Negative feedback loops
Negative feedback loops are processes where the output of a system acts to reduce or reverse changes, helping the system maintain stability.
- Feedback refers to processes in which the output or result of a system influences its own operation.
- Negative feedback loops are mechanisms that counteract change, helping systems maintain stability and equilibrium.
- They play a critical role in both natural ecosystems and human physiological systems, preventing extreme fluctuations that could threaten survival.
- Negative feedback loops are essential to homeostasis (in biological systems) and equilibrium (in ecological and planetary systems).
Negative feedback loops can be represented through systems diagram.
Mechanism of Negative Feedback
- Begins with a system in equilibrium, where inputs and outputs are balanced.
- A disturbance or external factor disrupts this balance (for example, a change in temperature, population size, or resource availability).
- The system responds in a way that reduces or reverses the initial change, restoring stability.
- This regulation ensures that systems fluctuate around an average condition rather than moving progressively away from it.
Predator-Prey Relationship
- When prey numbers increase, predators have more food and their population grows.
- As predator numbers rise, more prey are consumed, reducing prey abundance.
- With less prey available, predator numbers then decline due to food scarcity.
- The reduction in predator numbers allows the prey population to recover, and the cycle repeats.
- This ongoing cycle keeps both populations relatively stable around a long-term average
Carbon Cycle and Climate Regulation
- An environmental-scale feedback loop.
- When CO₂ levels increase:
- Higher temperatures enhance plant photosynthesis and biomass growth.
- Increased plant uptake reduces atmospheric CO₂.
- This moderates the greenhouse effect.
- When CO₂ decreases: Cooler conditions slow photosynthesis, allowing CO₂ to build up again.
- This stabilizing process prevents Earth’s climate from diverging dramatically over short timescales.
Hydrological Cycle and Cloud Feedback
- Increased global temperatures enhance evaporation → more cloud formation.
- Clouds reflect incoming solar radiation (high albedo), which reduces heating.
- As the planet cools, evaporation and cloud formation decrease again.
- This negative feedback moderates the Earth’s temperature within narrow limits.
Forest Canopy Regeneration
- When strong winds or storms blow down trees, gaps appear in the forest canopy.
- Increased sunlight stimulates rapid growth of understory plants and saplings.
- New vegetation fills the gap, re-establishing canopy cover and restoring the microclimate.
- This demonstrates self-restoration through negative feedback.
Temperature Regulation in the Human Body
- Human homeostasis offers a biological analogy for environmental feedback.
- When body temperature rises, mechanisms such as sweating and vasodilation cool the body.
- When the temperature drops, shivering and vasoconstriction increase heat production and retention.
- These opposing processes stabilize body temperature around 37°C, a biological steady-state equilibrium.
Daisyworld Model
- Developed by James Lovelock and Andrew Watson as part of the Gaia hypothesis, which proposes that life on Earth helps regulate environmental conditions.
- Daisyworld is a computer simulation of a hypothetical planet orbiting a star with gradually increasing luminosity (heat).
- The model shows how life can stabilize planetary temperature through negative feedback mechanisms.


