Climate Change and Greenhouse Gases

Major Greenhouse Gases

  • Key Greenhouse Gases:

    • Nitrous oxide
    • Carbon dioxide (CO2CO_2)
    • Water vapor (H2OH_2O)
    • Methane (CH4CH_4)
    • Chlorofluorocarbons (CFCs)
  • Natural vs. Human-Induced:

    • Some greenhouse gases are naturally occurring.
    • Human activities increase their concentration.
  • Sources of Greenhouse Gases:

    • Burning fossil fuels: Carbon dioxide and methane
    • Mining: Methane
    • Landfill decomposition: Methane
    • Cattle: Methane
    • Agriculture: Nitrous oxides
    • Man-made refrigerants and coolants: CFCs

Effects of Climate Change

  • Rising Temperatures:

    • Increase in average global temperature.
    • Does not eliminate cold weather events.
  • Melting Permafrost and Sea Ice

  • Rising Sea Levels:

    • Displacement of coastal populations.
  • Most Affected Areas:

    • Arctic
    • Coastal areas

Sea Level Rise

  • Thermal Expansion:

    • Liquids and gases expand when warmer.
    • Expansion of ocean volume contributes to sea level rise.
  • Ice Melting:

    • Melting of ice caps and glaciers increases sea level rise.
  • Coastal Impacts:

    • Increased flooding.
    • Changes in weather patterns lead to more intense storms.

Changes in Weather Patterns

  • Wind and Ocean Currents:

    • Climate change alters circulation patterns.
  • Jet Stream:

    • Larger oscillations cause more drastic weather changes (colder winters, hotter summers).
  • Local Climates:

    • Significant impacts due to altered weather patterns.

Polar Regions and Feedback Loops

  • Faster Response Times:

    • Polar regions react more quickly to climate change due to positive feedback loops.
  • Melting Snow and Ice:

    • Reduces reflectivity, increasing warming.
    • Snow and ice reflect light, which has a cooling effect
    • Less reflectivity increases the rate of warming: Positive feedback loop.
  • Permafrost Thawing:

    • Releases methane, further accelerating warming: Positive feedback loop.

Rising Sea Levels: Specific Impacts

  • Expected Rise:

    • Expect about one meter rise in sea level over 100 years.
    • Significant flooding, especially in flat coastal areas.
  • Miami Example:

    • Raising street levels to combat flooding.
    • Pumping water out of streets due to "sunny day flooding."

Regional Climate Change

  • Agricultural Areas:

    • Changing weather patterns alter agricultural areas.
  • Wildlife Ranges:

    • Shifting ranges away from the Equator and towards the poles.
  • Weather Changes:

    • Warmer, wetter winters in Europe.
    • More frequent El Ninos.
    • More intense thunderstorms and hurricanes.
  • Increased Superstorms:

    • More frequent damaging storms (e.g., Hurricane Katrina, Hurricane Sandy).

Ocean Acidification

  • Process:

    • Absorption of CO<em>2CO<em>2 creates carbonic acid (H</em>2CO3H</em>2CO_3).
    • Lowers the pH of the ocean.
  • Impact on Marine Life:

    • Affects organisms with calcium-based shells or structures (e.g., corals, mollusks).

Historical Correlation

  • Greenhouse Gases, Temperature, and Sea Level:

    • Correlation between increases in greenhouse gases, temperature, and sea level.
  • Impact on Temperature and Sea Level:

    • Increasing CO2CO_2 and methane in the atmosphere impacts temperature and sea level.

Visual Representation of Affected Areas

  • One Meter Rise in Sea Level:
    • Significant portions of coastal areas face constant flooding.

Glacial Retreat

  • Muir Glacier in Alaska:
    • Comparison of 1948 to 2004 shows significant retreat.
    • Photos taken at the same time of year.

Arctic Sea Ice Reduction

  • Feedback Loop

    • Decrease in reflectivity increases the rate of warming: Positive feedback loop
  • Comparison of 1979 to 2007:

    • Significant reduction in sea ice near the North Pole.

Athabasca Glacier in Canada

  • Retreating Glacier
    • Significant retreat between 1992 and 2005.

Wildlife Range Changes

  • Pest Introduction

    • Movement of wildlife introduces pests to new areas.
  • Mountain Pine Beetle:

    • Infestation in British Columbia's boreal forest leading to tree die-off.
    • Beetles expand territory due to warming climate.
  • Mosquitoes and Tropical Diseases:

    • Warming climate allows mosquitoes to survive year-round.
    • Spread of diseases like dengue fever into North America.

Albedo

  • Definition:

    • Measure of how reflective a surface is
    • High albedo: Very reflective
    • Low albedo: Not reflective
  • Examples:

    • Highest albedo: Snow and ice
    • Low albedo: Ocean, soil, forest
  • Impact

    • Melting ice caps decrease Earth's albedo.

