What is Earth's future warming due to the Sun's increasing luminosity?

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Discussion Overview

The discussion centers on the future warming of Earth due to the Sun's increasing luminosity, particularly in the context of long-term changes over billions of years. Participants explore the implications of solar evolution, the potential for life on Earth, and the effects of atmospheric composition on temperature changes.

Discussion Character

  • Exploratory
  • Technical explanation
  • Debate/contested
  • Mathematical reasoning

Main Points Raised

  • Some participants note that the Sun will eventually become a red giant, leading to extreme temperatures on Earth, but they seek to quantify the expected rise in temperature solely due to increased solar luminosity while holding atmospheric composition constant.
  • Others express skepticism about the timeline for when conditions will become uninhabitable for life due to changes in solar output, questioning whether this is based on scientific understanding or popular science.
  • A participant presents a mathematical model for solar luminosity evolution, suggesting a 1% increase in solar intensity per 100 million years, leading to significant temperature increases over a billion years, assuming constant climate sensitivity and albedo.
  • There is mention of the relationship between solar intensity and radiative forcing, with calculations indicating a potential increase of about 20 K in temperature over a billion years, with total temperatures exceeding 400 K towards the end of the Sun's life on the main sequence.
  • Some participants express concern about the implications of these temperature increases in the context of current climate change discussions, particularly regarding CO2 levels.

Areas of Agreement / Disagreement

Participants do not reach a consensus on the timeline for when Earth will become uninhabitable or the specific temperature increases due to solar luminosity. Multiple competing views and uncertainties remain regarding the assumptions and implications of the discussed models.

Contextual Notes

Limitations include assumptions about constant atmospheric composition, climate sensitivity, and albedo, which may not hold true over long timescales. The discussion also reflects varying interpretations of the scientific understanding of solar evolution and its effects on Earth.

swampwiz
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TL;DR
Presuming the same CO2, etc. level as today, what would be the rise in the average temperature of Earth due solely to the Sun's future rise in luminosity?
Obviously, at some point, the Sun will be a red giant, and it's going to be very, very hot on Earth. I'd like to know what the expected rise in temperature would be due solely to the Sun, while holding the composition of the Earth's atmosphere constant - or at least constant except for the gas that would be escaping due to the hot temperature.
 
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Forget about ##CO_2## et al. Long before the sun will become a red giant it will be too hot for our lifeforms. AFAIK this will start at some point when the ratio of helium fusion to hydrogen fusion gets too high.

I'm interested as well, whether this is actually true or just pop science knowledge, and when it will be the case. Certainly long before the rest of 4.5 billion years.
 
fresh_42 said:
Forget about ##CO_2## et al. Long before the sun will become a red giant it will be too hot for our lifeforms. AFAIK this will start at some point when the ratio of helium fusion to hydrogen fusion gets too high.

I'm interested as well, whether this is actually true or just pop science knowledge, and when it will be the case. Certainly long before the rest of 4.5 billion years.
I abstracted out the idea of the ratio of helium fusion to hydrogen fusion with the term "luminosity".

https://en.wikipedia.org/wiki/Solar_luminosity
 
swampwiz said:
Summary: Presuming the same CO2, etc. level as today, what would be the rise in the average temperature of Earth due solely to the Sun's future rise in luminosity?

Obviously, at some point, the Sun will be a red giant, and it's going to be very, very hot on Earth. I'd like to know what the expected rise in temperature would be due solely to the Sun, while holding the composition of the Earth's atmosphere constant - or at least constant except for the gas that would be escaping due to the hot temperature.
Based off of what I've read. A few billion years from now the sun will become a red giant. It will burn away the atmosphere, scorch the Earth and kill all life on Earth.

I'm wondering if your question is more around the sun's 11-year cycle of solar output? Sun's impact on climate change
 
HankDorsett said:
Based off of what I've read. A few billion years from now the sun will become a red giant. It will burn away the atmosphere, scorch the Earth and kill all life on Earth.

I'm wondering if your question is more around the sun's 11-year cycle of solar output? Sun's impact on climate change

No, it's the very, very long-term increase in luminosity I'm getting at - the one that is shown in that Wikipedia article.
 
swampwiz said:
what would be the rise in the average temperature of Earth due solely to the Sun's future rise in luminosity?
Here's what I came up with:
The long-term solar luminosity evolution on the main sequence can be approximated by the following equation (Gough, 1981):
$$\frac{L(t)}{L_0}=\frac{1}{1+\frac{2}{5}(1-\frac{t}{t_0})}$$
where ##L_0## is current solar luminosity and ##t_0## is present-day.
1564577699214.png

This translates to roughly 1% increase in solar intensity per 100 million years, at least in the relatively near future.

The relationship between equilibrium temperature and radiative forcing is $$\Delta T=\lambda\Delta F$$ where ##\lambda## is climate sensitivity - here we'll use 0.8 after Wikipedia.
The relationship between solar intensity (flux) and radiative forcing is $$\Delta F=\frac{1}{4}\Delta I*(1-\alpha)$$
The 1/4 factor is from Earth cross-section to surface area. ##\alpha## is albedo (approx. 0.3).

The result, assuming climate remains as sensitive as it is today and albedo doesn't change (both unreasonable assumptions):
1564580699220.png

So, under these assumptions (including the one about me not messing up), it would be about 20 K hotter in a billion years and over 400 K total towards the end of Sun's life on the main sequence.
When it goes red giant, depending on mass loss it might (or not) envelop Earth, in which case the latter will evaporate.
 
Bandersnatch said:
Here's what I came up with:
The long-term solar luminosity evolution on the main sequence can be approximated by the following equation (Gough, 1981):
$$\frac{L(t)}{L_0}=\frac{1}{1+\frac{2}{5}(1-\frac{t}{t_0})}$$
where ##L_0## is current solar luminosity and ##t_0## is present-day.
View attachment 247370
This translates to roughly 1% increase in solar intensity per 100 million years, at least in the relatively near future.

The relationship between equilibrium temperature and radiative forcing is $$\Delta T=\lambda\Delta F$$ where ##\lambda## is climate sensitivity - here we'll use 0.8 after Wikipedia.
The relationship between solar intensity (flux) and radiative forcing is $$\Delta F=\frac{1}{4}\Delta I*(1-\alpha)$$
The 1/4 factor is from Earth cross-section to surface area. ##\alpha## is albedo (approx. 0.3).

The result, assuming climate remains as sensitive as it is today and albedo doesn't change (both unreasonable assumptions):
View attachment 247377
So, under these assumptions (including the one about me not messing up), it would be about 20 K hotter in a billion years and over 400 K total towards the end of Sun's life on the main sequence.
When it goes red giant, depending on mass loss it might (or not) envelop Earth, in which case the latter will evaporate.
Yes, this analysis is what I was looking for. Thanks

OK, so the concern about CO2-genic global warming at +2K would have been realized in 100 million years in a static-CO2 situation.
 
Last edited:
I have so much and many thoughts I cannot rigorously prove I will stop myself at "That is quite a conclusion to draw."
 

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