Is Earth's Thermal Feedback Loop Unstable?

In summary, the article explores the concept of Earth's thermal feedback loop, examining its stability and potential implications for climate change. It discusses how feedback mechanisms, such as the ice-albedo effect and greenhouse gas emissions, can amplify warming. The analysis highlights concerns about tipping points and the possibility of an unstable feedback loop that could lead to accelerated climate change, emphasizing the need for further research and understanding of these complex interactions.
  • #1
stuartmacg
28
6
TL;DR Summary
Published CO2 and T data seem to imply unstability.
Looking at some apparently widely accepted data, I understand:

- CO2 mass change => direct "greenhouse" heating is approx linear over ranges considered
- Doubling CO2 (i.e. adding same again) would give 1C change for direct greenhouse.
- CO2 change x1.5 since pre-industrial times (half added), hence direct greenhouse would be 0.5C
- delta T has been observed to be 1C in same period, and attributed to CO2 increase.
- this suggests feedback gain around 1 => nearly unstable heat in-> heat out loop
- heat may generate some net CO2 directly e.g. by warmed sea out gassing
- this would suggest the thermal loop (even without any external forcing) is unstable, gain>1

An unstable Earth might change between 2 saturating temperatures, with little external "forcing". Saturating regions could have loop gains just below 1.
I expect there are flaws in the above, but it would be interesting to find out where.
 
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  • #2
You are assuming the system is linear.
If there is a tipping point, the system will be non-linear.
 
  • #3
I am not clear that that is so. A loop gain becoming >1 would generate exponential increases i.e. a "tipping point", in an otherwise linear system (e.g. microphone howl).
Non linear, second order, effects are what would change the loop gain, and create stable "saturation" levels.
What non linearities are you suggesting?
 
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  • #4
I see a "tipping point" as being a point where the gain of the system changes. It does not need to become greater than +1, it could just change sign, inducing a change in the trajectory of the system state.
 
  • #5
Our replies crossed. The observed T and CO2 changes and (I am told) agreed direct CO2 heating effect together suggest that there is a purely thermal loop gain close to 1, required to amplify the CO2 "forcing" change from 0.5C to the observed 1C.
 
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  • #6
I made a foolish mistake: feedback effectively generates a geometric series, so if the result is to double the input, the feedback gain is 1/2, not 1. i.e. factor=1/(1-gain).
 
  • #8
Thanks for the links. I'll work my way through this stuff.
 

FAQ: Is Earth's Thermal Feedback Loop Unstable?

What is Earth's thermal feedback loop?

Earth's thermal feedback loop refers to the processes that regulate the planet's temperature through interactions between the atmosphere, oceans, land, and ice. It involves mechanisms such as the greenhouse effect, where gases trap heat, and feedbacks like melting ice, which reduces the Earth's albedo (reflectivity), leading to further warming.

What are the main factors contributing to the instability of Earth's thermal feedback loop?

The instability of Earth's thermal feedback loop can be attributed to several factors, including increased greenhouse gas emissions, changes in land use, deforestation, and the melting of polar ice. These factors can amplify warming through positive feedback mechanisms, making it difficult to predict future climate scenarios accurately.

How does climate change impact the thermal feedback loop?

Climate change impacts the thermal feedback loop by altering the balance of energy entering and leaving the Earth's system. Increased temperatures can lead to more water vapor in the atmosphere, which is a potent greenhouse gas. Additionally, the melting of ice caps reduces the Earth's albedo, causing more solar energy to be absorbed and further increasing temperatures.

Are there signs that Earth's thermal feedback loop is becoming unstable?

Yes, there are several signs indicating that Earth's thermal feedback loop may be becoming unstable. These include accelerated ice melt in Greenland and Antarctica, increased frequency and intensity of extreme weather events, and rising ocean temperatures. These changes suggest that feedback mechanisms are amplifying warming trends, potentially leading to tipping points.

What can be done to stabilize Earth's thermal feedback loop?

To stabilize Earth's thermal feedback loop, it is essential to reduce greenhouse gas emissions through transitioning to renewable energy sources, improving energy efficiency, and implementing sustainable land-use practices. Additionally, protecting and restoring natural carbon sinks, such as forests and wetlands, can help mitigate the effects of climate change and promote a more stable thermal feedback loop.

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