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Climate change

 

The Earth is surrounded by a thin blanket of gases, known as the atmosphere. Contained in the atmosphere are a number of gases known as greenhouse gases, including carbon dioxide, methane and water vapour. They are called greenhouse gases because like a greenhouse they allow the Suns rays to pass through but trap some of the heat emitted back from the Earth’s surface.

This is a natural process which warms the Earth and makes it habitable - without greenhouse gases the Earth would be too cold to support life, and we wouldn't be here. Over the past few hundred years of industrialisation we have released more and more greenhouse gases – particularly carbon dioxide, through the burning of fossil fuels – such as coal, oil and gas in power stations, boilers and vehicles.

The net effect of this activity is much higher concentrations of greenhouse gases and increased warming of the Earth. The average temperature of the Earth is already increasing as a result – the International Panel on Climate Change (IPCC) predict an increase of between 1.1 and 6.4°C (with a best estimate of 1.8 to 4°C) above 1990 levels by the end of this century.

This global temperature rise does not mean that everywhere will enjoy warmer weather – some places will get hotter, some colder and some just more wild and unpredictable. This is what we call climate change.