planetary atmospheres, the environment and life (excos2y) topic 9: climate change chris parkes rm...
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Planetary Atmospheres, the Environment and Life (ExCos2Y)
Topic 9: Climate Change
Chris Parkes
Rm 455 Kelvin Building
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8. Storm systems
• Storm Systems– Hurricanes
• Formation• Structure
– Tornados• Formation
– Dust Devils, Water Spouts
Revision
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Climate Change
• Many forms discussed in lectures:
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Earth’s Long-Term Future Climate • Remained suitable for life for 4 billion years
– Feedback mechanisms
• Sun will continue to warm– Life on Earth ultimately doomed– Loose water > 1 billion years from now– CO2 cycle may provide regulation for longer– Life < 4 billion years
• Earth will become like venus– 1to 4 billion years
– More pressing worries….
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Climate Conditions for Human Life
Planets geology and biology:
• Pressure, Temperature – liquid water
• Oxygen – right amount in atmosphere
• Ozone Layer – absorbs UV
• Magnetospheres – deflects solar wind
Human Effects:
• Ozone depletion – now correcting
• Extinction of species
• Global warming
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Global warming
• Temperature increased by 0.5o in last 50 years
• Burning fossil fuels adds CO2 to atmosphere
– Concentration significantly higher than in 600,000 years
• Greenhouse mechanism well understood
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Global Warming• Effects on climate dependent on feedback
mechanisms– Temperature rise leads to more water evaporation– Water vapour acts as greenhouse gas
• increases temperature
– Water vapour forms clouds, reflect more• decreases temperature
– Temperature rise melts ice– Ice highly reflective, water highly absorbsant
• Increases temperature• And raises sea levels – flooding
• Effects on Forests, Eco-systems:– food production, fresh water
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Potential Effects of Global temperature rise
• Glacial Retreat
• Arctic Shrinkage
• Sea Level rise
• Change in ocean currents
• More Intense Hurricanes /extreme weather events
• Changes in eco-systems
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Glacier melting / ice caps / lakes
• Retreats of glaciers
World Glacier Monitoring Service
1973 2006
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Sea level
• Melting glacier ice gives sea rise– Melting sea ice
does not (as floating)
Contributes further to global warming through albedo
Potential for flooding major areas of population
Predictions IPCC
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Fossil CO2 emissions
Global yearly consumption (BP 2008)
0
5,000
10,000
15,000
20,000
25,000
30,000
35,000
1965 1970 1975 1980 1985 1990 1995 2000 2005
CO
2 em
issi
ons
(mill
ion
tonn
es)
Oil: emissions
Natural gas: emissions
Coal: emissions
Total emissions
CDIAC total fossil emissions
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Climate change in the past
Source T. Stocker 2005
2009 385 ppm(380 ppm in 2007, 330 ppm in 1974)
(Can extend graph to 850'000, T. Stocker 2006)
Homo Sapiens appears
Agriculture begins
Ice Core Data – gives temperature from heavy water (deuterium D)CO2 levels – high correlation
Deuterium=Temperature
CO2
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Climate change in the present
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Quality of climate models
• Reasonable agreement of models and measured temperatures over past data
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Projections
• Range of climate models• Assuming no special action taken
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Example exam questions
Q1. What are the potential Effects of Global Warming ?
Q2. How do we obtain long time scale data on previous CO2 levels and temperatures ?
Q3. How does global warming and changes in the Earth’s albedo interact ?
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