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Year 9 Science Earth Sciences AC9S9U03

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