Climate feedback loops are processes that can either amplify or dampen the effects of climate change. There are two types:

• Positive Feedback: Accelerates warming.

• Negative Feedback: Reduces warming.

Examples of Positive Feedback:

• Ice-Albedo Effect: Melting ice reduces Earth's reflectivity (albedo), so more sunlight is absorbed, causing further warming and melting.

• Permafrost Thaw: Melting permafrost releases methane, a potent GHG, intensifying warming.

Examples of Negative Feedback:

• Increased plant growth due to higher CO₂ levels may absorb more CO₂.

• Cloud formation could reflect sunlight and cool the Earth.

Understanding these loops is critical in predicting future climate scenarios and planning mitigation efforts.