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GLOBAL WARMING © 2007 Paul Billiet ODWS

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

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Page 1: GLOBAL WARMING © 2007 Paul Billiet ODWSODWS. The Greenhouse Effect © Oceanworld 2005 Robert R Stewart

GLOBAL WARMING

© 2007 Paul Billiet ODWS

Page 2: GLOBAL WARMING © 2007 Paul Billiet ODWSODWS. The Greenhouse Effect © Oceanworld 2005 Robert R Stewart

The Greenhouse Effect

© Oceanworld 2005 Robert R Stewart

Page 3: GLOBAL WARMING © 2007 Paul Billiet ODWSODWS. The Greenhouse Effect © Oceanworld 2005 Robert R Stewart

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 ODWS

Page 4: GLOBAL WARMING © 2007 Paul Billiet ODWSODWS. The Greenhouse Effect © Oceanworld 2005 Robert R Stewart

The Main Greenhouse Gases

Water Vapor Carbon Dioxide Nitrogen Oxides Methane

© Oceanworld 2005 Robert R Stewart

© Text 2007 Paul Billiet ODWS

Page 5: GLOBAL WARMING © 2007 Paul Billiet ODWSODWS. The Greenhouse Effect © Oceanworld 2005 Robert R Stewart

Infrared Absorption Spectra

© Oceanworld 2005 Robert R Stewart

Page 6: GLOBAL WARMING © 2007 Paul Billiet ODWSODWS. The Greenhouse Effect © Oceanworld 2005 Robert R Stewart

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 ODWS

Page 7: GLOBAL WARMING © 2007 Paul Billiet ODWSODWS. The Greenhouse Effect © Oceanworld 2005 Robert R Stewart

Mauna Loa Observatory

© Mauna Loa Observatory Site

© Earth System Research Laboratory

© Earth System Research Laboratory

Page 8: GLOBAL WARMING © 2007 Paul Billiet ODWSODWS. The Greenhouse Effect © Oceanworld 2005 Robert R Stewart

Carbon dioxide a greenhouse gas

© Mauna Loa Observatory Site

Page 9: GLOBAL WARMING © 2007 Paul Billiet ODWSODWS. The Greenhouse Effect © Oceanworld 2005 Robert R Stewart

South Pole Data

Page 10: GLOBAL WARMING © 2007 Paul Billiet ODWSODWS. The Greenhouse Effect © Oceanworld 2005 Robert R Stewart

Samoa data

Page 11: GLOBAL WARMING © 2007 Paul Billiet ODWSODWS. The Greenhouse Effect © Oceanworld 2005 Robert R Stewart

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)

Page 12: GLOBAL WARMING © 2007 Paul Billiet ODWSODWS. The Greenhouse Effect © Oceanworld 2005 Robert R Stewart

Average temperature of Earth

Page 13: GLOBAL WARMING © 2007 Paul Billiet ODWSODWS. The Greenhouse Effect © Oceanworld 2005 Robert R Stewart
Page 14: GLOBAL WARMING © 2007 Paul Billiet ODWSODWS. The Greenhouse Effect © Oceanworld 2005 Robert R Stewart

Visual of the Little Ice Age 1500-1700’s

Page 15: GLOBAL WARMING © 2007 Paul Billiet ODWSODWS. The Greenhouse Effect © Oceanworld 2005 Robert R Stewart

Levels during the last ice age

© Dennis Hartmann: Universoty of Washington: Department of Atmospheric Sciences

Page 16: GLOBAL WARMING © 2007 Paul Billiet ODWSODWS. The Greenhouse Effect © Oceanworld 2005 Robert R Stewart

Earth during the Jurassic Period

Page 17: GLOBAL WARMING © 2007 Paul Billiet ODWSODWS. The Greenhouse Effect © Oceanworld 2005 Robert R Stewart

The oceanic conveyor belt

Page 18: GLOBAL WARMING © 2007 Paul Billiet ODWSODWS. The Greenhouse Effect © Oceanworld 2005 Robert R Stewart

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

Page 19: GLOBAL WARMING © 2007 Paul Billiet ODWSODWS. The Greenhouse Effect © Oceanworld 2005 Robert R Stewart

Is it really getting warmer – This is not what the debate is about.

