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The Atmosphere: 
Climate, Climate Change & Ozone Depletion 
Reporters: 
Jovannie Espinosa & Markleen Guimbao
Earth’s Atmosphere 
The Earth's atmosphere is more 
than just the air we breathe. It's 
also a buffer that keeps us from 
being peppered by meteorites, a 
screen against deadly radiation, 
and the reason radio waves can 
be bounced for long distances 
around the planet.
Earth’s Atmosphere 
Troposphere 
The lowest is the troposphere, which is the 
layer that provides most of our weather. It 
contains about four-fifths of the Earth's air, 
but extends only to a height of about 11 
miles (17 kilometers) at the Equator and 
somewhat less at the Poles.
Earth’s Atmosphere 
Stratosphere 
Above the troposphere is the stratosphere. 
It extends to a height of about 30 miles (50 
kilometers) and includes the ozone layer, 
which blocks much of the sun's harmful 
ultraviolet rays. It is warmer than the 
troposphere because of the energy from 
the ultraviolet light absorbed by the ozone.
Earth’s Atmosphere 
Stratosphere 
Greenhouse Effect, the capacity of certain 
gases in the atmosphere to trap heat 
emitted from Earth’s surface, thereby 
insulating and warming the planet. Without 
the thermal blanketing of the natural 
greenhouse effect, Earth’s climate would be 
about 33°C (about 59°F) cooler—too cold 
for most living organisms to survive.
Earth’s Atmosphere 
Mesosphere 
In this layer, the air temperature drops 
again, down to nearly -180 degrees 
Fahrenheit (-120 degrees Celsius) at the 
top. Meteors generally burn up in the 
mesosphere, which extends to a height of 
about 52 miles (85 kilometers). This is why 
the Earth's surface isn't pocked with meteor 
craters, like the moon's.
Earth’s Atmosphere 
Ionosphere 
It extends to about 430 miles (690 
kilometers) and is so thin it's generally 
considered part of outer space. The 
International Space Station and many 
satellites orbit within the ionosphere. 
It is named for the ions created within this 
layer by energetic particles from sunlight 
and outer space. These ions create an 
electrical layer that reflects radio waves, 
allowing radio messages to be sent across 
oceans in the days before communication 
satellites.
Earth’s Atmosphere 
Exosphere 
This tenuous portion of the Earth's 
atmosphere extends outward until it 
interacts with the solar wind. Solar storms 
compress the exosphere. When the sun is 
tranquil, this layer extends further outward. 
Its top ranges from 620 miles (1,000 
kilometers) to 6,214 miles (10,000 
kilometers) above the surface, where it 
merges with interplanetary space.
Weather 
Weather is the state of the 
atmosphere at a specific time and 
place, with respect to temperature, 
precipitation, and other factors 
such as cloudiness.
Weather 
Weather is generated by 
many forces, some 
obvious, some not. Warm, 
humid air masses blowing 
in from oceans, for 
example, fuel rains. 
Sunlight heats the land, 
generating thermals that 
help produce summer 
thunderstorms.
Weather 
Mountains and cities also 
affect the weather. In 
mountains this occurs 
because the wind must 
rise as it crosses over the 
ridge. This lifts the air, 
causing it to cool. That 
produces clouds, rain, or 
snow.
Weather 
Cities, on the other hand, 
produce urban "heat 
islands" where roads, 
parking lots, and rooftops 
warm in the sun. This not 
only raises the city's 
temperature, but it can 
affect the weather, 
producing thunderstorms 
in some cities or altering 
storm tracks in others.
Climate 
Climate isn't the same 
thing as weather. 
Weather is the condition 
of the atmosphere over a 
short period of time; 
climate is the average 
course of weather 
conditions for a particular 
location over a period of 
many years.
Climate 
One of the factors that influences climate is 
the angle of the sun's rays. In the tropics, between 
23.5° N and 23.5° S, there is at least one time of 
year when the noontime sun is directly overhead and 
its rays hit at a direct angle. This produces a hot 
climate with relatively small temperature differences 
between summer and winter.
Climate 
Climate is also 
controlled by 
wind, oceans, and 
mountains.
Global 
Climate 
Change
Global Climate Change 
Global Warming or 
Climate Change is a 
measurable increase 
in the average 
temperature of 
Earth’s atmosphere, 
oceans, and 
landmasses.