Albedo and Evaporation

  • Cloud Cover

    • Increased evaporation creates more cloud cover
    • Cooling or warming effect depending on circumstances
  • Water Vapor:

    • Greenhouse gas leading to a warming effect: Positive feedback loop
    • Cycles out of the atmosphere quickly
  • Cloud Formation:

    • Increased cloud formation; fluffy white clouds increase albedo, leading to a cooling effect: Negative feedback loop

Types of Clouds and Their Effects

  • Cumulus Clouds:

    • Thick, white, fluffy clouds closer to the ground
    • Cooling effect: Reflect light back into space
  • Cirrus Clouds:

    • Thinner clouds at high altitude
    • Heating effect

Cooling Effects

  • Ocean Absorption

    • Ocean absorbs CO2CO_2, slowing down climate change
  • Planetary Albedo

    • Increase in bright white clouds has a cooling effect
  • Volcanic Eruptions and Sulfate Aerosols

    • Volcanic eruptions block sunlight, leading to a cooling effect
    • Sulfate aerosols (a form of pollution) create atmospheric haze, contributing to a cooling effect.
  • Ice Albedo

    • Reflectivity of ice: More ice reflects more sunlight
    • Decreasing ice cover results in less reflectivity, causing a warming effect: Positive feedback loop

Main Idea of Climate Change

  • Greenhouse Gases:

    • Greenhouse gases are increasing due to human activities, especially burning fossil fuels
  • Consequences:

    • Leads to climate change, causing significant problems

Solutions for Climate Change

  • Legislation

    • Importance of legislation
    • Examples: Clear Air Act, Kyoto Protocol (ozone), Montreal Protocol (climate change), and Paris Climate Accord (climate change).
  • Prevention

    • Reduce fossil fuel use: Transition to nuclear and renewable energies
    • Use less coal (dirtiest fossil fuel)
    • Improve energy efficiency and use less energy
    • Adopt new, more energy-efficient and renewable technologies
    • Reduce deforestation
  • Economic Measures

    • Put a price on greenhouse gas emissions
    • Shift subsidies from fossil fuels to renewables.
  • Reduce Population Growth

  • Carbon Sequestration:

    • Remove carbon from the atmosphere and store it elsewhere.
    • Increase forests.
    • Implement sustainable agricultural practices.
    • Develop new technologies to sequester CO2CO_2.
    • Reduce leaks from gas pipelines.
    • Change animal feeds to reduce methane production.

International Agreements

  • Kyoto Protocol:

    • One of the first international agreements by the United Nations to fight global warming.
    • Set targets for nations to reduce greenhouse gas emissions.
    • Signed by 41 nations, including the European Union and developed industrial nations, except for the US and Australia.
    • Went into effect in February 2005.
  • US Non-Participation

    • The United States did not participate in the Kyoto Protocol, making it less effective.
    • President Clinton supported it, while President Bush withdrew.
    • The US and China are the biggest emitters
    • US non-participation impacted the success of the Kyoto Protocol

Cap and Trade System in the US

  • Federal Law

    • Designed to reduce carbon dioxide and greenhouse gas emissions in a cost-effective manner
    • Places a limit (cap) on emissions for each large-scale emitter
    • Allows companies to trade permits if they emit less than their limit
  • Loophole

    • Creates a loophole for businesses with enough money to continue emitting by paying for extra permits
  • Advantages:

    • Legal limit on emissions and rewards cuts in emissions through cost savings.
    • Mostly successful and has low expenses for consumers.
  • Disadvantages:

    • Not predictable and vulnerable to cheating.
    • Rich polluters can continue polluting.
    • Puts a variable price on carbon.

Carbon and Energy Taxes

  • Main Disadvantage:
    • Everybody hates taxes.

Paris Climate Agreement

  • Modern Version of Kyoto Protocol

    • International agreement from 2015
    • Aims to strengthen the global response to climate change by keeping global temperature rise this century well below 2 degrees Celsius above pre-industrial levels
    • Attempts to limit the temperature increase to 1.5 degrees Celsius
  • Political Support

    • Supported under the Obama administration.
    • Trump withdrew The United States from the agreement, and Biden rejoined.

Personal Actions to Reduce CO2 Emissions

  • Calculate Carbon Footprint

  • Transportation

    • Drive more fuel-efficient vehicles.
    • Use alternate forms of transportation like biking, carpooling, and public transit.
  • Reduce Waste

    • Reduce garbage and waste to decrease manufacturing that causes CO2CO_2 emissions
  • Energy Efficiency

    • Use more energy-efficient appliances and lights.
    • Use warm or cold water instead of hot water.
    • Dry clothes on a rack or line instead of in a dryer.
    • Increase home insulation.

Point Source Pollution Reduction: Scrubbers

  • Function:
    • Removes airborne pollutants, including CO2CO_2, from smokestacks to cut down emissions

Mitigating Effects of Climate Change

  • Preparation
    • Prepare for inevitable consequences in coastal areas.
    • Change infrastructure, such as raising road levels and pumping water out of streets.
    • Move vulnerable infrastructure away from the coast, such as nuclear power plants and hazardous waste storage.
    • Employ building designs that raise structures off the ground.