Concept

Effect of Large Shocks on a Stable Equilibrium

While a stable equilibrium can recover from small shocks via negative feedback, a sufficiently large shock can push the system beyond its tipping point. For instance, in the climate model, if a series of unusually hot years reduces sea ice extent below the unstable equilibrium (point T), the system's self-correcting mechanism fails. Instead, a positive feedback loop is initiated, driving the system towards a different, less desirable equilibrium.

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Updated 2026-05-02

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