Schroder, Klaus-Peter · Sussex Research Online (University of Sussex) 2008 · computational simulation · n=?

Distant future of the Sun and Earth revisited

Cited 163 times in the scientific literature.

Level 5 - mechanism / opinion, no new human data

Level 5 by design analogy, not clinical CEBM (computational astrophysical modeling and theoretical simulation).

OpenAlex W3099060193 · doi:10.48550/arxiv.0801.4031 · record verified 2026-08-31

What was done

The authors computed stellar evolution models using a calibrated cool-wind mass-loss formula to simulate the distant future of the Sun and the solar system. For each time-step during the red giant phases, the model evaluated solar mass loss, Earth's resulting orbital expansion, and counteracting orbital angular momentum losses from tidal interactions and dynamical drag in the lower solar chromosphere.

What was found

The Sun is modeled to lose 0.332 solar masses by the tip-RGB phase (7.59 billion years from now). Tidal interaction and chromospheric drag overcome orbital expansion, resulting in Earth's engulfment during the tip-RGB phase. Planetary survival would require a present-day minimum orbital radius of approximately 1.15 AU. Due to heavy RGB mass loss, the subsequent tip-AGB giant will not exceed its tip-RGB size or drive a standard planetary nebula, producing at most a small circumstellar shell of a few hundredths of a solar mass.

Why it matters

This work provides an updated astrophysical model for the ultimate fate of the solar system, demonstrating that tidal dissipation counteracts mass-loss expansion to cause Earth's engulfment.

Limits

The findings depend entirely on theoretical evolutionary codes, parameterized mass-loss formulations, and simplified models of tidal coupling and chromospheric drag, none of which can be empirically observed for the future Sun.

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