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Index
Introduction
History
Green house gases
Global Warming Impacts
Control
Global Warming
An average increase in the
 temperature of the
 atmosphere near the Earth’s
 surface and in the
 troposphere, which can
 contribute to changes in
 global climate patterns
• Since the late 1800’s, the global average
  temperature has increased about 0.7 to
  1.4 degrees.

• The concentration of green house gases in
  the atmosphere were artificially raised by
  humans since past 250 years.
Green house effect:
         How does it work
The greenhouse effect insulates
 earth, resulting in the mild temperatures at
 the earth's surface that have allowed life to
 flourish.

The greenhouse effect is absolutely vital to
 allowing life, as we know it to survive on
 earth. Without the greenhouse effect, earth
 would be a cold planet, with a mean surface
 temperature well below freezing.
Main Warming Mechanism:
        The Greenhouse Effect
Our earth receives most of its energy in the form
 of radiation from the sun
The incoming solar energy (Ultra Violet UV) has
 a very short wavelength and passes through the
 atmospheric gases unaffected to reach the earth
 surface
The earth surface absorbs the solar energy and
 releases it back to the atmosphere at a different
 wavelength as infrared (IR) radiation, some of
 which goes back into space
Some of the IR radiation emitted by the earth
 is absorbed by greenhouse gases in the
 atmosphere.

These gases absorb the infrared radiation
 emitted by the earth and re-radiate the
 energy as heat back towards the earth
 causing a warming known as the greenhouse
 effect.
Present Day Climate Change:

In the history of earth, climate change
 happened many times.
Ones more in the history of the
 earth, the climate is changing.

There is however several differences
 between past changes in the climate
 and what we are observing today:
 - Present climate change is occurring very rapidly as
  opposed to past climate changes which usually
  occurs over millions of years (rapid change have
  occurred in the past but has a result of catastrophic
  events only e.g. meteorite impact, large volcanic
  eruptions, sudden feedback)

 - Present day climate change is not a natural event
  but a result of human activity

 - Present day climate change can be prevented as we
  do know the causes and how to limit the impacts
Brief History Of The Earth Climate:
          Natural Variability
 The Earth is a very dynamic planet which
 has undergone many transformations
 throughout its history and since its
 formation 4.6 billion years ago.

A succession of geological events and the
 appearance of life have dramatically
 influenced the climate of the earth.
History
The field of Paleoclimatology has
 provided information of climate change
 in the ancient past, supplementing
 modern observations of climate.

Climate variability usually occurs
 naturally on the planet over millions of
 years or suddenly as a result of a
 catastrophic event (e.g. major volcanic
 eruptions, meteor impacts).
Few Examples
Miocene Climate: (23–15 MYA)
   The climate during which was warmer than today's
   climate.


Early Cretaceous Climate: (145-65 MYA)
  The Early Cretaceous was a mild "Ice House" world.


Early & Middle Jurassic Climate: (206-144 MYA)
  Deserts covered what is now the Amazon and Congo
   rainforests.
History

Late Devonian Climate: (360 MYA)
  Thick coals formed for the first time in the tropical
   rainforests.


Early Permian Climate: (280 MYA)
  Much of the Southern Hemisphere was covered by
   ice as glaciers pushed northward.
Example Of A Warmer Climate:
Early & Middle Jurassic Climate
(206 To 144 Million Years Ago)

  The Jurassic is an example of a climate era
   which was much warmer than the climate
   that we are experiencing today.

  Much of the Jurassic world was warm and
   moist, with a greenhouse climate.
Early & Middle Jurassic
         Climate

The polar areas were ice-free during
 this period.
The ocean surface stood at a higher
 level with respect to the continents.
Much of the earth was covered in warm
 and moist tropical forest
Example Of A Colder Climate: The
Ordovician Climate (488 To 444 Million
              Years Ago)

The Ordovician is an example of a past climate
 which was much colder than the climate that we
 are experiencing today
Great Ice Age that gripped the earth at this
 time.
There were even glaciers in what is now the
 Sahara.
About 60% of animal genera became extinct,
Carbon dioxide (CO2)
Methane (CH4)
Nitrous oxide (N2O)
Chlorofluorocarbon (CFC)
Water vapour (H2O)
Carbon dioxide :
 It is generated by the human
  activities like burning of
  coal, wood, natural gas.oil
  etc.
 It is also released by animals
  & human beings during the
  process of respiration.
 The trees take in the carbon
  dioxide, therefore
  deforestation is also an
  important reason for increase
  in carbon dioxide.
 It accounts for 50% of the
  gases responsible for global
  warming.
METHANE

           Methane accounts for
            16% of all gases
            responsible for global
            warming .
           It is estimated that nearly
            30 to 200 million tones of
            methane is released
            every year.
           The main source of
            methane is rice field.
NITROUS OXIDE



          It is generated due to burning
           of
           biomass, agriculture, livestock
           waste, nitrogen rich fuels.

