The kinetic shell model of coronal heating and acceleration by ion cyclotron waves 1. Outward propagating waves

Citation
Pa. Isenberg et al., The kinetic shell model of coronal heating and acceleration by ion cyclotron waves 1. Outward propagating waves, J GEO R-S P, 106(A4), 2001, pp. 5649-5660
Citations number
64
Categorie Soggetti
Space Sciences
Journal title
JOURNAL OF GEOPHYSICAL RESEARCH-SPACE PHYSICS
ISSN journal
21699380 → ACNP
Volume
106
Issue
A4
Year of publication
2001
Pages
5649 - 5660
Database
ISI
SICI code
0148-0227(20010401)106:A4<5649:TKSMOC>2.0.ZU;2-M
Abstract
We introduce a new kinetic treatment of the heating of the magnetically ope n solar corona and the acceleration of the fast solar wind by the cyclotron resonant interaction of coronal protons with ion cyclotron waves. In this "kinetic shell" formalism we approximate the evolution of the collisionless coronal proton distribution by the assumption that the pitch angle diffusi on due to the resonant ion cyclotron waves is much faster than the other pr ocesses taking place. Under this assumption the resonant protons uniformly populate velocity space surfaces, or shells, of constant energy in the fram e moving with the wave phase speed. These resonant shells then evolve slowl y in response to the nonresonant large-scale forces in the system. For this initial demonstration of the kinetic shell concept, we additionally take t he resonant waves to be solely outward propagating and dispersionless. In t his case the resonant shells are spherical sections in velocity space which are confined to the sunward half of the proton distribution. We then calcu late the radial evolution of collisionless protons in a coronal hole using this simplified system, which also includes the effects of gravity, the cha rge-separation electric field, and the mirror force. We find that a fast so lar wind can be generated by this process using reasonable values of the ph ysical parameters. However, we also prove that the proton distribution gene rated by the interaction with only outward propagating waves will necessari ly be unstable to the generation of inward propagating waves. Thus this ill ustrative calculation is incomplete and will have to be extended to include waves in both propagation directions.