HR: 1330h
AN: SM42C-0617 [PDF]
TI: Radiation Belt Modeling: Implementation Issues When Solving Three-dimensional Diffusion
Equations
AU: * Ginet, G P
EM: gregory.ginet@hanscom.af.mil
AF: Space Vehicles Directorate, Air Force Research Laboratory, AFRL/VSBX
29 Randolph Rd, Hanscom AFB, MA 01731 United States
AU: Young, S L
EM: shawn.young@hanscom.af.mil
AF: Space Vehicles Directorate, Air Force Research Laboratory, AFRL/VSBX
29 Randolph Rd, Hanscom AFB, MA 01731 United States
AU: Albert, J M
EM: jay.albert@hanscom.af.mil
AF: Institute for Scientific Research, Boston College, 140 Commonwealth Ave, Boston, MA 02467 United States
AB:
The Diffusion in I, L, and B Energetic Radiation Tracker (DILBERT) is being developed by AFRL to model radiation belt
dynamics on both radial and pitch-angle diffusive time-scales with a realistic magnetic field model in three dimensions,
where one of the dimensions is parameterized by the $L$ shell. Large spatial variations in the pitch-angle
($D_{\alpha\alpha}$), energy ($D_{EE}$) and cross-term ($D_{\alpha E}$) quasi-linear diffusion coefficients make the
calculations challenging. Two basic aspects of the calculation will be considered here, the variable sub-space in which the
diffusion is computed, i.e pitch angle--energy, \{$\alpha_{eq}$,$E$\}, or adiabatic invariant, \{$\mu$,$J$\}, and constraints
on the grid size. In the \{$\alpha_{eq},E$\}
space the coefficients compare to each other as $|D_{\alpha\alpha}|\gg|D_{\alpha E}|\gg|D_{EE}|$, while in \{$\mu,J$\} space,
the coefficients $D_{\mu\mu}, D_{\mu J}$ and $D_{JJ}$, have the relation, $|D_{\mu\mu}|\sim|D_{\mu J}|\sim|D_{JJ}|$. Pitch
angle--energy space is attractive in two dimensions because the dominance of $D_{\alpha\alpha}$ makes the calculation almost
one dimensional. Complications are introduced, however, by including the third dimension and it is argued that adiabatic
invariant space is the better choice. Large spatial gradients in the coefficients in either variable space cause
``convective'' behavior in the numerical formulation of the equations. Based on estimated timescales for the ``convective''
and ``diffusive'' components of the equation constraints are derived on the grid resolution and it is shown that the required
grid spacing varies by orders of magnitude.
DE: 2720 Energetic particles, trapped
DE: 2722 Forecasting
DE: 2753 Numerical modeling
SC: SPA - Magnetospheric Physics [SM]
MN: 2003 Fall Meeting