Key Concepts
- The greenhouse effect is a natural process that produces a relatively warm environment near the earth's surface conducive to life on earth.
- The natural greenhouse effect is caused by greenhouse gases which occur naturally in the earth's atmosphere.
- The main natural greenhouse gases are carbon dioxide (CO2(g)), methane (CH4(g)), nitrous oxide (N2(g)O), and water (H2O(g)).
- The enhanced greenhouse effect is caused by human activities which release greenhouse gases into the atmosphere.
- The main anthropogenic, or human-induced, greenhouse gases are carbon dioxide (CO2(g)), nitrous oxide (N2O(g)), hydrofluorocarbons (HCFs), perfluorocarbons (PFCs), methane (CH4(g)) and sulfur hexafluoride (SF6(g)).
- The enhanced greenhouse effect is widely believed to be responsible for the increase in global temperatures seen in the 20th century (global warming).
Greenhouse Gases
Sources of greenhouse gases, the length of time they exist in the atmosphere, and the percentage of emissions they represent are shown in the table below:
| Gas Name |
Gas Symbol |
Common Sources |
Sinks |
Atmospheric Lifetime (years) |
% Emissions |
| carbon dioxide |
CO2 |
-combustion of fossil fuels -deforestation -gas flaring -cement production |
-photosynthesis -ocean surface |
5-200 |
60 |
|
| methane |
CH4 |
-landfills -production and distribution of natural gas and petroleum -fermentation from digestive system of livestock -rice cultivation -natural wetlands -combustion of fossil fuels |
-reaction with tropospheric hydroxyl (OH) -removal by soils |
12 |
20 |
|
| nitrous oxide |
N2O |
-combustion of fossil fuels -fertilizers manure -nylon production -biological sources in oceans and soils |
-removal by soils -stratospheric photolysis |
114 |
6 |
|
| hydrofluorocarbons |
HFCs |
-aerosol propellants -refrigeration gases -foam-blowing agents -solvents -fire retardants -aluminium smelting -semiconductor production |
-CFCs, HCFCs removal by stratospheric photolysis -HCFC, HFC reaction with tropospheric hydroxyl (OH) |
2 - 50,000 (dependent on compound) |
<14% |
|
| perfluorocarbons |
PFCs |
-aluminium production -semiconductor production |
|
>10,000 |
<1% |
|
| sulfur hexafluoride |
SF6 |
-electrical transmission and distribution systems -circuit breakers -magnesium production |
|
3,200 |
<1% |
The Greenhouse Gas Effect
Greenhouse gases in the earth's atmosphere absorb infrared radiation from the ground.
This radiation (heat) is re-emitted in all directions. Heat radiated back towards the earth's surface leads to the warming of the surface.
Using data from ice cores and other sources, scientists have been able to determine the temperature variation and carbon dioxide concentrations on earth over time:
Since 1950, temperature variations have been observed that can not be explained solely on the basis of the presence of natural greenhouse gases.
Scientists have modeled this unusual temperature variation to take into account man-made sources of greenhouse gases and have found that this may explain the temperature variations being observed.
During the 21st century, the earth is likely to experience:
- higher maximum temperatures and more hot days
- higher minimum temperatures and fewer cold days
- more intense precipitation events like rain over many areas
- melting of polar ice caps resulting in rising sea levels
Suggestions for combatting global warming have been:
- reduction in combustion of fossil fuels and sourcing new fuel alternatives
- reducing deforestation and replanting forests
- reducing and/or eliminating the use of HCFs, HCFCs, perfluorocarbons and sulfur hexafluoride.
Finding alternatives to these greenhouse gases in chemical and industrial processes has led to the development of a new branch of chemistry called Green Chemistry.
|