Global Climate Change 
Scientists believe that the Earth is 
currently facing a period of rapid warming 
brought on by rising levels of heat-trapping 
gases, known as greenhouse 
gases, in the atmosphere.
Global Climate Change 
Since the beginning of the Industrial 
Revolution in the mid-1700s, however, 
human activities have added more and 
more of these gases into the atmosphere.
Response to 
Climate Change
Response to Climate Change 
The first time climate change was recognized as a 
serious problem by an international gathering was in 
1979. The First World Climate Conference, held in 
February of that year, was a major scientific meeting. 
It issued a declaration calling on the world's 
governments "to foresee and prevent potential man-made 
changes in climate that might be adverse to 
the well-being of humanity."
Response to Climate Change 
A large number of international conferences on 
climate change have been convened since 
then. Attended by policy-makers, government 
leaders, and scientists, they have addressed 
both scientific and policy issues.
Response to Climate Change 
In 1985 the Vienna Convention for the 
Protection of the Ozone Layer was adopted. In 
1987 a protocol under the Vienna Convention, 
known as the Montréal Protocol, was signed 
and later ratified by 36 nations, including the 
United States.
Response to Climate Change 
The Second World Climate Conference, held in 
1990 in Geneva, was a particularly crucial step 
towards a binding global convention on climate 
change. Some of these meetings have taken place 
under the auspices of the United Nations and its 
specialized agencies. Others have been held within 
regional for a such as the European Community, the 
Commonwealth, and the South Pacific Forum.
Response to Climate Change 
The December 1997 summit on global warming in 
Kyōto, Japan, which included representatives from 
the United States, the European Union (EU), and 
many developing nations, reached an agreement 
for reducing emissions of gases that many 
scientists believe may lead to global warming and 
depletes ozone layer.
Depletion 
of the 
Ozone 
Layer
Ozone Layer Depletion 
The term "Ozone Layer" is used to 
describe the ozone molecules present 
in the stratosphere. The ozone layer 
stretches around the entire globe of the 
Earth like a bubble, filtering out harmful 
ultraviolet radiation from the sun. 
Destruction of the ozone layer 
increases the amount of ultraviolet 
radiation reaching the earth which can 
cause severe effects on human health 
and the environment.
Ozone Layer Depletion
Ozone Layer Depletion 
What is Ozone Layer Depletion? 
Ozone layer depletion is destruction of the upper 
atmospheric layer of ozone gas, caused by 
substances formed from breakdown of ozone 
depleting substances. The main cause of this is 
the release of chlorofluorocarbon (CFC).
Ozone Layer Depletion 
Chlorofluorocarbons or CFC’s 
are created and used in 
refrigerators and air 
conditioners. These are not 
harmful to humans and have 
been a benefit to us. Once 
released into the atmosphere, 
CFC’s are bombarded and 
destroyed by ultraviolet rays. In 
the process chlorine is 
released to destroy the ozone 
molecules.
Ozone Layer Depletion 
Destruction of ozone by chlorine
Ozone Layer Depletion
Ozone Layer Depletion 
NASA (2006) says ozone layer hole 
5th biggest on record… 
at a size of about 
27.4 million square 
kilometres (size of 
North America). 
http://www.cbc.ca/news/world/story/2008/11/05/ozone-hole.html
Atmospheric Pollution
Air Pollution Essentials 
Atmospheric pollution (also commonly 
called air pollution) is derived chiefly 
from the spewing of gasses and solid 
particulates into the atmosphere. Many 
pollutants occur naturally, but most air 
pollution is caused by human activity.
Air Pollutants – General Overview 
A substance in the air that can cause 
harm to humans and the environment is 
known as an air pollutant. Pollutants 
can be in the form of solid particles, 
liquid droplets, or gases.
Air Pollutants – General Overview 
Pollutants can be classified as primary or 
secondary. Usually, primary pollutants are 
directly emitted from a process, such as 
ash from a volcanic eruption, the carbon 
monoxide gas from a motor vehicle 
exhaust or sulfur dioxide released from 
factories. Secondary pollutants are not 
emitted directly. Rather, they form in the air 
when primary pollutants react or interact.