          It accounts for 6% of the gases
           responsible for global warming.
Chlorofluorocarbon [CFC]



   It accounts for nearly 20% of the gases
    responsible for global warming.
   These are non-toxic, nonflammable & highly
    stable compounds.
   They are also used as coolants in compressors of
    air conditioners & refrigerators.
   They are also use in insulators, fire extinguishers,
    aerosol etc.
Gas                       Major Source                     %
                                                                 Contri
                                                                 bution
   Carbon dioxide            Fossil fuel & deforestation          50


      Methane                Fossil fuel, wood burning.           16




   Nitrogen Oxide       Wood burning, fertilizer, fossil fuel.    06




Chlorofluro carbons &   Industries, insulation, refrigeration.    20
    other carbon
What’s the proof that
global warming is taking
         place?
Portage Glacier
    Alaska




                         1914                                                   2004


Photos: NOAA Photo Collection and Gary Braasch – WorldViewOfGlobalWarming.org
Colorado River
Arizona




   June 2002          Dec 2003
Ocean
                    Life
       Living
                               Habitat
       Plants


                 Impact of
                    rise in
  CO2
Emission        temperature           Weather
                 of 1.8oC to
                      4oC

       Crops                   Sea level

                   Human
                   Health
Effects of Global Warming
  Rising Sea Level     Increased Temperature




  Habitat Damage and
  Species Affected     Changes in Water Supply
Effects Of
                       Global
                     Warming




Human     Plants &                 Human    Marine
          Animals    Agriculture
Society                            Beings    Life
On human Society:
• Siberia & Canada might experience
  increase in temperature from 10 to 12
  degrees.

• The rainfall have increased by 2 to 3%
  per decade over tropical regions due to
  high rate of evaporation.
On Plants & Animals:
• Slowly disappearing & eventually die if
  the current trend in global warming
  countries.

• There are rapid rise in global temperature
  in next 100 years

• The wetland & coral reef may also
  undergo decline due to climatic changes
On Agriculture:
• There may be negative effect on various
  type of crop in different regions of the
  world.
• Soil moisture may decrease, water
  requirement of the crop will increase &
  will affect the crop yield.
• Due to Green house effect, several plants
  cripple down their size, fruits & leaves.
On Human Health:
•   It may lead to changes in rainfall
    pattern & some areas may
    become breeding ground for
    mosquitoes & some other insects
    which are vector of disease like
    malaria, dengue fever, yellow
    fever, etc.

•   In low rainfall there will be
    waterborne disease.

•   Heat waves are harmful to
    health.
On Ocean Life:
• It is estimated that there will be rise in
  sea level by 20 to30 cm by 2030.
• Due to increase in the temperature, the
  water expands & require more space.
• It also occur as a result of melting of
  glacier.
• Due to global warming the ice extent &
  snow cover have decreased.
• Scientists use information from several
  sources to analyze global warming that
  occurred before people began to use
  thermometers.
• Computers help climatologists to analyze
  past climate change & predict the future
  changes.
Measures on controlling the problem



Government

 * Set some laws to limit the amount of
 pollutants produced by factories

 * Develop the skills of using
 renewable fuels, e.g. solar energy,
 wind energy
Measures on controlling the problem
   * Encourage the factories to replace fossil
    fuels by renewable fuels, which would not
    cause environmental pollution

   * Carry out energy saving scheme →
    reduce the pollution produced by burning
    fossil fuels

   * Planting more plants → reduce the
    pollutants e.g. CO2
What’s being done now to
   reduce our emissions?




