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Inferring magnetospheric heavy ion density using EMIC waves

机译:推断磁性层的重离子密度使用位的波

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We present a method to infer heavy ion concentration ratios from electromagnetic ion cyclotron (EMIC) wave observations that result from ion-ion hybrid (IIH) resonance. A key feature of the IIH resonance is the concentration of wave energy in a field-aligned resonant mode that exhibits linear polarization. These mode-converted waves at the IIH resonance are localized at the location where the frequency of a compressional wave driver matches the IIH resonance condition, which depends sensitively on the heavy ion concentration. This dependence makes it possible to estimate the heavy ion concentration ratio. In this paper, we evaluate the absorption coefficients at the IIH resonance at Earth's geosynchronous orbit for variable concentrations of He~+ and wave frequencies using a dipole magnetic field model. We find that the resonance only occurs over a limited range of wave frequency such that the IIH resonance frequency is close to but not exactly the same as the crossover frequency. Using the wave absorption and EMIC waves observed from the GOES 12 satellite, we demonstrate how this technique can be used to estimate the He~+ concentration of around 4% near L = 6.6 assuming electron-H~+-He~+ plasma.
机译:我们提出一个方法来推断重离子从电磁离子浓度比率回旋加速器(位的)波的观测结果从离子间混合(IIH)共振。IIH共振的特点是浓度field-aligned波浪能量的共振模式展品线性极化。在IIH mode-converted波共振本地化的频率位置一个压缩波驱动匹配IIH敏感取决于共振条件沉重的离子浓度。可以估计重离子浓度比。在IIH共振吸收系数在地球同步轨道的变量他~ +和波频率使用浓度一个偶极磁场模型。共振只在有限的范围内发生波的频率,这样IIH共振频率接近但不完全一样交叉频率。吸收和波位的观察12颗卫星,我们演示这种技术可以用来估计他~ +的浓度大约4% L = 6.6附近假设electron-H ~ +他~ +等离子体。

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