Air Pollutants – General Overview 
An important example of a secondary 
pollutant is ground level ozone — one of 
the many secondary pollutants that make 
up photochemical smog. Some pollutants 
may be both primary and secondary: that 
is, they are both emitted directly and 
formed from other primary pollutants.
Atmospheric Pollution 
Major Air Pollutants & Their Sources 
In the last 200 years or so there appeared several 
fundamental trends which became the major 
forces behind the surge in levels of air pollution 
throughout the globe. These are: 
• Industrialization 
• Population Growth 
• Globalization
Major Air Pollutants 
Industrialization 
Among other things, 
industrialization set in 
motion the widespread use 
of fossil fuels (oil, gas & 
coal) which are now 
the main pollution sources.
Major Air Pollutants 
Population Growth 
With population numbers literally 
exploding around the world, the 
demand for food and other goods 
goes up. This demand is met by 
expanded production and use of 
natural resources, which in its 
turn leads to higher levels 
of environmental pollution in 
general, and air pollution in 
particular.
Major Air Pollutants 
Globalization 
Globalization has become an 
effective facilitator of air pollution. 
Developing countries usually have 
much looser laws on environmental 
protection. With this “benefit” as 
well as the population growth and 
easy availability of cheap labor, big 
industry prefers to move its 
facilities to such “pollution havens” 
rather than work in more regulated 
markets.
Atmospheric Pollution 
More on Sources of Pollutants 
Ozone (03) 
Formed when reactive organic 
gases (ROG) and nitrogen oxides 
react in the presence of sunlight. 
ROG sources include any source 
that burns fuels, (e.g., gasoline, 
natural gas, wood, oil) solvents, 
petroleum processing and storage 
and pesticides.
More on Sources of Pollutants 
Respirable Particulate Matter (PM10) 
Road Dust, Windblown Dust (Agriculture) and 
Construction (Fireplaces). Also formed from 
other pollutants (acid rain, NOx, SOx, organics). 
Incomplete combustion of any fuel.
More on Sources of Pollutants 
Carbon Monoxide (CO) 
Any source that burns fuel such 
as automobiles, trucks, heavy 
construction equipment, farming 
equipment and residential 
heating.
More on Sources of Pollutants 
Sulfur Dioxide (SO2) 
Coal or Oil Burning 
Power Plants and 
Industries, Refineries, 
Diesel Engines
More on Sources of Pollutants 
Fine Particulate Matter (PM2.5) 
Fuel Combustion in Motor Vehicles, 
Equipment and Industrial Sources, 
Residential and Agricultural Burning. 
Also formed from reaction of other 
pollutants (acid rain, NOx, SOx, 
organics).
Atmospheric Pollution 
Acid Deposition
Acid Deposition 
Acid deposition is a general name 
for a number of phenomena, namely 
acid rain, acid fog and acid mist. 
This means it can imply both wet 
and dry (gaseous) precipitation. Acid 
deposition is a rather well 
known environmental problem, for 
example acid fog killed several 
thousand people in London in 1952.
Acid Deposition 
Acid deposition is concerned with long-range 
rather than local effects. Pollutants are mixed in 
the atmosphere and therefore usually cannot 
be attributed to any local source. Pollutants are 
generally more dispersed and of lower 
concentrations than local ground level 
pollutants.
Acid Deposition 
Acid deposition 
typically has a pH 
below 4, but this may 
be as low as 1.5 
under seriously acidic 
conditions. It primarily 
consists of two types 
of compounds, 
namely sulphuric acid 
(H2SO4) and nitric 
acid (HNO3).
Acid Deposition 
Sulphuric acid is 
formed by conversion 
of sulphur dioxide 
emitted from power 
stations, melting 
processes, home 
fires, car exhausts 
and other sources. It 
contributes about 
70% to the overall 
acidity of deposition. 
Reaction mechanism: 
SO3 + H2O -> H2SO4
Acid Deposition 
Nitric acid is formed 
from nitrogen oxide 
(NOx) emissions 
from fossil 
fuel combustion. It 
contributes about 
30% to the overall 
acidity of deposition. 
Reaction mechanism: 
NO2 + OH- -> HNO3
Atmospheric Pollution 
Impacts of Air Pollutants
Impacts of Air Pollutants 
The World Health 
Organization states that 2.4 
million people die each year 
from causes directly 
attributable to air pollution, 
with 1.5 million of these 
deaths attributable to indoor 
air pollution.
