Chapter 12 Notes UPDATED
Chapter 12 Climate Change and Humans
Global Warming
The average temperature on Earth may increase due to global warming, but the concept of impact on the environment remains uncertain.
Potential effects could be both positive and negative for Canadians.
Positive Effects of a Warmer Climate in Alberta
Reduced Heating Needs: Warmer winters could lead to less fossil fuel consumption for heating.
Extended Growing Season: A longer growing season may benefit agriculture.
Shift in Climate Zones: Northern Alberta may become more suitable for agriculture as the taiga diminishes, making way for grasslands and deciduous forests.
Greenhouse Effect
Key Greenhouse Gases:
Water vapor
Carbon dioxide (CO2)
Methane (CH4)
Dinitrogen monoxide (N2O)
Halocarbons
Tropospheric ozone (O3)
Role of Water Vapor in the Greenhouse Effect
Water vapor accounts for about 65% of infrared radiation absorbed by Earth's surface.
Increased human activity raises greenhouse gases, leading to:
More water evaporation.
Potential enhancement of the greenhouse effect due to warmer atmospheres possibly holding more water vapor.
Enhanced Greenhouse Effect: Describes the cycle where warming leads to more water vapor, which in turn causes further warming.
The Greenhouse Mechanism
Sunlight enters a greenhouse, where it is absorbed and re-emitted as long-wave infrared radiation.
The greenhouse glass reflects infrared energy, further warming objects inside.
Similarly, Earth's heated surface radiates infrared energy which may be trapped by greenhouse gases.
The more greenhouse gases present, the more energy is retained, increasing Earth's temperature.
Essential Nature of the Greenhouse Effect
Without this effect, Earth's average temperature would be too low to support life.
Excessive greenhouse gases could lead to dangerously high temperatures, threatening life sustainability.
Feedback Mechanisms
Positive Water Vapor Feedback
Increased warming leads to more water vapor, perpetuating the initial warming effect.
Negative Water Vapor Feedback
More water vapor may cause cloud formation that reflects sunlight, inducing a cooling effect.
Research supports that positive feedback appears to dominate.
Deforestation
The clearing of trees has significant repercussions on:
Biodiversity
Climate stability
Atmospheric composition (trees consume CO2 for oxygen during photosynthesis)
Deforestation is often done for:
Lumber and firewood
Agricultural land
Deforestation Challenges
Cleared areas in rainforests yield poor agricultural conditions due to nutrient-poor soil.
Tree removal releases CO2 into the atmosphere, accounting for about 25% of global CO2 emissions from human activities.
The Carbon Cycle Contributions
Various components of the carbon cycle include:
Atmosphere, vegetation, oceans, and fossil fuels, with their respective carbon reservoirs.
Precautionary Principle
The 1992 Rio Declaration advocates for a precautionary approach to environmental threats, promoting cost-effective measures to prevent degradation even amid scientific uncertainty.
Gaia Hypothesis
Proposed by Dr. James Lovelock in the 1960s, it suggests:
Earth functions as a single, interconnected living organism.
All forms of life contribute to maintaining the environment suitable for life.
Complexity of the Biosphere
The biosphere interacts through complex systems to provide an optimal environment for living organisms.
Skepticism on Global Warming
Some scientists, such as Richard Lindzen, argue that:
The threat of global warming may be overstated.
Human contributions to global warming may not be as significant as perceived.
Assignments
Reference Assignment BLM 12-6 on page 27 for further studies.