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Jenni MacLean
Jillian Holbrook
Jenni MacLean
Jillian Holbrook
The greenhouse effect is the process by which energy from the sun is trapped in the form of heat by various types of gas. It is a natural process that helps regulate the temperature of the Earth's surface!
Although the sun is incredibly hot and releases both thermal and light energy, the energy that actually reaches the Earth is visible light and ultraviolet radiation. When the sun's energy hits the Earth's surface, some of it is absorbed and re-emitted as lower-energy infrared radiation. That energy then begins to move away from the Earth and back into space.
However, the Earth's atmosphere is composed of a number of gases, including water vapor, carbon dioxide, methane, and nitrous oxide, known as greenhouse gases. So when the infrared radiation sent back from Earth's surface reaches the atmosphere, a portion of it is trapped by gases instead of being lost. This phenomenon allows the surface of the Earth to rise in temperature.
Greenhouse gases absorb infrared radiation and convert it to heat energy, holding it primarily in the troposphere. The greenhouse effect is a vital process that keeps the Earth warm enough for life to exist. Without these gasses converting and trapping energy close to Earth's surface, it would be too cold for modern life to exist.
Greenhouse gases have a high thermal retention property. They include:
· Carbon dioxide (CO2)
· Methane
· Water vapor
· Nitrous oxide
· Chlorofluorocarbons (CFCs)
While water vapor is a greenhouse gas and has thermal retention, it has a short residence time in the atmosphere, which means that it does not contribute significantly to global climate change. In fact, different greenhouse gases have varying potency when it comes to their potential impact on climate change.
The global warming potential (GWP) of a gas is used to distinguish its potential impact on global climate change. GWP estimates how much a molecule of any compound could contribute to global warming within 100 years in comparison to carbon dioxide. Carbon dioxide has a GWP of 1, which is why it is often used as a comparison point for other glasses. Chlorofluorocarbons (CFCs) have the highest GWP (13,000), followed by nitrous oxide (300), then methane (25).
The GWP of a gas 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 25, this means that one ton of methane has the same warming effect as 25 tons of CO2 over a 100-year time period.
Why care about GWP? GWP is an important measure because it helps policymakers and researchers understand the relative impact of different greenhouse gases on global warming. It is used to set targets and policies to reduce greenhouse gas emissions and mitigate the impacts of global warming.
Natural sources of carbon dioxide emissions:
Human-induced sources of increased CO2 emissions include:
Natural sources of methane emissions include:
Human-induced sources of methane include:
Natural sources of water vapor include:
Human-induced sources of increased water vapor include:
Natural sources of nitrous oxide include:
Human-induced sources of increased atmospheric nitrous oxide:
Chlorofluorocarbons (CFCs) are a group of man-made chemicals that were once widely used as aerosol propellants. CFCs are highly potent greenhouse gases that contribute to the depletion of the ozone layer in addition to the warming of the Earth's atmosphere.
All of the main sources of CFCs are human-induced:
CFCs are no longer produced or used in many countries due to the negative impacts they have on the ozone layer and their exceptionally high GWP. In 1987, the Montreal Protocol was signed, which called for the phasing out of CFC production. As a result, CFC emissions have significantly decreased in recent years. However, CFCs that have already been released into the atmosphere continue to impact the environment.
The greenhouse effect is important because it helps to regulate the Earth's temperature and make it habitable for living things. Without the greenhouse effect, the Earth's average temperature would be much colder, making it difficult for life as we know it to exist. This is thanks to the high thermal retention properties of greenhouse gases.
However, the large-scale increase of greenhouse gases in the atmosphere is contributing to climate change, which has environmental impacts ranging from frequent and severe heatwaves to droughts and storms to rising sea levels. Using GWP, efforts to target the reduction of greenhouse gases can more successfully evaluate the different potencies of greenhouse gases and inform regulatory policies for human-sourced emissions.