1979 2003

© NASA

Page 20: GLOBAL WARMING © 2007 Paul Billiet ODWSODWS. The Greenhouse Effect © Oceanworld 2005 Robert R Stewart

The consequences Sea level rise – Melting ice caps

Flooding coastal areasReduced agricultural land

Displacement of populations Climate change

Displacement of ecosystemsChange in range of insect vectors of pathogensReduced biodiversity

© 2007 Paul Billiet ODWS

Page 21: GLOBAL WARMING © 2007 Paul Billiet ODWSODWS. The Greenhouse Effect © Oceanworld 2005 Robert R Stewart

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 ODWS

Page 22: GLOBAL WARMING © 2007 Paul Billiet ODWSODWS. The Greenhouse Effect © Oceanworld 2005 Robert R Stewart

What can be done?Reduce carbon emissions

Stop burning as much fossil fuel.

© 2007 Paul Billiet ODWS

Page 23: GLOBAL WARMING © 2007 Paul Billiet ODWSODWS. The Greenhouse Effect © Oceanworld 2005 Robert R Stewart

What can be done?

Increase natural processes that use up CO2 Reduce deforestation Increase reforestation

© 2007 Paul Billiet ODWS

Page 24: GLOBAL WARMING © 2007 Paul Billiet ODWSODWS. The Greenhouse Effect © Oceanworld 2005 Robert R Stewart

What can be done?

Artificial ways to reduce atmospheric CO2 are being researched.

Filter CO2 sources using hydroxide scrubbers

Injection of CO2 into deep ocean layersForms CO2 reservoirsImpact on sea life unknown

Injecting CO2 into disused oil wells

© 2007 Paul Billiet ODWS

Page 25: GLOBAL WARMING © 2007 Paul Billiet ODWSODWS. The Greenhouse Effect © Oceanworld 2005 Robert R Stewart

The bottom lineThere 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 ODWS

Page 26: GLOBAL WARMING © 2007 Paul Billiet ODWSODWS. The Greenhouse Effect © Oceanworld 2005 Robert R Stewart

Finally:Make your own decision

about what is going to happen and WHY the earth is getting warmer.

Page 27: GLOBAL WARMING © 2007 Paul Billiet ODWSODWS. The Greenhouse Effect © Oceanworld 2005 Robert R Stewart

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 ODWS

The Moai statues, Easter Island © Martin Gray, World Mysteries

Page 28: GLOBAL WARMING © 2007 Paul Billiet ODWSODWS. The Greenhouse Effect © Oceanworld 2005 Robert R Stewart

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 Department

© Text 2007 Paul Billiet ODWS

Page 29: GLOBAL WARMING © 2007 Paul Billiet ODWSODWS. The Greenhouse Effect © Oceanworld 2005 Robert R Stewart

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 ODWS

© Asociación Cultural Nueva Acrópolis en Barcelona

Page 30: GLOBAL WARMING © 2007 Paul Billiet ODWSODWS. The Greenhouse Effect © Oceanworld 2005 Robert R Stewart

The planet will look after itself in the end Greenland Viking colony AD982 – 1350 Cause: Deforestation,

soil degradation & cooling of the climate

© Emporia State University

© Text 2007 Paul Billiet ODWS

Page 31: GLOBAL WARMING © 2007 Paul Billiet ODWSODWS. The Greenhouse Effect © Oceanworld 2005 Robert R Stewart
Page 32: GLOBAL WARMING © 2007 Paul Billiet ODWSODWS. The Greenhouse Effect © Oceanworld 2005 Robert R Stewart

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Who’s next?

© NASA