Impacts of Air Pollutants 
Because people are 
exposed to so many 
potentially dangerous 
pollutants, it is often hard to 
know exactly which 
pollutants are responsible 
for causing sickness. Also, 
because a mixture of 
different pollutants can 
intensify sickness, it is often 
difficult to isolate those 
pollutants that are at fault.
Impacts of Air Pollutants 
Many diseases could be 
caused by air pollution 
without their becoming 
apparent for a long 
time. Diseases such as 
bronchitis, lung cancer, and 
heart disease may all 
eventually appear in people 
exposed to air pollution.
Impacts of Air Pollutants 
Older people are highly vulnerable to 
diseases induced by air pollution. Those 
with heart or lung disorders are under 
additional risk. Children and infants are also 
at serious risk.
Impacts of Air Pollutants 
Air pollutants such as ozone, nitrogen 
oxides, and sulfur dioxide also have harmful 
effects on natural ecosystems. They can kill 
plants and trees by destroying their leaves, 
and can kill animals, especially fish in highly 
polluted rivers.
Atmospheric Pollution 
Bringing Air Pollution Under Control
Bringing Air Pollution Under Control 
Two main types of pollution control 
Input control involves preventing a 
problem before it occurs, or at least 
limiting the effects the process will 
produce. 
1
Bringing Air Pollution Under Control 
Two main types of pollution control 
Five major input control methods exist. People 
may try to restrict population growth, use less 
energy, improve energy efficiency, reduce 
waste, and move to non-polluting renewable 
forms of energy production. Also, automobile-produced 
pollution can be decreased with highly 
beneficial results. 
Clean Air Act
Bringing Air Pollution Under Control 
Two main types of pollution control 
Output control, the opposite method, 
seeks to fix the problems caused by air 
pollution. This usually means cleaning 
up an area that has been damaged by 
pollution. 
2
Bringing Air Pollution Under Control 
Two main types of pollution control 
Input controls are 
usually more effective 
than output 
controls. Output 
controls are also more 
expensive, making them 
less desirable to tax 
payers and polluting 
industries.
Atmospheric Pollution 
Coping with Acid Deposition
Coping with Acid Deposition 
Short Term Method 
Liming (calcium hydroxide) is one of the very 
few ways to reduce the effects of acid rain. 
This can only be a short-term method as 
liming requires to be done regularly and that 
will prove to be very costly. The only way to 
stop acid rain is to reduce the amount of 
acidic oxides released into the air.
Coping with Acid Deposition 
Long Term Method 
1. Reducing the use of fossil 
fuels by using more public 
transport and practicing 
carpooling and using less of 
cars but more of walking 
and bicycles. 
2. Using fossil fuels of low 
sulphur contents
Coping with Acid Deposition 
3. Extracting sulphur from the 
existing fossil fuels before 
using them. However, this 
method might not be very 
feasible, as it is very costly 
to do so, especially at a 
large scale. 
Long Term Method
Coping with Acid Deposition 
4. Using pollution control 
equipment such as catalytic 
converters in vehicles and 
scrubbers in factories and 
power stations and also 
using the method of 
desulphurisation. 
Long Term Method
Atmospheric Pollution 
Unresolved 
Issues
Unresolved Issues
Unresolved Issues 
• Expanded use of emissions trading for 
pollutants other than SO2 ; 
• The use and control of fuel additives, 
including methyl tertiary butyl ether (MTBE); 
• Sulfur removal from gasoline and diesel fuel; 
• The interstate transport of NOx emissions; 
• Regional haze; and 
• Automobile emissions, especially issues concerning 
the “right-to-know” and hazardous emissions from 
coal-fired electric power plants.
Total World Electricity Generation 
Source: IEA 2008 
*Other includes solar, wind, combustible renewables, geothermal & waste
Unresolved Issues 
Two broader policy issues that the nation must 
deal with are: 
1. The role of the developed and 
developing nations in the control of 
emissions of global warming 
gases; and 
2. The extent to which the 
environment will be protected from 
the effects of the deregulation of 
the electric power generating 
industry.
When I was a kid, we never heard of 
smog, ozone depletion, acid rain, 
green house gasses. 
