Study Notes on Greenhouse Gas Emissions

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Greenhouse Gas Emissions

  • Author: Amy Hackney Blackwell

  • Date: 2024

  • Source: Gale Environmental Studies Online Collection

  • Length: 1,548 words

Definition of Greenhouse Gases

  • Greenhouse gases are atmospheric gases that absorb and re-emit energy from the sun.

  • This process of absorbing and emitting radiation is known as the greenhouse effect.

  • Common greenhouse gases include:

    • Carbon dioxide (CO₂)

    • Methane (CH₄)

    • Water vapor (H₂O)

    • Ozone (O₃)

    • Nitrous oxide (N₂O)

    • Chlorofluorocarbons (CFCs)

Emission Sources

  • Greenhouse gases are released from both natural sources (like vegetation and water bodies) and human activities such as:

    • Industrial processes

    • Automobile emissions

The Greenhouse Effect

  • The greenhouse effect is crucial for life, as it traps warmth from sunlight in the atmosphere, keeping the Earth warm enough to support life.

  • Without this effect, Earth's global temperatures would be much lower, making many areas uninhabitable.

Comparison to a Greenhouse
  • The phenomenon resembles a greenhouse used for plant growth, where:

    • Light and heat enter through glass

    • Heat is retained, preventing escape, thus warming the interior

  • On Earth, the atmosphere functions like the glass panels—allowing sunlight in but preventing much of the heat from escaping back into space.

Radiation Absorption

  • The Sun emits various types of radiation (visible light, infrared light, etc.) which:

    • Pass through Earth's atmosphere

    • Are absorbed by the ground, oceans, and vegetation

    • Are re-radiated back into the atmosphere in the form of heat

  • Greenhouse gases capture this heat, which warms the atmosphere further.

Greenhouse Gas Types

Water Vapor
  • Considered a natural greenhouse gas.

  • Acts to insulate; cloudy nights retain heat better than clear ones.

  • Behavior:

    • During the day, clouds can block sunlight leading to cooling effects

    • Dry regions show extreme temperature changes due to lack of water vapor.

  • Increased global temperature causes more evaporation, which increases water vapor levels, enhancing the greenhouse effect.

Carbon Dioxide (CO₂)
  • About 74% of greenhouse emissions are CO₂.

  • It is the primary driver of anthropogenic climate change due to its high prevalence in emissions.

  • Lifetime: Approximately 12 years in the atmosphere.

  • Significant emissions stem from:

    • Burning fossil fuels (coal, oil, gas)

    • Motor vehicle emissions

    • Industrial activities

  • Historical Carbon Emissions Trend:

    • Levels increased from 315 ppm in 1960 to 400 ppm in 2015.

    • Current levels as of October 2023 are around 419 ppm—the highest in approximately 4.5 million years.

    • Emissions distribution changed from 90% from U.S. and Europe in 1900 to a lower share by 2020, with China and Asia becoming predominant sources.

Methane (CH₄)
  • Accounts for 17% of greenhouse emissions.

  • It has significantly higher global warming potential than CO₂:

    • 30 times more effective than CO₂ over 100 years

    • 82 times more effective over 20 years

  • Methane persists in the atmosphere for 15-20 years.

  • Sources:

    • Natural decay in wetlands and permafrost

    • Livestock digestion (mainly cattle)

    • Human activities contribute to 60% of atmospheric methane.

  • Current concentration is approximately 1.9 ppm, up 150% since 1750, and methane contributes to about one-fifth of greenhouse heating effects.

Other Greenhouse Gases
  • Ozone (O₃):

    • Emitted from industrial sources and contributes to warming, though in lower concentrations than CO₂.

  • Nitrous Oxide (N₂O):

    • Produced by agricultural processes and industrial emissions, with a warming potential of 265 times that of CO₂ over 100 years and a lifespan of about 121 years in the atmosphere.

  • Chlorofluorocarbons (CFCs):

    • Used in refrigeration, aerosol sprays, and solvents, contributing strongly to atmospheric warming.

  • Volatile organic compounds (VOCs) impact the photochemistry of ozone and climate.

  • Aerosols can have cooling or warming effects depending on their properties (light vs. dark particles).

Global Emissions Overview

  • According to the U.S. Environmental Protection Agency (EPA):

    • U.S. greenhouse gas emissions decreased by 20% from 2005 to 2020.

  • Globally, emissions increased by 43% from 1990 to 2015.

  • Primary contributing sectors in the U.S. include:

    • Transportation, electricity generation, and industry (about 75% of emissions)

    • Agriculture (approximately 10%)

    • Commercial and residential uses (around 13% including air conditioning and appliances).

  • Countries with the highest emissions:

    • United States and China.

    • Sub-Saharan African nations such as Chad and Niger exhibit the lowest per-capita emissions.

Further Readings

  • Dagsvik, John, and Sigmund Moen. “To what extent are temperature levels changing due to greenhouse gas emissions?” September 2023. Statistics Norway.

  • “Greenhouse gases.” May 22, 2023. MIT Climate Portal.

  • Ritchie, Hannah, et al. “Global greenhouse gas emissions.” June 10, 2020. Our World in Data.

  • “Sources of greenhouse gas emissions.” U.S. Environmental Protection Agency.

  • “Trends in Atmospheric Carbon Dioxide.” NOAA Global Monitoring Laboratory.