Bounce-averaged Hamiltonian for charged particles in an axisymmetric but nondipolar model magnetosphere
Journal Article
·
· Journal of Geophysical Research
- Lockheed Alto Research Lab., CA (United States)
- The Aerospace Corporation, El Segundo, CA (United States)
In order to facilitate bounce-averaged guiding center simulations of geomagnetically trapped particles, the authors express the kinetic energy of a particle with magnetic coordinates (L,{Phi}) as an analytic function of the first two adiabatic invariants (M, J) and the L value of the field line. The magnetic field model is axisymmetric, consisting of a dipolar B field plus a uniform southward magnetic field parallel to the dipole moment {mu}{sub E}. This model magnetosphere is surrounded by a circular equatorial neutral line whose radius b is an adjustable parameter. The L value of a field line is (by definition) inversely proportional to the flux enclosed by the corresponding magnetic shell of equatorial radius r{sub O}, and the L value at the neutral line (r{sub 0}=b) is denoted L{sup *}. The azimuthal coordinate {Phi} measures magnetic local time. This representation, which leads (except for a manageable small region of parameter space) to better than 1% accuracy in the specification of B{sub m} as a function of K and L, allows bounce-averaged guiding center simulations to be performed without actually tracing the bounce motions of individual particles. This formulation thus provides a computationally efficient method for tracing the bounce-averaged adiabatic motion (conserving all three invariants) and nonadiabatic transport (violating the third invariant while conserving the first two invariants) of geomagnetically trapped particles in the model magnetosphere. 18 refs., 5 figs., 2 tabs.
- OSTI ID:
- 166205
- Journal Information:
- Journal of Geophysical Research, Journal Name: Journal of Geophysical Research Journal Issue: A4 Vol. 100; ISSN 0148-0227; ISSN JGREA2
- Country of Publication:
- United States
- Language:
- English
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