Climate Change Lecture Notes
Climate vs. Weather
- Weather: The condition of the atmosphere in a specific area at a given time.
- Climate: The long-term average of weather conditions in an area.
- Major elements of both include:
- Temperature
- Air pressure
- Wind
- Solar energy
- Humidity
- Precipitation
- Topography
Key Terminology
- Greenhouse Effect: A natural process where certain gases in the atmosphere trap heat, keeping the Earth warm.
- Global Warming: Refers specifically to the increase in Earth's average surface temperature due to rising levels of greenhouse gases.
- Climate Change: A broader term that includes any change in climate over time, whether due to natural variability or human activity.
The Greenhouse Effect
- Process:
- Solar radiation passes through the atmosphere.
- Some is reflected back to space, while some is absorbed and re-emitted by greenhouse gases.
- This process warms the Earth's surface and the lower atmosphere.
- Key Gases: Carbon dioxide (CO2), methane (CH4), nitrous oxide (N2O), and chlorofluorocarbons (CFCs).
- Importance: This process is essential for life on Earth, but human activities have enhanced it, causing global warming.
Measuring Global Average Temperature
- Scientists gather temperature measurements from various locations around the globe.
- They convert these to temperature anomalies: the difference from long-term averages.
- Multiple independent analyses show a consistent upward trend in global temperatures.
Understanding Temperature Anomalies
- Positive Anomalies: Above average temperatures.
- Negative Anomalies: Below average temperatures.
Natural vs. Anthropogenic Factors
- The Earth has undergone natural warming periods, but current changes are largely attributed to human activities, mainly fossil fuel combustion and deforestation.
- Astronomical factors can also affect climate cycles (e.g., Earth's orbital variations).
Composition of Earth's Atmosphere
- Mostly nitrogen and oxygen.
- Permanent Gases: Constant concentrations.
- Variable Gases: Fluctuate due to natural processes and human activities.
Global Warming Potential (GWP)
- A measure comparing how much heat a greenhouse gas traps in the atmosphere relative to CO2, which has a GWP of 1.
- Examples of GWP:
- Methane: 28–36 times greater than CO2.
- Nitrous Oxide: 265–298 times greater than CO2.
Sources of Carbon Dioxide
- Human activities contribute 87% of CO2 emissions, primarily from burning fossil fuels. Deforestation and agriculture also play significant roles.
Impact of Emissions and Climate Change
- Rising global temperature: Averaged about 1.53°F (0.85°C) increase from 1880 to 2012.
- Extreme Weather: Increasing frequency and intensity of hurricanes, floods, and droughts.
- Melting Ice: Decreased sea ice and rising sea levels, significantly impacting biodiversity and human settlements.
Paleoclimate Evidence
- Ice Cores: Provide historical climate data through trapped gases and isotopes.
- Tree Rings: Rings reveal climatic conditions over time.
- Ocean Sediment: Accumulation of marine organisms reflects past temperatures and ice cover.
The Keeling Curve
- Represents the increase of atmospheric CO2 levels since measurements began in 1957 at Mauna Loa Observatory.
Indicators of Climate Change
- Humidity, global temperatures, sea-level rise, ocean heat content, glacial retreat, and snow cover are major indicators of climate warming.
Impacts of Climate Change
- Global temperature rise, ice melting, sea-level rise, altered precipitation patterns, and extreme weather events all signal significant changes in our climate.
Conclusion
- Climate change poses threats on multiple fronts, affecting natural ecosystems and human societies.
- Responses must include both mitigation and adaptation strategies to navigate these challenges effectively.