Global Change Review Notes
Kyoto Protocol
An international treaty that commits its parties to reduce greenhouse gas emissions, based on the premise that global warming exists and human-made CO2 emissions have caused it.
Adopted in 1997 and entered into force in 2005.
Aims to stabilize GHG concentrations in the atmosphere.
Montreal Protocol
An international treaty designed to protect the ozone layer by phasing out the production of numerous substances that are responsible for ozone depletion.
Signed in 1987, it successfully led to a reduction in CFCs and other ozone-depleting substances.
The Keeling Curve
Represents the concentration of CO2 in Earth's atmosphere since 1958.
Y-axis: CO2 levels (measured in parts per million, ppm)
X-axis: Years (time)
Important for demonstrating the increase of CO2 and implying correlation with global warming.
Major Greenhouse Gases (GHGs)
Carbon Dioxide (CO2): Produced by fossil fuel combustion, respiration; contributes significantly to the greenhouse effect.
Methane (CH4): Comes from agriculture (e.g., livestock), landfills; has a much higher GWP than CO2.
Nitrous Oxide (N2O): Result of agricultural and industrial activities; potent greenhouse gas.
Fluorinated gases: Synthetic gases used in various industrial applications; can trap heat much more efficiently than CO2.
Excess of GHGs leads to enhanced greenhouse effect, resulting in climate change, extreme weather events, and other environmental impacts.
Global Warming Potential (GWP)
A measure of how much a given mass of greenhouse gas contributes to global warming relative to the same mass of CO2 over a specified time (usually 100 years).
GWP Comparison of Major GHGs
CO2: GWP of 1 (baseline)
Methane (CH4): GWP of 28-36 over 100 years.
Nitrous Oxide (N2O): GWP of 298.
Fluorinated gases: Extremely high GWPs, ranging from thousands to tens of thousands.
Anthropogenic GHG
Carbon Dioxide is the primary GHG that comes from anthropogenic sources (fossil fuel combustion).
Chlorofluorocarbons (CFCs)
Synthetic compounds used as refrigerants, propellants, and solvents; highly effective in ozone depletion.
CFCs have been largely phased out due to Montreal Protocol.
Advantages and Disadvantages of CFC Alternatives
HCFs (Hydrochlorofluorocarbons): Less harmful to ozone, but still potent GHGs.
HFCs (Hydrofluorocarbons): No ozone depletion potential but significant global warming potential.
HC (Hydrocarbons): Natural, low toxicity, low GWP but flammable and less efficient.
Greenhouse Effect
The process by which GHGs trap heat from the Earth's surface, keeping the planet warm enough to sustain life.
Natural process but intensified by human emissions leading to climate change.
Ocean Acidification
Increase in CO2 absorption by the oceans leading to lower pH levels.
Causes: CO2 emissions from fossil fuels, deforestation.
Effects: harming marine life, especially organisms with calcium carbonate shells (e.g., coral reefs, shellfish).
Environmental Effects of Ozone
Stratospheric Ozone: Protects against UV radiation; depletion leads to increased UV levels impacting health and ecosystems.
Tropospheric Ozone: Harmful air pollutant; can cause respiratory issues and crop damage.
Human Health Impacts of Ozone Depletion
Increased risk of skin cancer, cataracts, and immune system suppression due to heightened UV exposure.
Economic Impact of Ozone Depletion
Increased healthcare costs due to UV-related illnesses.
Losses in agriculture and fisheries affecting livelihoods.
Scientific Data Supporting Global Warming
Increased frequency of extreme weather events.
Rising ocean temperatures and levels.
Melting glaciers and diminishing ice sheets.
Mitigating Global Warming
Transitioning to renewable energy sources (solar, wind).
Enhancing energy efficiency.
Reforestation and sustainable land use practices.
Economic Impacts of Global Warming
Increased disaster recovery costs.
Damage to infrastructure from extreme weather.
Shifts in agriculture affecting food supply and prices.
Effects on Human Health
Increased heat-related illnesses
Expansion of vector-borne diseases (e.g., malaria, dengue).
Effects on Biodiversity/Ecosystems
Habitat loss due to changing climate patterns.
Species migration and potential extinction due to inability to adapt.
Effects on Water Supplies
Changes in precipitation patterns affecting freshwater availability.
Increased evaporation rates leading to water scarcity.
Effects on Agriculture
Altered growing seasons impacting food production.
Pests and diseases may proliferate with warming temperatures.
Effects on Coral Reefs
Increased ocean temperatures leading to bleaching.
Ocean acidification weakening coral structures.
Sea Level Rise and Global Warming
Melting of ice caps contributes to higher sea levels.
Thermal expansion of seawater as it warms.
Impact of Sea Level Rise on Coastal Ecosystems
Coastal erosion affecting habitats and wildlife.
Increased flooding impacting estuarine environments.
Positive Feedback Loops in Global Warming
Melting polar ice reduces albedo, leading to increased heat absorption and further warming.
Thawing permafrost releases methane, enhancing the greenhouse effect.
Albedo
The measure of how much sunlight is reflected by a surface.
Ice and snow have a high albedo, while dark surfaces absorb more heat.
Diseases Linked to Climate Change
Malaria: Greater prevalence due to expanded mosquito ranges.
West Nile Virus: Increased due to warmer temperatures.
Cholera: Warming water bodies facilitate bacterial growth.
Zika, Plague, Tuberculosis, SARS, MERS, Dysentery: Epidemiological shifts related to changing climates.
Nuclear Power: Advantages and Disadvantages
Advantages: Low greenhouse gas emissions, high energy density.
Disadvantages: Radioactive waste, risk of catastrophic failure.
Renewable Energy Sources: Pros and Cons
Wind: Inexhaustible, eco-friendly but intermittent.
Hydroelectric: Reliable, low emissions, but ecological disruption.
Hydrogen Fuel Cells: Clean, renewable but expensive production methods.
Photovoltaic Solar: Abundant resource, but dependent on weather.
Biomass: Reduces waste, but agricultural competition for land.