- Dennis Weaver
It's absolutely stupid that we live 
without an ozone layer. We have 
men, we've got rockets, we've got 
saran wrap – FIX IT! 
- Lewis Black
From a scientific perspective there is 
some indication that a nuclear war could 
deplete the earth's ozone layer or, less 
likely, could bring on a new Ice Age - but 
there is no suggestion that either the 
created order or mankind would be 
destroyed in the process. 
- Herman Khan
So I'm going to go on and work on 
preserving the ozone layer, encouraging 
everyone to recycle. 
- Dean Stockwell
Thank You 
for 
Listening! 
Jovannie Espinosa 
& 
Markleen Guimbao

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The Atmosphere: Climate, Climate Change and Ozone Depletion

  • 1. The Atmosphere: Climate, Climate Change & Ozone Depletion Reporters: Jovannie Espinosa & Markleen Guimbao
  • 2. Earth’s Atmosphere The Earth's atmosphere is more than just the air we breathe. It's also a buffer that keeps us from being peppered by meteorites, a screen against deadly radiation, and the reason radio waves can be bounced for long distances around the planet.
  • 3. Earth’s Atmosphere Troposphere The lowest is the troposphere, which is the layer that provides most of our weather. It contains about four-fifths of the Earth's air, but extends only to a height of about 11 miles (17 kilometers) at the Equator and somewhat less at the Poles.
  • 4. Earth’s Atmosphere Stratosphere Above the troposphere is the stratosphere. It extends to a height of about 30 miles (50 kilometers) and includes the ozone layer, which blocks much of the sun's harmful ultraviolet rays. It is warmer than the troposphere because of the energy from the ultraviolet light absorbed by the ozone.
  • 5. Earth’s Atmosphere Stratosphere Greenhouse Effect, the capacity of certain gases in the atmosphere to trap heat emitted from Earth’s surface, thereby insulating and warming the planet. Without the thermal blanketing of the natural greenhouse effect, Earth’s climate would be about 33°C (about 59°F) cooler—too cold for most living organisms to survive.
  • 6. Earth’s Atmosphere Mesosphere In this layer, the air temperature drops again, down to nearly -180 degrees Fahrenheit (-120 degrees Celsius) at the top. Meteors generally burn up in the mesosphere, which extends to a height of about 52 miles (85 kilometers). This is why the Earth's surface isn't pocked with meteor craters, like the moon's.
  • 7. Earth’s Atmosphere Ionosphere It extends to about 430 miles (690 kilometers) and is so thin it's generally considered part of outer space. The International Space Station and many satellites orbit within the ionosphere. It is named for the ions created within this layer by energetic particles from sunlight and outer space. These ions create an electrical layer that reflects radio waves, allowing radio messages to be sent across oceans in the days before communication satellites.
  • 8. Earth’s Atmosphere Exosphere This tenuous portion of the Earth's atmosphere extends outward until it interacts with the solar wind. Solar storms compress the exosphere. When the sun is tranquil, this layer extends further outward. Its top ranges from 620 miles (1,000 kilometers) to 6,214 miles (10,000 kilometers) above the surface, where it merges with interplanetary space.
  • 9. Weather Weather is the state of the atmosphere at a specific time and place, with respect to temperature, precipitation, and other factors such as cloudiness.
  • 10. Weather Weather is generated by many forces, some obvious, some not. Warm, humid air masses blowing in from oceans, for example, fuel rains. Sunlight heats the land, generating thermals that help produce summer thunderstorms.
  • 11. Weather Mountains and cities also affect the weather. In mountains this occurs because the wind must rise as it crosses over the ridge. This lifts the air, causing it to cool. That produces clouds, rain, or snow.
  • 12. Weather Cities, on the other hand, produce urban "heat islands" where roads, parking lots, and rooftops warm in the sun. This not only raises the city's temperature, but it can affect the weather, producing thunderstorms in some cities or altering storm tracks in others.
  • 13. Climate Climate isn't the same thing as weather. Weather is the condition of the atmosphere over a short period of time; climate is the average course of weather conditions for a particular location over a period of many years.
  • 14. Climate One of the factors that influences climate is the angle of the sun's rays. In the tropics, between 23.5° N and 23.5° S, there is at least one time of year when the noontime sun is directly overhead and its rays hit at a direct angle. This produces a hot climate with relatively small temperature differences between summer and winter.
