Numerical Simulation of the Viscous-like Flow in and Around the Plasma Tail of a Comet

TL;DR

This paper presents a numerical simulation model of viscous-like flow in a comet's plasma tail, analyzing how viscous effects influence solar wind interactions and matching in situ measurements from the Giotto spacecraft.

Contribution

Developed a 2D hydrodynamical simulation incorporating viscous-like forces to study plasma flow around a comet, highlighting the significance of viscous effects in solar wind interactions.

Findings

Flow exhibits three transitions depending on Reynolds number and coupling timescales.

Model aligns qualitatively with Giotto measurements for low Reynolds numbers (<100).

Viscous-like processes may significantly influence solar wind-comet plasma interactions.

Abstract

We model the interaction of the solar wind with the plasma tail of a comet by means of numerical simulations, taking into account the effects of viscous-like forces.A 2D hydrodynamical, two species, finite difference code has been developed for the solution of the time dependent continuity, momentum and energy conservation equations, as applied to the problem at hand. Velocity, density and temperature profiles across the tail are obtained. Several cases with different flow parameters are considered in order to study the relative importance of viscous-like effects and the coupling between species on the flow dynamics. Assuming a Mach number equal to 2 for the incident solar wind as it flows past the comet nucleus, the flow exhibits three transitions with location and properties depending on the Reynolds number for each species and on the ratio of the timescale for inter-species coupling to the crossing time of the free flowing solar wind. By comparing our results with the measurements taken in situ by the Giotto spacecraft during its flyby of comet Halley we constrain the flow parameters for both plasmas. In the context of our approximations, we find that our model is qualitatively consistent with the in situ measurements as long as the Reynolds number of the solar wind protons and of cometary H2O+ ions is low, less than 100, suggesting that viscous-like momentum transport processes may play an important role in the interaction of the solar wind and the plasma environment of comets.