The Greenhouse Effect (College Board AP® Environmental Science): Study Guide

Jacque Cartwright

Written by: Jacque Cartwright

Reviewed by: Alistair Marjot

Updated on

What are greenhouse gases?

  • Greenhouse gases (GHGs) trap heat in the atmosphere to regulate Earth's climate through a natural process called the greenhouse effect

  • The principal greenhouse gases are

    • carbon dioxide (CO₂)

    • methane (CH₄)

    • water vapor (H₂O)

    • nitrous oxide (N₂O)

    • chlorofluorocarbons (CFCs)

  • Carbon dioxide (CO₂) is a colorless, odorless gas that's a natural part of the atmosphere

  • It accounts for 20% of the greenhouse effect

    • Levels have risen from 315 parts per million (ppm) in 1950 to over 421 ppm in 2022

    • 2050 levels are expected to be 550 ppm 

    • The increase is due to human activities—burning fossil fuels and deforestation

      • Deforestation also decreases carbon storage, as trees remove CO₂ from the atmosphere during photosynthesis

  • Methane is a colorless, odorless, flammable gas that's a main part of natural gas

  • It accounts for 17% of the natural greenhouse effect 

    • Methane is 28 times more potent than CO₂ at warming the Earth

    • Produced naturally and through human activities such as:

      • The decay of organic matter in wetlands, forests, and oceans

      • Agriculture (particularly rice growing and livestock farming), fossil fuel extraction, and waste landfills

  • Nitrous oxide (N₂O) is also known as laughing gas

    • It is a long-lived, potent GHG with a warming effect nearly 300 times that of carbon dioxide per molecule over a 100-year period

    • It remains in the atmosphere for around 121 years

    • Naturally present in the atmosphere as part of Earth's nitrogen cycle

      • This gas is emitted from agricultural activities, such as using nitrogen fertilizers and animal waste on farmland and pastures

      • Fossil fuel combustion

      • Industrial processes

    • From 1980 to 2020, nitrous oxide emissions grew 40%

    • In 2022, the concentration of atmospheric N₂O reached 336 parts per billion, which is much higher than previous predictions

  • Chlorofluorocarbons (CFCs) and hydrofluorocarbons (HFCs) account for 1.5% of GHGs in the atmosphere

    • These are man-made chemicals that are

      • 10,000 times stronger than CO₂ at trapping heat

      • Increasing at a rate of 6% per year

      • Banned by many countries as they deplete the ozone layer (1 CFC atom can destroy thousands of ozone molecules)

    • HFCs are weak ozone-depleting substances but they are strong greenhouse gases

Examiner Tips and Tricks

Do not confuse the ozone layer with global warming.

Yes, ozone is a greenhouse gas, but the ozone layer protects the Earth from ultraviolet light.

Ozone is different because it absorbs incoming UV light and outgoing infrared light from the Earth.

The hole in the ozone layer increases the rate of skin cancer by allowing more UV rays to enter the atmosphere. It has no effect on incoming solar energy.

Is water vapor a greenhouse gas?

  • Water vapor is the most abundant greenhouse gas 

  • It accounts for about 95% of GHGs by volume

  • Water vapor is responsible for 50% of the natural greenhouse effect

  • While water vapor is a greenhouse gas, it doesn’t contribute to global climate change because it has a short residence time in the atmosphere of a few days or even hours

  • Instead, increased water vapor is a consequence of global warming

  • Increased water vapor in the atmosphere amplifies the warming caused by other greenhouse gases

    • A warmer atmosphere holds more water vapor, leading to more warming and greater evaporation

    • This is called a 'positive feedback loop,' and the effect more than doubles the warming that would happen due to increasing carbon dioxide alone

  • Human activities indirectly affect temperature and moisture through:

    • Deforestation, land-use changes, and burning fossil fuels

What is the greenhouse effect?