  • 15. Climate Climate is also controlled by wind, oceans, and mountains.
  • 17. Global Climate Change Global Warming or Climate Change is a measurable increase in the average temperature of Earth’s atmosphere, oceans, and landmasses.
  • 18. Global Climate Change Scientists believe that the Earth is currently facing a period of rapid warming brought on by rising levels of heat-trapping gases, known as greenhouse gases, in the atmosphere.
  • 19. Global Climate Change Since the beginning of the Industrial Revolution in the mid-1700s, however, human activities have added more and more of these gases into the atmosphere.
  • 21. Response to Climate Change The first time climate change was recognized as a serious problem by an international gathering was in 1979. The First World Climate Conference, held in February of that year, was a major scientific meeting. It issued a declaration calling on the world's governments "to foresee and prevent potential man-made changes in climate that might be adverse to the well-being of humanity."
  • 22. Response to Climate Change A large number of international conferences on climate change have been convened since then. Attended by policy-makers, government leaders, and scientists, they have addressed both scientific and policy issues.
  • 23. Response to Climate Change In 1985 the Vienna Convention for the Protection of the Ozone Layer was adopted. In 1987 a protocol under the Vienna Convention, known as the Montréal Protocol, was signed and later ratified by 36 nations, including the United States.
  • 24. Response to Climate Change The Second World Climate Conference, held in 1990 in Geneva, was a particularly crucial step towards a binding global convention on climate change. Some of these meetings have taken place under the auspices of the United Nations and its specialized agencies. Others have been held within regional for a such as the European Community, the Commonwealth, and the South Pacific Forum.
  • 25. Response to Climate Change The December 1997 summit on global warming in Kyōto, Japan, which included representatives from the United States, the European Union (EU), and many developing nations, reached an agreement for reducing emissions of gases that many scientists believe may lead to global warming and depletes ozone layer.
  • 26. Depletion of the Ozone Layer
  • 27. Ozone Layer Depletion The term "Ozone Layer" is used to describe the ozone molecules present in the stratosphere. The ozone layer stretches around the entire globe of the Earth like a bubble, filtering out harmful ultraviolet radiation from the sun. Destruction of the ozone layer increases the amount of ultraviolet radiation reaching the earth which can cause severe effects on human health and the environment.
  • 29. Ozone Layer Depletion What is Ozone Layer Depletion? Ozone layer depletion is destruction of the upper atmospheric layer of ozone gas, caused by substances formed from breakdown of ozone depleting substances. The main cause of this is the release of chlorofluorocarbon (CFC).
  • 30. Ozone Layer Depletion Chlorofluorocarbons or CFC’s are created and used in refrigerators and air conditioners. These are not harmful to humans and have been a benefit to us. Once released into the atmosphere, CFC’s are bombarded and destroyed by ultraviolet rays. In the process chlorine is released to destroy the ozone molecules.
  • 31. Ozone Layer Depletion Destruction of ozone by chlorine
  • 33. Ozone Layer Depletion NASA (2006) says ozone layer hole 5th biggest on record… at a size of about 27.4 million square kilometres (size of North America). http://www.cbc.ca/news/world/story/2008/11/05/ozone-hole.html
  • 35. Air Pollution Essentials Atmospheric pollution (also commonly called air pollution) is derived chiefly from the spewing of gasses and solid particulates into the atmosphere. Many pollutants occur naturally, but most air pollution is caused by human activity.
  • 36. Air Pollutants – General Overview A substance in the air that can cause harm to humans and the environment is known as an air pollutant. Pollutants can be in the form of solid particles, liquid droplets, or gases.
  • 37. Air Pollutants – General Overview Pollutants can be classified as primary or secondary. Usually, primary pollutants are directly emitted from a process, such as ash from a volcanic eruption, the carbon monoxide gas from a motor vehicle exhaust or sulfur dioxide released from factories. Secondary pollutants are not emitted directly. Rather, they form in the air when primary pollutants react or interact.
  • 38. Air Pollutants – General Overview An important example of a secondary pollutant is ground level ozone — one of the many secondary pollutants that make up photochemical smog. Some pollutants may be both primary and secondary: that is, they are both emitted directly and formed from other primary pollutants.
