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Monitoring and maintaining the environment - OCR Gateway The greenhouse effect and global warming

Biodiversity is a measure of how many different species live in an ecosystem. Human activities like changing land use, deforestation and peat bog destruction reduce this.

Part of Biology (Single Science)Global challenges

Greenhouse effect and evidence of enhanced greenhouse effect

The greenhouse effect

When energy from the Sun hits the surface of Earth, some of it is absorbed and some of it is reflected back. Some of this reflected energy passes through the into space, but some of it is reflected back again to Earth.

This is why it is hot sitting in a car or greenhouse on a sunny day, and so is called the greenhouse effect. Without the greenhouse effect the mean temperature on Earth would be -18掳C and there would be very little or no life.

The greenhouse effect traps some of the energy from the Sun, which keeps our planet at a suitable temperature for life.

However, our increased release of gases such as carbon dioxide and methane is causing an increase in the greenhouse effect called the enhanced greenhouse effect. This is leading to climate change. Some of the effects of climate change are:

Global warming

Global warming is the increase in the mean temperature of the Earth. The ten hottest years since records began have been in the last 30 years. The mean increase in the last 100 years has been around 1掳C. This might seem small, but is enough to have devastating consequences on many in different parts of the world.

Global warming graph showing the percentage of CO2 in the atmosphere since 1700. It remains steady at 0.028 per cent until approx 1850 and then starts rising steeply reaching 0.035 per cent by 2000.
Graph showing change in global temperature over 100 year period

As the percentage of carbon dioxide in our atmosphere has increased, so has the Earth's mean temperature. Note that the shape of the first graph showing the amount of carbon dioxide in the atmosphere is and is a similar shape to graphs showing human population change over the same time period.

When comparing graphs such as changes to carbon dioxide levels and temperature against time, note that the axes are drawn to different scales, and do not start at '0'. There is a between percentage carbon dioxide in the atmosphere and the mean global temperature, though a has yet to be fully proven.

Additional consequences of global warming are:

  • melting of the polar ice caps
  • the rise in sea level may one day threaten many cities such as London, New York and Amsterdam
  • weather patterns will change with more unusual weather
  • animals will migrate towards the poles to find habitats with suitable temperatures
  • tropical diseases may become more common in other regions, such as Europe
  • many more are likely to become

The rate of global warming can be reduced by reducing the rate at which greenhouse gases are being released. For example:

  • using energy resources more efficiently, eg more cars with a higher fuel efficiency
  • using renewable sources of energy (eg solar power) instead of fossil fuels
  • reducing waste by recycling (eg plastic bottles)
  • reducing deforestation (eg reducing the conversion of rainforest to farmland)
  • developing techniques to capture and store the carbon dioxide released from power stations