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THE GREENHOUSE EFFECT © 2016 Paul Billiet ODWS
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Sunlight energy in the atmosphere
© 2016 Paul Billiet ODWS
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The layers of the atmosphere
The troposphere is the atmospheric part of the biosphere The stratosphere contains the ozone layer The stratosphere is also a zone of warm air that keeps a lid on the troposphere. The troposphere does not mix with the upper atmosphere © 2016 Paul Billiet ODWS
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The Greenhouse Effect © 2016 Paul Billiet ODWS
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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°C to +123°C © 2016 Paul Billiet ODWS
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The Greenhouse Gases H2O vapour CO2 CH4 NOx CFC
© 2016 Paul Billiet ODWS
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Infrared Absorption Spectra
© 2016 Paul Billiet ODWS
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The Greenhouse Gases Water vapour in the atmosphere is stable
The atmosphere is saturated CO2 levels are currently rising They have varied in the past Methane levels are increasing: as more cattle are farmed, as more paddy fields are planted, as permafrost melts NOx levels increase due to increased circulation of motor vehicles. © 2016 Paul Billiet ODWS
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