🎥 Watch: AP Environmental Science Streams
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Jenni MacLean
Jillian Holbrook
Jenni MacLean
Jillian Holbrook
The greenhouse effect is the process by which energy from the sun is trapped in the form of heat by various types of gas. It is a natural process that helps regulate the temperature of the Earth's surface!
Although the sun is incredibly hot and releases both thermal and light energy, the energy that actually reaches the Earth is visible light and ultraviolet radiation. When the sun's energy hits the Earth's surface, some of it is absorbed and re-emitted as lower-energy infrared radiation. That energy then begins to move away from the Earth and back into space.
However, the Earth's atmosphere is composed of a number of gases, including water vapor, carbon dioxide, methane, and nitrous oxide, known as greenhouse gases. So when the infrared radiation sent back from Earth's surface reaches the atmosphere, a portion of it is trapped by gases instead of being lost. This phenomenon allows the surface of the Earth to rise in temperature.
Greenhouse gases absorb infrared radiation and convert it to heat energy, holding it primarily in the troposphere. The greenhouse effect is a vital process that keeps the Earth warm enough for life to exist. Without these gasses converting and trapping energy close to Earth's surface, it would be too cold for modern life to exist.
Greenhouse gases have a high thermal retention property. They include:
· Carbon dioxide (CO2)
· Methane
· Water vapor
· Nitrous oxide
· Chlorofluorocarbons (CFCs)
While water vapor is a greenhouse gas and has thermal retention, it has a short residence time in the atmosphere, which means that it does not contribute significantly to global climate change. In fact, different greenhouse gases have varying potency when it comes to their potential impact on climate change.
The global warming potential (GWP) of a gas is used to distinguish its potential impact on global climate change. GWP estimates how much a molecule of any compound could contribute to global warming within 100 years in comparison to carbon dioxide. Carbon dioxide has a GWP of 1, which is why it is often used as a comparison point for other glasses. Chlorofluorocarbons (CFCs) have the highest GWP (13,000), followed by nitrous oxide (300), then methane (25).
The GWP of a gas 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 25, this means that one ton of methane has the same warming effect as 25 tons of CO2 over a 100-year time period.
Why care about GWP? GWP is an important measure because it helps policymakers and researchers understand the relative impact of different greenhouse gases on global warming. It is used to set targets and policies to reduce greenhouse gas emissions and mitigate the impacts of global warming.
Natural sources of carbon dioxide emissions:
Human-induced sources of increased CO2 emissions include:
Natural sources of methane emissions include:
Human-induced sources of methane include:
Natural sources of water vapor include:
Human-induced sources of increased water vapor include:
Natural sources of nitrous oxide include:
Human-induced sources of increased atmospheric nitrous oxide:
Chlorofluorocarbons (CFCs) are a group of man-made chemicals that were once widely used as aerosol propellants. CFCs are highly potent greenhouse gases that contribute to the depletion of the ozone layer in addition to the warming of the Earth's atmosphere.
All of the main sources of CFCs are human-induced:
CFCs are no longer produced or used in many countries due to the negative impacts they have on the ozone layer and their exceptionally high GWP. In 1987, the Montreal Protocol was signed, which called for the phasing out of CFC production. As a result, CFC emissions have significantly decreased in recent years. However, CFCs that have already been released into the atmosphere continue to impact the environment.
The greenhouse effect is important because it helps to regulate the Earth's temperature and make it habitable for living things. Without the greenhouse effect, the Earth's average temperature would be much colder, making it difficult for life as we know it to exist. This is thanks to the high thermal retention properties of greenhouse gases.
However, the large-scale increase of greenhouse gases in the atmosphere is contributing to climate change, which has environmental impacts ranging from frequent and severe heatwaves to droughts and storms to rising sea levels. Using GWP, efforts to target the reduction of greenhouse gases can more successfully evaluate the different potencies of greenhouse gases and inform regulatory policies for human-sourced emissions.
🎥 Watch: AP Environmental Science Streams
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