  • 39. Atmospheric Pollution Major Air Pollutants & Their Sources In the last 200 years or so there appeared several fundamental trends which became the major forces behind the surge in levels of air pollution throughout the globe. These are: • Industrialization • Population Growth • Globalization
  • 40. Major Air Pollutants Industrialization Among other things, industrialization set in motion the widespread use of fossil fuels (oil, gas & coal) which are now the main pollution sources.
  • 41. Major Air Pollutants Population Growth With population numbers literally exploding around the world, the demand for food and other goods goes up. This demand is met by expanded production and use of natural resources, which in its turn leads to higher levels of environmental pollution in general, and air pollution in particular.
  • 42. Major Air Pollutants Globalization Globalization has become an effective facilitator of air pollution. Developing countries usually have much looser laws on environmental protection. With this “benefit” as well as the population growth and easy availability of cheap labor, big industry prefers to move its facilities to such “pollution havens” rather than work in more regulated markets.
  • 43. Atmospheric Pollution More on Sources of Pollutants Ozone (03) Formed when reactive organic gases (ROG) and nitrogen oxides react in the presence of sunlight. ROG sources include any source that burns fuels, (e.g., gasoline, natural gas, wood, oil) solvents, petroleum processing and storage and pesticides.
  • 44. More on Sources of Pollutants Respirable Particulate Matter (PM10) Road Dust, Windblown Dust (Agriculture) and Construction (Fireplaces). Also formed from other pollutants (acid rain, NOx, SOx, organics). Incomplete combustion of any fuel.
  • 45. More on Sources of Pollutants Carbon Monoxide (CO) Any source that burns fuel such as automobiles, trucks, heavy construction equipment, farming equipment and residential heating.
  • 46. More on Sources of Pollutants Sulfur Dioxide (SO2) Coal or Oil Burning Power Plants and Industries, Refineries, Diesel Engines
  • 47. More on Sources of Pollutants Fine Particulate Matter (PM2.5) Fuel Combustion in Motor Vehicles, Equipment and Industrial Sources, Residential and Agricultural Burning. Also formed from reaction of other pollutants (acid rain, NOx, SOx, organics).
  • 49. Acid Deposition Acid deposition is a general name for a number of phenomena, namely acid rain, acid fog and acid mist. This means it can imply both wet and dry (gaseous) precipitation. Acid deposition is a rather well known environmental problem, for example acid fog killed several thousand people in London in 1952.
  • 50. Acid Deposition Acid deposition is concerned with long-range rather than local effects. Pollutants are mixed in the atmosphere and therefore usually cannot be attributed to any local source. Pollutants are generally more dispersed and of lower concentrations than local ground level pollutants.
  • 51. Acid Deposition Acid deposition typically has a pH below 4, but this may be as low as 1.5 under seriously acidic conditions. It primarily consists of two types of compounds, namely sulphuric acid (H2SO4) and nitric acid (HNO3).
  • 52. Acid Deposition Sulphuric acid is formed by conversion of sulphur dioxide emitted from power stations, melting processes, home fires, car exhausts and other sources. It contributes about 70% to the overall acidity of deposition. Reaction mechanism: SO3 + H2O -> H2SO4
  • 53. Acid Deposition Nitric acid is formed from nitrogen oxide (NOx) emissions from fossil fuel combustion. It contributes about 30% to the overall acidity of deposition. Reaction mechanism: NO2 + OH- -> HNO3
  • 54. Atmospheric Pollution Impacts of Air Pollutants
  • 55. Impacts of Air Pollutants The World Health Organization states that 2.4 million people die each year from causes directly attributable to air pollution, with 1.5 million of these deaths attributable to indoor air pollution.
  • 56. Impacts of Air Pollutants Because people are exposed to so many potentially dangerous pollutants, it is often hard to know exactly which pollutants are responsible for causing sickness. Also, because a mixture of different pollutants can intensify sickness, it is often difficult to isolate those pollutants that are at fault.
  • 57. Impacts of Air Pollutants Many diseases could be caused by air pollution without their becoming apparent for a long time. Diseases such as bronchitis, lung cancer, and heart disease may all eventually appear in people exposed to air pollution.
  • 58. Impacts of Air Pollutants Older people are highly vulnerable to diseases induced by air pollution. Those with heart or lung disorders are under additional risk. Children and infants are also at serious risk.
