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GLOBAL WARMING © 2007 Paul Billiet ODWSODWS. The Greenhouse Effect © Oceanworld 2005 Robert R Stewart.

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Presentation on theme: "GLOBAL WARMING © 2007 Paul Billiet ODWSODWS. The Greenhouse Effect © Oceanworld 2005 Robert R Stewart."— Presentation transcript:

1 GLOBAL WARMING © 2007 Paul Billiet ODWSODWS

2 The Greenhouse Effect © Oceanworld 2005 Robert R Stewart

3 The Greenhouse Effect The molecules of some gases in the atmosphere absorb heat energy and retain it This can be a good thing Without an atmosphere the Earth would have same temperature as the moon Moon mean surface temperature -46°C Moon temperature range: -233 to +123°C © 2007 Paul Billiet ODWSODWS

4 The Main Greenhouse Gases Water Vapor Carbon Dioxide Nitrogen Oxides Methane © Oceanworld 2005 Robert R Stewart © Text 2007 Paul Billiet ODWSODWS

5 Infrared Absorption Spectra © Oceanworld 2005 Robert R Stewart

6 The Greenhouse Gases Water vapor in the atmosphere is stable Carbon Dioxide levels are currently rising but they have been higher in the past Methane levels are increasing: Waste, cattle (manure), more rice paddy fields, as permafrost melts Nitrogen Oxide levels increase due to increased circulation of motor vehicles © 2007 Paul Billiet ODWSODWS

7 Mauna Loa Observatory © Mauna Loa Observatory Site © Earth System Research Laboratory Earth System Research Laboratory © Earth System Research LaboratoryEarth System Research Laboratory

8 Carbon dioxide a greenhouse gas © Mauna Loa Observatory Site

9 South Pole Data

10 Samoa data

11 Since the Industrial Revolution Concentration of Carbon Dioxide from trapped air measurements for the DE08 ice core near the summit of Law Dome, Antarctica. (Data measured by CSIRO Division of Atmospheric Research from ice cores supplied by Australian Antarctic Division)

12 Average temperature of Earth

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14 Visual of the Little Ice Age 1500-1700’s

15 Levels during the last ice age © Dennis Hartmann: Universoty of Washington: Department of Atmospheric Sciences

16 Earth during the Jurassic Period

17 The oceanic conveyor belt

18 The melting Arctic ice The length of the melt season inferred from surface temperature weekly data has been increasing by 9, 12, 12, and 17 days per decade in sea ice covered areas © NASA

19 Is it really getting warmer – This is not what the debate is about. 1979 2003 © NASA

20 The consequences Sea level rise – Melting ice caps Flooding coastal areas Reduced agricultural land Displacement of populations Climate change Displacement of ecosystems Change in range of insect vectors of pathogens Reduced biodiversity © 2007 Paul Billiet ODWSODWS

21 The consequences Increased rates of photosynthesis Increased agricultural production at high latitudes Amount of water vapor in the air will increase leading to more tropical-like ecosystems. © 2007 Paul Billiet ODWSODWS

22 What can be done? Reduce carbon emissions Stop burning as much fossil fuel. © 2007 Paul Billiet ODWSODWS

23 What can be done? Increase natural processes that use up CO 2 Reduce deforestation Increase reforestation © 2007 Paul Billiet ODWSODWS

24 What can be done? Artificial ways to reduce atmospheric CO 2 are being researched. Filter CO 2 sources using hydroxide scrubbers Injection of CO 2 into deep ocean layers Forms CO 2 reservoirs Impact on sea life unknown Injecting CO 2 into disused oil wells © 2007 Paul Billiet ODWSODWS

25 The bottom line There is NO debate, the earth is going through a warming phase. The question that no one seems to have an answer for and what the debate is about: 1. The earth is getting warmer due to burning fossil fuels. 2. The earth is getting warmer due to a natural warming trend. © 2007 Paul Billiet ODWSODWS

26 Finally: Make your own decision about what is going to happen and WHY the earth is getting warmer.

27 The planet will look after itself in the end Easter Island (Rapanui) in the Pacific Settled between AD900 and 1200 Community in severe decline AD 1700 Cause: excessive deforestation © Text 2007 Paul Billiet ODWSODWS The Moai statues, Easter Island © Martin Gray, World Mysteries

28 The planet will look after itself in the end Chaco Canyon, New Mexico Anasazi culture AD 850 – 1250 Cause: Deforestation combined with a decline in rainfall © New Mexico Tourism DepartmentNew Mexico Tourism Department © Text 2007 Paul Billiet ODWSODWS

29 The planet will look after itself in the end Mesopotamia Sumerian civilization 3100 – 1200 BC Increased salt levels in soil due to irrigation systems & arid environment Reduced food yield © Text 2007 Paul Billiet ODWSODWS © Asociación Cultural Nueva Acrópolis en BarcelonaAsociación Cultural Nueva Acrópolis en Barcelona

30 The planet will look after itself in the end Greenland Viking colony AD982 – 1350 Cause: Deforestation, soil degradation & cooling of the climate © Emporia State UniversityEmporia State University © Text 2007 Paul Billiet ODWSODWS

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32 forumpolitics.com/pics/earth-photo.jpg Who’s next? © NASA


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