Wind Power   Solar Power   Fuel-Efficiency
Measures on controlling the problem
Citizens

* Reduce the use of plastic bags → as
 degradation of plastic emit CH4

* Recycle the resources, e.g. plastic

* Reduce the use of sprays → as CFCs would
 be emitted out
Measures on controlling the problem

* Reduce the use of air-conditioner, which will
  emit CFCs

* Use public transportation instead of
  private cars → reduce the pollutants emitted
  by cars
Global warming
Global warming
Global warming
Global warming
Global warming
Global warming
Global warming
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Global warming

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Global warming

  • 1.
  • 3. Global Warming An average increase in the temperature of the atmosphere near the Earth’s surface and in the troposphere, which can contribute to changes in global climate patterns
  • 4. • Since the late 1800’s, the global average temperature has increased about 0.7 to 1.4 degrees. • The concentration of green house gases in the atmosphere were artificially raised by humans since past 250 years.
  • 5. Green house effect: How does it work The greenhouse effect insulates earth, resulting in the mild temperatures at the earth's surface that have allowed life to flourish. The greenhouse effect is absolutely vital to allowing life, as we know it to survive on earth. Without the greenhouse effect, earth would be a cold planet, with a mean surface temperature well below freezing.
  • 6. Main Warming Mechanism: The Greenhouse Effect Our earth receives most of its energy in the form of radiation from the sun The incoming solar energy (Ultra Violet UV) has a very short wavelength and passes through the atmospheric gases unaffected to reach the earth surface The earth surface absorbs the solar energy and releases it back to the atmosphere at a different wavelength as infrared (IR) radiation, some of which goes back into space
  • 7. Some of the IR radiation emitted by the earth is absorbed by greenhouse gases in the atmosphere. These gases absorb the infrared radiation emitted by the earth and re-radiate the energy as heat back towards the earth causing a warming known as the greenhouse effect.
  • 8.
  • 9. Present Day Climate Change: In the history of earth, climate change happened many times. Ones more in the history of the earth, the climate is changing. There is however several differences between past changes in the climate and what we are observing today:
  • 10.  - Present climate change is occurring very rapidly as opposed to past climate changes which usually occurs over millions of years (rapid change have occurred in the past but has a result of catastrophic events only e.g. meteorite impact, large volcanic eruptions, sudden feedback)  - Present day climate change is not a natural event but a result of human activity  - Present day climate change can be prevented as we do know the causes and how to limit the impacts
  • 11. Brief History Of The Earth Climate: Natural Variability  The Earth is a very dynamic planet which has undergone many transformations throughout its history and since its formation 4.6 billion years ago. A succession of geological events and the appearance of life have dramatically influenced the climate of the earth.
  • 12. History The field of Paleoclimatology has provided information of climate change in the ancient past, supplementing modern observations of climate. Climate variability usually occurs naturally on the planet over millions of years or suddenly as a result of a catastrophic event (e.g. major volcanic eruptions, meteor impacts).
  • 13. Few Examples Miocene Climate: (23–15 MYA)  The climate during which was warmer than today's climate. Early Cretaceous Climate: (145-65 MYA) The Early Cretaceous was a mild "Ice House" world. Early & Middle Jurassic Climate: (206-144 MYA) Deserts covered what is now the Amazon and Congo rainforests.
  • 14. History Late Devonian Climate: (360 MYA) Thick coals formed for the first time in the tropical rainforests. Early Permian Climate: (280 MYA) Much of the Southern Hemisphere was covered by ice as glaciers pushed northward.
  • 15. Example Of A Warmer Climate: Early & Middle Jurassic Climate (206 To 144 Million Years Ago) The Jurassic is an example of a climate era which was much warmer than the climate that we are experiencing today. Much of the Jurassic world was warm and moist, with a greenhouse climate.
  • 16. Early & Middle Jurassic Climate The polar areas were ice-free during this period. The ocean surface stood at a higher level with respect to the continents. Much of the earth was covered in warm and moist tropical forest
  • 17. Example Of A Colder Climate: The Ordovician Climate (488 To 444 Million Years Ago) The Ordovician is an example of a past climate which was much colder than the climate that we are experiencing today Great Ice Age that gripped the earth at this time. There were even glaciers in what is now the Sahara. About 60% of animal genera became extinct,
