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Greenhouse gases are crucial to keeping our planet at a habitable temperature. Without the natural greenhouse effect, the heat emitted by the Earth would simply pass outwards from the Earth’s surface into space. The Earth would have an average temperature of about -20°C.
A greenhouse gas is so called because it absorbs infrared radiation in the form of heat, which is circulated in the atmosphere and eventually lost to space. Greenhouse gases also increase the rate at which the atmosphere can absorb short-wave radiation from the sun, but this has a much weaker effect on global temperatures.
Greenhouse gases in our atmosphere are:
- carbon dioxide
- water vapour
- nitrous oxide
The carbon dioxide released from the burning of fossil fuels is accumulating as an insulating blanket around the Earth, trapping more of the Sun’s heat in our atmosphere. Anthropogenic release of carbon dioxide contributes to the current
Which gases cause the greenhouse effect?
The contribution that a greenhouse gas makes to the greenhouse effect depends on how much heat it absorbs, how much it re-radiates and how much of it is in the atmosphere. In descending order, the gases that contribute most to the Earth’s greenhouse effect are: water vapour (H2O), carbon dioxide (CO2), nitrous oxide (N2O), methane (CH4) and ozone (O3).
In terms of the amount of heat they can absorb and re-radiate (known as their global warming potential or GWP), methane is 23 times more effective and nitrous oxide 296 times more effective than carbon dioxide. However, there is much more carbon dioxide in the Earth’s atmosphere than there is methane or nitrous oxide.
Not all the greenhouse gas that we emit to the atmosphere remains there indefinitely. For example, the amount of CO2 in the atmosphere and the amount of CO2 dissolved in surface waters of the oceans stay in equilibrium, because the air and water mix well at the sea surface. Thus when we add more CO2 to the atmosphere, a proportion of it dissolves into the oceans.
Man-made (anthropogenic) greenhouse gases
Since the start of the industrial revolution in the mid-18th century, human activities have greatly increased the concentrations of greenhouse gases in the atmosphere. Consequently, measured atmospheric concentrations of carbon dioxide are many times higher than pre-industrial levels.
The main sources of greenhouse gases due to human activity are:
Carbon dioxide levels are substantially higher now than at any time in the last 750 000 years. The burning of fossil fuels has elevated CO2 levels from an atmospheric concentration of approximately 280 parts per million (ppm) in pre-industrial times to over 400 ppm in 2018. This is a 40% increase since the industrial revolution.
CO2 concentrations are increasing at a rate of about 2–3 ppm/year and are expected to exceed 900 ppm by the end of the 21st century.
If this continues, and together with rising emissions of methane and other greenhouse gases, by 2100 the global average surface temperature could have increased by up to 4.8°C compared to pre-industrial levels. Consequently, some scientists suggest goals to limit concentrations to keep temperature change below 2°C. This would include substantial cuts in man-made (anthropogenic) greenhouse gas emissions by the middle of the 21st century through large-scale changes in energy systems and land use.
In 2010, the burning of coal, natural gas, and oil for electricity and heat was the largest single source of global greenhouse gas emissions (25%). By comparison, in 2010, 14% of global greenhouse gas emissions came from fossil fuels burned for road, rail, air and marine transportation.
Agriculture, deforestation and other changes in land-use account for one quarter of net anthropogenic greenhouse gas (GHG) emissions. According to a United Nations report, livestock is responsible for about 14.5 per cent of this. The main sources of emissions are: feed production and processing (45 per cent), outputs of GHG during digestion by cows (39 per cent), and manure decomposition (10 per cent). The rest is attributable to the processing and transportation of animal products.
Higher concentrations of atmospheric methane are also caused by changes in land and wetland use, pipeline losses, and landfill emissions. The use of fertilizers can also lead to higher nitrous oxide (N2O) concentrations.
Agriculture is estimated to be the main driver for around 80% of deforestation worldwide. Source: Pixabay.
Cement manufacture contributes carbon dioxide (CO2) to the atmosphere when calcium carbonate is heated, producing lime and carbon dioxide.
Estimates vary, but it is widely accepted that the cement industry produces between 5 and 8 per cent of global man-made CO2 emissions, of which 50 per cent is produced from the chemical process itself, and 40 per cent from burning fuel to power that process. The amount of CO2 emitted by the cement industry is more than 900 kg of CO2 for every 1000 kg of cement produced.
Aerosols are small particles suspended in the atmosphere that can be produced when we burn fossil fuels. Other man-made sources of aerosols include pollution from cars and factories, chlorofluorocarbons (CFCs) used in refrigeration systems and CFCs and halons used in fire suppression systems and manufacturing processes. Aerosols can also be produced naturally from a number of natural processes e.g. forest fires, volcanoes and isoprene emitted from plants.
We know that greenhouse gases provide a warming effect to Earth’s surface, but aerosol pollution in the atmosphere can counteract this warming effect. For example, sulphate aerosols from fossil fuel combustion, exert a cooling influence by reducing the amount of sunlight that reaches the Earth.
Aerosols also have a detrimental impact on human health and affect other parts of the climate system, such as rainfall.
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1. Enhanced Greenhouse effect
'Greenhouse gases' are actually crucial to keeping our planet at a habitable temperature, without them the Earth would be about minus 17 degrees! Anthropogenic or human release of carbon dioxide is what is contributing to an additional or enhanced greenhouse effect.