Causation

Positive Feedback Amplification Beyond a Tipping Point

When a system is pushed beyond a tipping point by a large shock, the dynamic shifts from self-correcting to self-reinforcing. Instead of being dampened by negative feedback, the initial shock is amplified by a positive feedback process. In the Arctic climate model, for example, a reduction in sea ice below the tipping point triggers positive feedback that further reduces ice cover, driving the system toward a new low-ice equilibrium.

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Updated 2025-08-08

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