Habitable Zones

Onset Of Habitable Conditions On The Hadean Earth Set By Feedback Between Tides And Greenhouse Forcing

By Keith Cowing
Status Report
astro-ph.EP
November 4, 2025
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Onset Of Habitable Conditions On The Hadean Earth Set By Feedback Between Tides And Greenhouse Forcing
Evolution of nominal-composition cases across the full range of fO2 and tidal power densities simulated (see Section 2.3). Panel A (left): stages in planet’s lifetime after model initialization. Dotted lines trace cumulative tidal heat dissipation; marker size increases with total dissipated energy. Solid lines indicate tidally-supported GRE states; black vertical bars (||) mark tVMR. Crosses (×) denote solidification, defined at ϕ < 0.005. Panel B (right): volume mixing ratios of volatiles at tVMR — astro-ph.EP

In the aftermath of the Moon-forming giant impact, the Hadean Earth’s mantle and surface crystallized from a global magma ocean blanketed by a dense volatile-rich atmosphere.

While prior studies have explored the thermal evolution of such early Earth scenarios under idealized, oxidizing conditions, the potential feedback between tidal heating driven by Earth–Moon orbital forcing and variable redox scenarios have not yet been explored in detail.

We investigate whether tidal heating could have prolonged this early magma ocean phase and supported quasi-steady state epochs of global radiative equilibrium: periods of thermal balance between outgoing radiation and interior heat flux. Using the 𝙿𝚁𝙾𝚃𝙴𝚄𝚂 simulation framework, we simulate Earth’s early evolution under a range of plausible tidal power densities, oxygen fugacities, and volatile inventories.

Our results suggest that feedback between tidal heating and atmospheric forcing can induce substantial variation in magma ocean lifetimes, from ∼30 Myr up to ∼500 Myr, sensitive to interior redox conditions. Global radiative equilibrium epochs commonly arise across this range, lasting from ∼2 to ∼320 Myr, and typically occur from 24 Myr after the Moon-forming impact.

Under oxidizing conditions, late-stage H2O degassing promotes melt retention and sustained heating due to its significant contribution to greenhouse forcing. Weak tides increase the atmospheric abundance of H2S and NH3 and deplete CO. Therefore, the feedback between tides and atmospheric forcing induces a disequilibrium signature in the magma ocean atmosphere.

Marijn R. van Dijk, Harrison Nicholls, Tim Lichtenberg

Comments: 14 figures, 9 pages. under review, comments welcome
Subjects: Earth and Planetary Astrophysics (astro-ph.EP); Atmospheric and Oceanic Physics (physics.ao-ph); Geophysics (physics.geo-ph)
Cite as: arXiv:2511.00952 [astro-ph.EP] (or arXiv:2511.00952v1 [astro-ph.EP] for this version)
https://doi.org/10.48550/arXiv.2511.00952
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Submission history
From: Marijn Van Dijk
[v1] Sun, 2 Nov 2025 14:26:45 UTC (658 KB)
https://arxiv.org/abs/2511.00952

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