Modelling the Neutral Sodium Tails of Comets
Abstract:
At present the source of neutral sodium in comets is unknown, primarily because the evolution of neutral cometary sodium is difficult to intuitively predict due to the Swings and Greenstein effects. Several authors [review presented in Cremonese et al, 1999] have suggested various combinations of sources of neutral sodium in the nuclear region, near-nuclear region, dust tail and ion tail.
In order to understand the wide variety of cometary observations of neutral sodium available we have developed the first fully three dimensional, heliocentric distance dependent, versatile Monte Carlo neutral sodium tail model (initially based on a model developed by [Brown et al, 1998]). Our model is known as COMPASS (Cometary Orbital Motion at Perihelion: an Adaptable Sodium Simulation), and incorporates the unintuitive variation in radiation pressure influences on sodium atoms with different heliocentric velocities.
We present the initial results of a comparison between COMPASS and observational data. We have found good agreement between the overall morphology of the neutral sodium tail imaged at comet Hale-Bopp and COMPASS, and have begun to extend the study to other comets of interest. We also present a comparison between simulated COMPASS spectra and observations. The versatility of COMPASS allows it to be easily adapted to any other neutral cometary sodium tail observations available.
