Use positive angular frequencies and abbreviate p=ωpe, b=ωce. The left-handed index is nL2=1−p2/[ω(ω+b)]. It is negative below its positive zero,For the right-handed mode, nR2=1−p2/[ω(ω−b)]. Below the cyclotron resonance 0<ω<b its denominator is negative and the index square is positive. Just above the resonance it is negative untilThis is the lossless electron-only cold-plasma model. Ions, collisions and resonance absorption matter outside its applicable range.
ωL=2b2+4p2−b.
ωR=2b+b2+4p2,b<ω<ωR is the stop band.
For a whistler with ω≪b and p2/(ωb)≫1,The travel time through a uniform slab is t−ts=Lpω−1/2/(2cb). In terms of ordinary frequency,An arbitrary emission time changes the intercept, not the slope. The original figure labels a dispersion constant D=81±0.5Hz1/2s: it is the reciprocal of the plotted slope, not the slope itself. ThereforeFor B=80 nT and L=6.0×107 m this gives b≃1.41×104s−1, p≃2.41×105s−1, andThe resulting forbidden right-handed frequency width isThe lower edge is about 2.24 kHz and the upper edge about 39.5 kHz. In the real nonuniform plasma, the travel-time coefficient measures a path integral proportional to ∫ωpe/ωceds. The inferred density is consequently an effective uniform-slab estimate, not a unique local density at the spacecraft. Uncertainty in the path and magnetic field likely exceeds the formal error in D.
k≃cbpω,vg=(dωdk)−1≃p2cbω.
dtd(f−1/2)=Lp2c2πb.
p=L2c2πbD,b=meeB.
ne=e2ε0mep2≃1.8×107m−3≃18cm−3.
Δf=2πωR−b=4πb2+4p2−b≃3.7×104Hz.
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