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.
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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):
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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.