Climate Feedback Mechanisms
Climate feedback mechanisms amplify or dampen the initial effects of climate change. Understanding positive and negative feedbacks is essential to modelling future climate scenarios.
What You Need to Know
Key Concept Diagram
Positive feedback amplifies change: melting Arctic ice reduces albedo, absorbing more heat, causing more melting
Negative feedback dampens change: warmer oceans increase evaporation and cloud cover, reflecting more sunlight
Water vapour feedback is a major positive feedback in climate warming
Methane release from permafrost as temperatures rise is a significant positive feedback
Key Vocabulary
Positive feedback
A feedback mechanism that amplifies the original change in a system
Negative feedback
A feedback mechanism that dampens or reduces the original change in a system
Albedo
The proportion of solar energy reflected by a surface; ice has high albedo
Permafrost
Permanently frozen ground that stores large amounts of carbon and methane
Knowledge Check
Select the correct answer for each question. Click "Check Answer" to see if you are right.
Question 1
Arctic sea ice melting reduces albedo and causes further warming. This is a:
Question 2
If increased evaporation from warmer oceans leads to more cloud cover and more sunlight being reflected back to space, this is a:
Question 3
Why is methane release from melting permafrost a concern for climate scientists?
Key Concepts Summary
- ●Positive feedback amplifies change: melting Arctic ice reduces albedo, absorbing more heat, causing more melting
- ●Negative feedback dampens change: warmer oceans increase evaporation and cloud cover, reflecting more sunlight
- ●Water vapour feedback is a major positive feedback in climate warming
- ●Methane release from permafrost as temperatures rise is a significant positive feedback