosystems
coastal wetlands
tundra
More extinctions
Antarctica: less silverfish less Adélie
penguins; more egg failures
Bleaching of coral reefs ; increase 10-20 C
Tree species may shift ranges
More heat-related illness
More malaria, dengue & yellow fever: why?
More schistosomiasis, cholera
CO2 must be the focus
Two ways to manage
Mitigation
Moderate/postpone global climate change
Buy us time
Adaptation
Response to changes
Implies that climate change is unavoidable
Mitigation of Global
Climate Change
Developing fuel alternatives
Increasing energy efficiency
Plant and maintain trees:
Carbon management
Separate and capture CO2
Sequester from atmosphere
Coastal populations must move inland
Build massive sea walls
Plant different crops: why?
Develop heat and drought-resistant trees
Change coastal sewage systems to reduce
flooding
Pollutant in troposphere
Essential in stratosphere: why?
CFC’s, halons,
industrial solvents
First used in 1960’s
These chemical were
cheap and easy to
produce
Were eventually
banned
More UV radiation reaches Earth
Damage to ecosystems
Human health problems
More cataracts
More skin cancer
Weakened immunity
1987 Montreal Protocol – 50% reduction
By 2007, 191 countries participating
Industry substitutes such as
hydroflurocarbons do not attack ozone
but are potent greenhouse gases
Most countries have phased out HCFC’s
Long residence time
Eco Canada Career Focus
Consider a career as
a Climatologist
Use long range data
to study trends and
make predictions
about climate
change
Case Study: IDHP
Management of the atmospheric
environment on a global scale
Promotes scientific and social research
Initiated in 1990
Decision making, policy creation, raising
awareness happens across many
governmental levels
Assists with linkages and multi-level
decision making