Positive feedback loop
Positive feedback loops are processes that exacerbate the effects of a small disturbance.
- A positive feedback loop occurs when a disturbance amplifies itself, pushing a system further away from equilibrium rather than restoring balance.
- This can cause rapid and sometimes irreversible changes in natural and human systems.
Positive feedback loops can be shown through systems diagram.
How Positive Feedback Loops Work
- Positive feedback amplifies initial disturbances rather than counteracting them.
- The system experiences self-reinforcing cycles, where outputs act to strengthen the original process.
- Over time, these loops destabilize the system and may lead to a new equilibrium or even system collapse.
- Unlike negative feedback, which stabilizes a system, positive feedback accelerates change in either direction (increase or decrease).
- Population Growth → More people reproduce → Even larger population increase (Exponential Growth).
- Species Extinction → Fewer individuals remain → Harder to find mates → Further population decline (Extinction Vortex).
Key Characteristics
- Destabilizing: drives systems away from equilibrium.
- Amplifying: increases deviation from the initial state.
- Nonlinear: changes accelerate over time rather than occur proportionally.
- Common in human and natural systems such as climate processes, population dynamics, and resource depletion.
Melting Ice-Albedo Feedback (Climate System)
Process
- Global temperatures rise due to greenhouse gas emissions.
- Ice caps and glaciers melt, reducing surface reflectivity (albedo).
- Less sunlight is reflected, and more solar radiation is absorbed by darker ocean or land surfaces.
- Temperatures rise further, accelerating more ice melt.
Result
- A self-reinforcing cycle of warming and melting that destabilizes the climate system.
- Leads to positive feedback between energy absorption and temperature increase.
Long-Term Implication
- The system moves away from its original equilibrium toward a new, warmer climate regime.
- Melting Arctic sea ice contributes to sea-level rise, ocean circulation changes, and increased climate extremes.
Higher temperature → ice melt → lower albedo → more heat absorption → higher temperature.
Population Growth and Decline
Population Growth Feedback
- As population increases, reproductive potential (number of breeding individuals) also increases.
- This leads to more births, further increasing population size.
- The larger the population, the faster it grows — an exponential growth loop.


