The Greenhouse Effect

Authors Avatar

Sullivan Hollands                Year 10 Geography

The Greenhouse Effect

About half of the Sun's energy is absorbed into the Earth's surface. The rest is either reflected back into space by the atmosphere or absorbed by dust and gas particles. The solar energy that does reach the Earth's surface heats the land and oceans. Successively, the land and oceans release heat in the form of infrared radiation. Carbon dioxide and methane have the ability to absorb some of the infrared radiation leading to warming of the lower atmosphere. Heat trapping gases similar to these are known as greenhouse gases. This absorption of heat, which keeps the surface of our planet warm enough to sustain us, is called the greenhouse effect. Without heat-trapping greenhouse gases in the air, the Earth's surface temperature would average a freezing -18°C, rather than 15°C.

Join now!

   Burning of fossil fuels and land clearing during the past 200 years has led to a growth in the density of greenhouse gases in the atmosphere. This has led to an increase in the amount of infrared radiation that is captured by the atmosphere, which leads to an increase in the average temperature of the atmosphere, producing a run away greenhouse effect.

    Increased temperatures in the lower atmosphere are likely to produce changes to weather and climate world-wide. Therefore, the enhanced greenhouse effect is often referred to as climate change or global warming.

    The effects ...

This is a preview of the whole essay