Multifluid MHD model for comet 1P/Halley
Transcription
Multifluid MHD model for comet 1P/Halley
Comet 1P/Halley Multifluid MHD model for the Giotto Fly-By M. Rubin, M. R. Combi, L. K. S. Daldorff, T. I. Gombosi, K. C. Hansen, Y. Shou, V. M. Tenishev, G. Tóth, B. van der Holst, and K. Altwegg Rubin et al. 2014, ApJ, 781, 86 Model description Individual ion fluids with their own continuity (mi), momentum (miuxi, miuyi, miuzi), and pressure equations (pi) - SWp+ (Origin: SW, only sinks inside the model) - H2O+ (Origin: Photoionization of cometary neutrals) - H+ (Origin: Photoionization of cometary neutrals) - separate electron pressure equation (pe→Te) Neutral gas (analytic description) H2O is described by a Haser model H, H2 is fitted to Combi (1996) Included physics : - Photoionization & dissociation, electron-impact ionization - Ion-electron recombination - Ion-neutral charge exchange (through friction term) - Lorentz-force interaction between the fluids - Elastic collision (ion-ion, ion-electron, ion-neutral, electron-neutral) - Electron heating by photoelectrons - H2O cooling of electrons (inelastic electron-H2O collisions) - UV absorption by photoionization Modeled species Model input Results • Comparison with Giotto observations • Overview of the different plasma species Nucleon density [amu/cm ] 3 Density 5 106 10 2 3 104 10 10 0 101 10 10-1 10 2 10 3 4 10 6 JPA protons BATS-R-US solar wind protons BATS-R-US cometary light ions JPA heavy ions IMS HIS 12-32 amu ions BATS-R-US cometary heavy ions 5 10 10 Distance to comet [km] 10 Electron temperature Temperature [K] 106 105 104 103 102 101 10 2 10 3 4 10 6 Gombosi et al. (1996) Eberhardt and Krankowsky (1995) BATS-R-US 5 10 10 Distance to comet [km] 10 0 -400 200 400 600 Neubauer (1987) BATS-R-US Universal Time Closest Mar 14, 1986 Mar 14, 1986 Approach 00:08 00:13 0 Time from closest approach [s] -200 1986 Mar 13, 1986 53 23:58 Magnetic field Plasma velocities Velocity [km/s] 1000 100 10 1 0.1 2 10 10 3 5 10 6 JPA protons BATS-R-US solar wind protons BATS-R-US cometary light ions JPA heavy ions IMS HIS Mass Analyzer 12-32 amu ions IMS HIS Angle Analyzer 12-32 amu ions IMS HERS 12-32 amu ions BATS-R-US cometary heavy ions 4 10 10 Distance to comet [km] 10 Plasma temperatures Temperature [K] 7 108 10 4 5 106 10 10 2 103 10 101 10 2 10 3 4 10 6 JPA protons BATS-R-US solar wind protons BATS-R-US cometary light ions JPA water group IMS HIS Mass analyzer water group IMS HIS Angle analyzer water group IMS HERS water group BATS-R-US cometary heavy ions 5 10 10 Distance to comet [km] 10 Density Lorentz-force Magnetic field Temperatures Conclusions • Multifluid MHD seems to be doing a reasonable job in fitting Giotto plasma observations • Co-located inner shock for cometary species • Ion pile-up does not necessarily peak at the same location for the different species • Solar wind absent from the innermost region • Lorentz-force interaction between the fluids can be observed (non-vanishing Bx component)