  • 59. Impacts of Air Pollutants Air pollutants such as ozone, nitrogen oxides, and sulfur dioxide also have harmful effects on natural ecosystems. They can kill plants and trees by destroying their leaves, and can kill animals, especially fish in highly polluted rivers.
  • 60. Atmospheric Pollution Bringing Air Pollution Under Control
  • 61. Bringing Air Pollution Under Control Two main types of pollution control Input control involves preventing a problem before it occurs, or at least limiting the effects the process will produce. 1
  • 62. Bringing Air Pollution Under Control Two main types of pollution control Five major input control methods exist. People may try to restrict population growth, use less energy, improve energy efficiency, reduce waste, and move to non-polluting renewable forms of energy production. Also, automobile-produced pollution can be decreased with highly beneficial results. Clean Air Act
  • 63. Bringing Air Pollution Under Control Two main types of pollution control Output control, the opposite method, seeks to fix the problems caused by air pollution. This usually means cleaning up an area that has been damaged by pollution. 2
  • 64. Bringing Air Pollution Under Control Two main types of pollution control Input controls are usually more effective than output controls. Output controls are also more expensive, making them less desirable to tax payers and polluting industries.
  • 65. Atmospheric Pollution Coping with Acid Deposition
  • 66. Coping with Acid Deposition Short Term Method Liming (calcium hydroxide) is one of the very few ways to reduce the effects of acid rain. This can only be a short-term method as liming requires to be done regularly and that will prove to be very costly. The only way to stop acid rain is to reduce the amount of acidic oxides released into the air.
  • 67. Coping with Acid Deposition Long Term Method 1. Reducing the use of fossil fuels by using more public transport and practicing carpooling and using less of cars but more of walking and bicycles. 2. Using fossil fuels of low sulphur contents
  • 68. Coping with Acid Deposition 3. Extracting sulphur from the existing fossil fuels before using them. However, this method might not be very feasible, as it is very costly to do so, especially at a large scale. Long Term Method
  • 69. Coping with Acid Deposition 4. Using pollution control equipment such as catalytic converters in vehicles and scrubbers in factories and power stations and also using the method of desulphurisation. Long Term Method
  • 72. Unresolved Issues • Expanded use of emissions trading for pollutants other than SO2 ; • The use and control of fuel additives, including methyl tertiary butyl ether (MTBE); • Sulfur removal from gasoline and diesel fuel; • The interstate transport of NOx emissions; • Regional haze; and • Automobile emissions, especially issues concerning the “right-to-know” and hazardous emissions from coal-fired electric power plants.
  • 73. Total World Electricity Generation Source: IEA 2008 *Other includes solar, wind, combustible renewables, geothermal & waste
  • 74. Unresolved Issues Two broader policy issues that the nation must deal with are: 1. The role of the developed and developing nations in the control of emissions of global warming gases; and 2. The extent to which the environment will be protected from the effects of the deregulation of the electric power generating industry.
  • 75. When I was a kid, we never heard of smog, ozone depletion, acid rain, green house gasses. - Dennis Weaver
  • 76. It's absolutely stupid that we live without an ozone layer. We have men, we've got rockets, we've got saran wrap – FIX IT! - Lewis Black
  • 77. From a scientific perspective there is some indication that a nuclear war could deplete the earth's ozone layer or, less likely, could bring on a new Ice Age - but there is no suggestion that either the created order or mankind would be destroyed in the process. - Herman Khan
  • 78. So I'm going to go on and work on preserving the ozone layer, encouraging everyone to recycle. - Dean Stockwell
  • 79. Thank You for Listening! Jovannie Espinosa & Markleen Guimbao

Hinweis der Redaktion

  1. Nox – nirogen oxides; Sox – sulphur oxides
  2. The pH scale measures how acidic or basic a substance is. It ranges from 0 to 14. A pH of 7 is neutral. A pH less than 7 is acidic, and a pH greater than 7 is basic. 
  3. Catalytic converter is a device in the exhaust system of a motor vehicle, containing a catalyst for converting pollutant gases into less harmful ones.
  4. Emissions trading is a market-based approach used to control pollution by providing economic incentives for achieving reductions in the emissions of pollutants. Regional haze has reduced scenic views in national parks and wilderness areas.