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Terrestrial magnetospheric imaging: numerical modeling of low-energy neutral atoms

机译:地面磁层成像:低能中性原子的数值模拟

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Abstract: Imaging of the terrestrial magnetosphere can be performed by detection of low energy neutral atoms (LENAs) that are produced by charge exchange between magnetospheric plasma ions and cold neutral atoms of the Earth's geocorona. As a result of recent instrumentation advances it is now feasible to make energy-resolved measurements of LENAs from less than 1 keV to greater than 30 keV. To model expected LENA fluxes at a spacecraft, we initially used a simplistic, spherically symmetric magnetospheric plasma model. We now present improved calculations of both hydrogen and oxygen line-of-sight LENA fluxes expected on orbit for various plasma regimes as predicted by the Rice University Magnetospheric Specification Model. We also estimate expected image count rates based on realistic instrument geometric factors, energy passbands, and image accumulation intervals. The results indicate that presently proposed LENA instruments are capable of imaging of storm time ring current and potentially even quiet time ring current fluxes, and that phenomena such as ion injections from the tail and subsequent drifts toward the dayside magnetopause may also be deduced.!17
机译:摘要:地球磁层的成像可以通过检测低能中性原子(LENA)来进行,该低能中性原子是由磁层等离子体离子与地球电晕的冷中性原子之间的电荷交换产生的。由于最近仪器的进步,现在可行的是,对LENA的能量分辨测量从小于1 keV到大于30 keV。为了在航天器上模拟预期的LENA通量,我们最初使用了一个简单的球对称磁层等离子体模型。现在,我们根据莱斯大学磁层规范模型的预测,提出了针对各种等离子体状态在轨道上预期的氢和氧视线LENA通量的改进计算方法。我们还会根据实际的仪器几何因素,能量通带和图像累积间隔来估计预期的图像计数率。结果表明,目前提出的LENA仪器能够对风暴时间环电流甚至潜在的安静时间环电流通量进行成像,并且还可以推断出诸如从尾部注入离子以及随后向日间磁更年期漂移的现象。!17

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