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

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

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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