Synchronisation of a tidal binary by inward orbital migration. The case of Pluto and Charon

TL;DR

This paper explores how the Pluto-Charon system could have achieved mutual synchronization through tidal approach rather than recession, analyzing the conditions, scenarios, and geophysical implications of such evolution.

Contribution

It introduces a detailed analysis of tidal approach synchronization, compares it with tidal recession, and applies it to the Pluto-Charon system considering capture and spin-reversal scenarios.

Findings

Capture scenario is more consistent with geophysical evidence.

Temporary spin-orbit resonances can occur during early evolution.

Lower tidal stress and dissipation explain lack of fracture patterns.

Abstract

It is usually taken for granted that mutual synchronisation of a tidal two-body system is attained through tidal recession, assuming the reduced Hill sphere is not reached. However, synchronisation can be achieved also via tidal approach, provided the Roche limit is not crossed. For each of the two scenarios, we derive the condition under which the evolving synchronicity radius catches up with the tidally evolving orbit. We consider the two scenarios for the Pluto-Charon system and examine the impact-origin hypothesis of Charon's formation against capture. Based on geophysical evidence, we propose that capture appears more likely. Motivated by this conclusion, we investigate the capture scenario, wherein the orbital evolution of Charon starts at a larger distance than present and undergoes tidal descent, both analytically and numerically. We also consider the possibility that Pluto's initial prograde spin underwent a reversal by a tidally approaching retrograde Charon. Depending on the initial conditions, we observe temporary locking of Charon into higher spin-orbit resonances (3:2 to 7:2) during the first 0.5 Myr of the system's evolution. Owing to a greater initial separation between the partners, the power dissipated in each of them turns out to be much lower than in the case of tidal recession of bodies of the same internal structure. The greater initial separation also results in lower tidal stress, which may explain the absence of tidally generated fracture patterns.