  • The greenhouse effect is a naturally occurring phenomenon where short-wave radiation (in the form of visible light and ultraviolet radiation) from the sun passes through to the Earth's surface

  • Some of this energy is absorbed by the Earth's surface and re-emitted as long-wave infrared radiation

  • This energy passes through the atmosphere, where some is emitted into space

  • The remaining thermal energy is trapped by the greenhouse gases and then re-emitted in all directions back into the atmosphere and causes the temperature of the surface to rise

  • This process is important to ensure that Earth is warm enough for life

  • Without the greenhouse effect, the average temperature would be much colder, making the planet uninhabitable

    • For example, the average surface temperature of Earth is about 15 °C

    • Without the greenhouse effect, it would be about -18 °C

The natural greenhouse effect

Diagram illustrating Earth's thermal radiation, emission, and reflection by greenhouse gases (horizontal blue line), with arrows showing different radiation paths. Blue arrow showing thermal radiation from the sun to Earth, red arrow showing reflection of thermal radiation back out to space, and a yellow arrow showing some reflection from the greenhouse gases (blue horizontal line) back to Earth's atmosphere.
The natural greenhouse effect where some thermal radiation is reflected back to into Earth's atmosphere by greenhouse gases

The enhanced greenhouse effect

  • The enhanced greenhouse effect is caused by human activities that produce excessive greenhouse gases (GHGs) into the atmosphere, causing heat trapping and global warming

  • Human activity has increased CO₂ levels in the atmosphere by more than 100 parts per million (ppm) to 420ppm in 2020

  • Increased amounts of greenhouse gases have led to less long-wave radiation escaping the atmosphere

  • Increasing global average temperatures by over 1°C since pre-industrial times

Diagram illustrating the greenhouse effect and enhanced greenhouse effect, showing differences in heat absorption and radiation by greenhouse gases in the atmosphere.
Human activities lead to the emission of greenhouse gases that enhance the greenhouse effect, contributing to global warming

Global warming potential

  • Certain gases can retain heat energy longer than others because they have high thermal retention properties

  • Greenhouse gases are known to have a high thermal retention property

  • Each greenhouse gas has varying potency when it comes to their potential impact on global warming

Examiner Tips and Tricks

Even though water vapor has thermal retention and is a greenhouse gas, it is short-lived in the atmosphere. This means that it does not contribute to long-term global climate change.

  • The global warming potential (GWP) of a gas is used to identify what potential impact it will have on global climate change

  • The GWP value is the amount of warming that 1 tonne of a GHG would create in relation to 1 tonne of CO₂ over a 100-year timescale

  • As the most common greenhouse gas (and one that stays in the atmosphere for a very long time) carbon dioxide is used as the standard baseline gas with a GWP of 1

  • This makes it easy to compare the warming potential of other gases

  • Global greenhouse gas emissions are converted to CO₂ equivalents (CO₂e) by multiplying each GHG by its 100-year value

  • Methane (CH₄) survives in the atmosphere for 11.8 years and is approximately 27-30 times more potent than CO₂ at warming the climate

  • Nitrous oxide (N₂O) resides in the atmosphere for 109 years and is 273 times more potent at warming the climate than CO₂

  • Fluorinated gases (CFCs, HFCs, sulfur hexafluoride, perfluorocarbons) have a residency time in the atmosphere from a few weeks to thousands of years and their GWP varies from 12 to 25,000 times more potent than CO₂

Examiner Tips and Tricks

GWP is calculated by multiplying the gas's warming effect by its atmospheric lifetime and the ratio of its global warming effect to that of CO₂. For example, since the GWP of methane is 27, this means that one ton of methane has the same warming effect as 27 tons of CO₂ over a 100-year time scale.

Importance of GWP

  • Scientists and policymakers use GWP to analyze the effects of different greenhouse gases on the climate

  • It allows them to prioritize which gases to reduce emissions of and understand how various activities affect the climate overall

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Jacque Cartwright

Author: Jacque Cartwright

Expertise: Geography Content Creator

Jacque graduated from the Open University with a BSc in Environmental Science and Geography before doing her PGCE with the University of St David’s, Swansea. Teaching is her passion and has taught across a wide range of specifications – GCSE/IGCSE and IB but particularly loves teaching the A-level Geography. For the past 5 years Jacque has been teaching online for international schools, and she knows what is needed to get the top scores on those pesky geography exams.

Alistair Marjot

Reviewer: Alistair Marjot

Expertise: Environmental Systems and Societies & Biology Content Creator

Alistair graduated from Oxford University with a degree in Biological Sciences. He has taught GCSE/IGCSE Biology, as well as Biology and Environmental Systems & Societies for the International Baccalaureate Diploma Programme. While teaching in Oxford, Alistair completed his MA Education as Head of Department for Environmental Systems & Societies. Alistair has continued to pursue his interests in ecology and environmental science, recently gaining an MSc in Wildlife Biology & Conservation with Edinburgh Napier University.