Van Allen Beltinator 3D Fokker-Planck Radiation Belt Explorer
Rendering T+0.0h
Physics Parameters
L* (Drift Shell) 4.5
Energy (MeV) 1.0
Equatorial Pitch Angle α₀ (°) 45
DL*L* (Radial Diffusion) 1.0e-6 ⟲
Dpp (Momentum Diffusion) 1.0e-7
Dα₀α₀ (Pitch-Angle Diffusion) 1.0e-5
Dα₀p (Mixed Diffusion) 0 (off)
Loss Timescale τ (days) 10.0
Geomagnetic Conditions
Kp Baseline 3
Dst Index (nT) -30
Solar Wind Vsw (km/s) 400
Quiet Conditions
Kp(t) — 3-Hour Cadence Profile
0h12h24h
Visualization
Sim Speed (×) 60
Flux Intensity (cm⁻²s⁻¹sr⁻¹MeV⁻¹)
10²10⁴10⁶10⁸
Presets
Satellites (Click in 3D to zoom)
Van Allen Probes (RBSP A/B)
THEMIS A / D / E
GOES (GEO)
LEO Satellites
Lomonosov

Computed Values

T(α₀) Bounce Factor 1.0802
Phase Space Density f 2.34e-10
Differential Flux j 4.56e+04
DL*L* (Kp-driven) 1.0e-6
Kp(t) Current 3.0
Magnetopause Lmp 10.2 RE
Last Closed Drift Shell 7.8 RE
Bounce Loss Cone αBLC 3.2°
Drift Loss Cone αDLC 5.1°
Particle Status Trapped

Governing Equations

Eq.1 — Generalized Diffusion Equation
∂f/∂t = ∂/∂Jᵢ (Dᵢⱼ ∂f/∂Jⱼ)
i,j = 1,2,3

Phase space density f evolves via diffusion in the three adiabatic invariants (J₁, J₂, J₃), corresponding to gyration, bounce, and azimuthal drift motion.

Eq.2 — Fokker-Planck (no mixed terms)
∂f/∂t = L*² ∂/∂L*|μ,J (DL*L* L*⁻² ∂f/∂L*|μ,J)
+ 1/p² ∂/∂p|y,L (p² ⟨Dpp(y,p)⟩ba ∂f/∂p|y,L)
+ 1/(T(y)·y) ∂/∂y|p,L (T(y)·y·⟨Dyy(y,p)⟩ba ∂f/∂y|p,L)
− f/τ

Separates radial diffusion (L*), momentum diffusion (p), and pitch-angle diffusion (y = sin α₀) with bounce-averaged coefficients. DL*L* is now time-dependent via Kp(t).

Eq.3 — Fokker-Planck with Mixed Terms
∂f/∂t = L*² ∂/∂L*|μ,J (DL*L* L*⁻² ∂f/∂L*|μ,J)
+ 1/p² ∂/∂p|α₀,L p²(⟨Dpp⟩ ∂f/∂p + ⟨Dpα₀⟩ ∂f/∂α₀)
+ 1/(T(α₀)sin2α₀) ∂/∂α₀|p,L T(α₀)sin2α₀
  ·(⟨Dα₀α₀⟩ ∂f/∂α₀ + ⟨Dα₀p⟩ ∂f/∂p) − f/τ

Dα₀p is the mixed energy–pitch angle diffusion coefficient. Cross-diffusion terms couple momentum and pitch-angle evolution.

Bounce Period Factor T(α₀)
T(α₀) = 1.3802 − 0.3198·(sin(α₀) + sin²(α₀))

Approximation for the normalized bounce period (Schulz & Lanzerotti 1974). Particles near the loss cone have T ≈ 1.38; those near 90° have T ≈ 0.74.

DL*L*(Kp) — Brautigam & Albert 2000
DL*L* = D₀ · 10^(0.506·Kp − 9.325) · L*¹⁰

Radial diffusion coefficient parameterized by Kp index and L-shell. Higher Kp dramatically increases radial transport, driving inward diffusion and energization during storms. Kp is updated every 3 hours in this simulation.

Radiation Belt Physics

Relativistic electrons (>500 keV) undergo three periodic motions: gyration (μ), bounce (J), and azimuthal drift (Φ = L*). ULF waves drive radial diffusion, chorus waves produce local acceleration, and magnetopause shadowing causes loss on the dayside.

Magnetic Field Notes

The local B-field determines energy from μ. Because electron spectra are steep, small ΔB errors produce large flux errors — especially at high L. At LEO, populations include Trapped, BLC, and DLC electrons requiring accurate magnetic mapping to classify.

L* 4.5 RE
E 1.0 MeV
α₀ 45°
Kp(t) 3.0
DLL 1.0e-6
Model Eq.2
Sim T+0.0h