  • 18. Carbon dioxide (CO2) Methane (CH4) Nitrous oxide (N2O) Chlorofluorocarbon (CFC) Water vapour (H2O)
  • 19. Carbon dioxide :  It is generated by the human activities like burning of coal, wood, natural gas.oil etc.  It is also released by animals & human beings during the process of respiration.  The trees take in the carbon dioxide, therefore deforestation is also an important reason for increase in carbon dioxide.  It accounts for 50% of the gases responsible for global warming.
  • 20. METHANE  Methane accounts for 16% of all gases responsible for global warming .  It is estimated that nearly 30 to 200 million tones of methane is released every year.  The main source of methane is rice field.
  • 21. NITROUS OXIDE  It is generated due to burning of biomass, agriculture, livestock waste, nitrogen rich fuels.  It accounts for 6% of the gases responsible for global warming.
  • 22. Chlorofluorocarbon [CFC]  It accounts for nearly 20% of the gases responsible for global warming.  These are non-toxic, nonflammable & highly stable compounds.  They are also used as coolants in compressors of air conditioners & refrigerators.  They are also use in insulators, fire extinguishers, aerosol etc.
  • 23. Gas Major Source % Contri bution Carbon dioxide Fossil fuel & deforestation 50 Methane Fossil fuel, wood burning. 16 Nitrogen Oxide Wood burning, fertilizer, fossil fuel. 06 Chlorofluro carbons & Industries, insulation, refrigeration. 20 other carbon
  • 24.
  • 25.
  • 26. What’s the proof that global warming is taking place?
  • 27. Portage Glacier Alaska 1914 2004 Photos: NOAA Photo Collection and Gary Braasch – WorldViewOfGlobalWarming.org
  • 28. Colorado River Arizona June 2002 Dec 2003
  • 29. Ocean Life Living Habitat Plants Impact of rise in CO2 Emission temperature Weather of 1.8oC to 4oC Crops Sea level Human Health
  • 30. Effects of Global Warming Rising Sea Level Increased Temperature Habitat Damage and Species Affected Changes in Water Supply
  • 31. Effects Of Global Warming Human Plants & Human Marine Animals Agriculture Society Beings Life
  • 32. On human Society: • Siberia & Canada might experience increase in temperature from 10 to 12 degrees. • The rainfall have increased by 2 to 3% per decade over tropical regions due to high rate of evaporation.
  • 33. On Plants & Animals: • Slowly disappearing & eventually die if the current trend in global warming countries. • There are rapid rise in global temperature in next 100 years • The wetland & coral reef may also undergo decline due to climatic changes
  • 34. On Agriculture: • There may be negative effect on various type of crop in different regions of the world. • Soil moisture may decrease, water requirement of the crop will increase & will affect the crop yield. • Due to Green house effect, several plants cripple down their size, fruits & leaves.
  • 35. On Human Health: • It may lead to changes in rainfall pattern & some areas may become breeding ground for mosquitoes & some other insects which are vector of disease like malaria, dengue fever, yellow fever, etc. • In low rainfall there will be waterborne disease. • Heat waves are harmful to health.
  • 36. On Ocean Life: • It is estimated that there will be rise in sea level by 20 to30 cm by 2030. • Due to increase in the temperature, the water expands & require more space. • It also occur as a result of melting of glacier. • Due to global warming the ice extent & snow cover have decreased.
  • 37. • Scientists use information from several sources to analyze global warming that occurred before people began to use thermometers. • Computers help climatologists to analyze past climate change & predict the future changes.
  • 38. Measures on controlling the problem Government * Set some laws to limit the amount of pollutants produced by factories * Develop the skills of using renewable fuels, e.g. solar energy, wind energy
  • 39. Measures on controlling the problem * Encourage the factories to replace fossil fuels by renewable fuels, which would not cause environmental pollution * Carry out energy saving scheme → reduce the pollution produced by burning fossil fuels * Planting more plants → reduce the pollutants e.g. CO2
  • 40. What’s being done now to reduce our emissions? Wind Power Solar Power Fuel-Efficiency
  • 41. Measures on controlling the problem Citizens * Reduce the use of plastic bags → as degradation of plastic emit CH4 * Recycle the resources, e.g. plastic * Reduce the use of sprays → as CFCs would be emitted out
  • 42. Measures on controlling the problem * Reduce the use of air-conditioner, which will emit CFCs * Use public transportation instead of private cars → reduce the pollutants emitted by cars