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NASA NTRS · 19930036985

Quasi-linear velocity space diffusion of heavy cometary pickup ions on bispherical diffusion characteristics

Abstract

We consider an ion transport equation describing the source, convection, adiabatic acceleration, and quasi-linear velocity diffusion of cometary pickup ions. The equation is solved numerically along solar wind plasma flow lines for the environment of Comet Halley, to obtain distributions at positions on the Giotto spacecraft trajectory which may be compared with observations. We obtain full two-dimensional (pitch angle and velocity) numerical distributions which show pitch angle scattering about the wave scattering centers at +/- V(A), where V(A) is the Alfven wave speed in the solar wind frame. Peak ion phase-space densities approximately follow the bispherical shell geometry. The energy distributions F(v) agree well with Giotto observations at lower v, but in the high-energy tail there is evidence possibly for the first-order Fermi acceleration mechanism taking place in the Comet Halley foreshock region.

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BibTeXRIS

Huddleston, D. E., Coates, A. J., Johnstone, A. D.. 1992-12-01. Quasi-linear velocity space diffusion of heavy cometary pickup ions on bispherical diffusion characteristics. https://ntrs.nasa.gov/citations/19930036985

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