Notes on Global Climate Change
Intro to Global Climate Change
- Topic 9.5: Global Climate Change
- Divided into two parts due to complexity.
- Objective: Explain impacts of short/long-term climate changes on ecosystems.
- Practice skill: Use data to support a hypothesis.
Historic Long-Term Climate Change
Difference between anthropogenic and natural climate change.
Earth's Orbital Changes
Eccentricity: Variations in Earth's orbit from circular to elliptical over ~100,000 years.
Obliquity: Axial tilt of the Earth which affects sunlight received by Northern latitudes.
Both contribute to Milankovitch cycles, which are periodic changes in climate.
Evidence of Historical Climate Change
- Foraminifera Statues: Sediment layers containing shells indicate past temperatures based on species preferences.
- Ice Core Analysis: Air bubbles in ice contain atmospheric snapshots, revealing historical carbon dioxide levels.
- Oxygen Isotope Ratios: Ratio of heavy (O-18) to light oxygen (O-16) indicates temperature, with a higher presence of O-18 suggesting warmer periods.
Temperature and CO₂ Correlation
Historical temperature and CO₂ levels show strong correlation due to Milankovitch cycles.
Increasing CO₂ leads to more heat retention, with both being involved in a complex relationship.
Current CO₂ levels are the highest in 800,000 years, raising concerns about increasing global temperatures.
Impacts of Climate Change on Ecosystems
- Global Warming: Average surface temperatures on the rise, leading to habitat loss.
- Drought: Regions may experience prolonged dry spells affecting habitats and accelerating extinction rates.
- Increased Precipitation in Certain Areas: Some regions will become wetter due to changed atmospheric conditions.
- Soil Desiccation: Higher temperatures lead to drier soils, influencing agricultural viability.
- Rising Sea Level: Melting ice contributes to sea level rise, affecting marine and coastal ecosystems.
- Melting Permafrost: Leads to anaerobic decomposition producing greenhouse gases, creating a positive feedback loop.
Future Projections and Risks of Climate Change
The IPCC predicts significant ecosystem threats by a 2°C increase by 2100, including:
Loss or shift in ecosystems.
Increased extreme weather.
Risk of coral bleaching and coastal flooding.
Coastal Communities: Displacement risks due to rising sea levels; wealthier areas may adapt better.
Loss of Barrier Islands: Integral for protecting coastal ecosystems are at risk from inundation.
Impact on Atmospheric Circulation
Hadley Cell Changes: Expected to widen and weaken as polar regions warm more than equatorial regions, changing subtropical weather patterns.
Jet Stream Variability: Destabilized jet stream may lead to extreme weather patterns, as seen during the cold snap in 2014 attributed to climate change.
Explore maps illustrating temperature correlations in the U.S. to support hypotheses about jet stream impacts.