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What is climate change?

        
greyarrow.jpg (4688 bytes) Sources and sinks of GHGs

Sources

The major anthropogenic (man-made) sources of GHGs are:

redbullet.jpg (4598 bytes) Energy production and industry
The anthropogenic activity producing the largest quantity of GHGs (particularly CO2), is the production and use of energy. At least half of the warming that has already occurred is due to CO2 and its contribution is expected to remain the same even in the future.

Other significant sources of CO2 are: the burning of fossil fuels - coal, petroleum, natural gas - for industrial, commercial, transportation, residential and other uses. Small amounts of methane (CH4) are emitted during coal mining and the venting of natural gas.

The production and use of CFCs and other halocarbons during industrial processes also emits GHGs. The Montreal Protocol concerns issues related to these substances.

redbullet.jpg (4598 bytes) Changes in land use patterns
Deforestation, biomass burning (including fuelwood) and other changes in land-use practice release carbon dioxide, methane and nitrous oxide into the atmosphere.

redbullet.jpg (4598 bytes) Agriculture and livestock
Methane is released from rice cultivation and livestock systems; nitrous oxide is released when nitrogenous fertilizers are used.

redbullet.jpg (4598 bytes) Waste
Methane is also released from landfills.


Sinks of GHGs

Sinks refer to 'storehouses' of the gases - places where they can be sequestered.

redbullet.jpg (4598 bytes) The oceans are, perhaps, the biggest sink and contain about 40 000 GtC (giga tonnes of carbon). By contrast, the atmosphere contains 750 Gt and the terrestrial biosphere, 2200 Gt (IPCC 1996).

redbullet.jpg (4598 bytes) Vegetation and soil also have the capacity to sequester carbon. Soils also remove methane to some degree.

redbullet.jpg (4598 bytes) Atmospheric methane, however, is removed mainly by its oxidation by the OH radical in the troposphere.

redbullet.jpg (4598 bytes) Halocarbons do not have any significant mechanism of removal. They persist in the upper atmosphere (mid-upper stratosphere) for long periods and break down in the presence of sunlight. Nitrous oxide may also break down in this manner.

Regional distribution of carbon dioxide emissions

It is ironical that the contribution of developing nations to GHG emissions is less than half of that emitted by the developed countries. The latter have been responsible for more than 60% of the stock of GHGs. Over the last 100 years India has contributed only 2% of the total carbon emissions from fossil fuel burning (Marland G, Boden TA and Andres R J. 2000).


  
Regional contributions to cumulative CO2 emissions from industrial sources and land use change (1900-99)
 
Source Baumert K A and Kete N. 2001 (after Marland G, Boden T A and Andres R J. 2000)

 

References

redbullet.jpg (4598 bytes) Baumert K A and Kete N. 2001
The US, developing countries and climate protection: leadership or stalemate?
In Climate Issue Brief: World Resources Institute. Washington, DC: World Resources Institute. 12 pp.

redbullet.jpg (4598 bytes) IPCC. 1996
Climate Change 1995: The Science of Climate Change
Cambridge: Cambridge University Press. 572 pp.

redbullet.jpg (4598 bytes) Marland G, Boden T A and Andres R J. 2000
Global, Regional and National CO2 Emissions
In Trends: a compendium of data on global change. Oak Ridge, Tennessee, USA: Carbon Dioxide Information Analysis Center, Oak Ridge National Laboratory, U.S. Department of Energy

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