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Inferring Source Properties of Monoenergetic Electron Precipitation From Kappa and Maxwellian Moment‐Voltage Relationships

机译:从κ和麦克斯韦矩-电压关系推断单能电子沉淀的源性质

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摘要

We present two case studies of FAST electrostatic analyzer measurements of both highly nonthermal ( κ 2.5) and weakly nonthermal/thermal monoenergetic electron precipitation at ∼4,000 km, from which we infer the properties of the magnetospheric source distributions via comparison of experimentally determined number density‐, current density‐, and energy flux‐voltage relationships with corresponding theoretical relationships. We also discuss the properties of the two new theoretical number density‐voltage relationships that we employ. Moment uncertainties, which are calculated analytically via application of the Gershman et al. (2015, ) moment uncertainty framework, are used in Monte Carlo simulations to infer ranges of magnetospheric source population densities, temperatures, κ values, and altitudes. We identify the most likely ranges of source parameters by requiring that the range of κ values inferred from fitting experimental moment‐voltage relationships correspond to the range of κ values inferred from directly fitting observed electron distributions with two‐dimensional kappa distribution functions. Observations in the first case study, which are made over ∼78–79° invariant latitude in the Northern Hemisphere and 4.5–5.5 magnetic local time, are consistent with a magnetospheric source population density n m= 0.7–0.8 cm−3, source temperature T m≈ 70 eV, source altitude h= 6.4–7.7 R E, and κ= 2.2–2.8. Observations in the second case study, which are made over 76–79° invariant latitude in the Southern Hemisphere and ∼21 magnetic local time, are consistent with a magnetospheric source population density n m= 0.07–0.09 cm−3, source temperature T m≈ 95 eV, source altitude h 6 R style="italic-in-any-context">E, and style="italic-in-any-context">κ= 2–6.
机译:我们提供了两个FAST静电分析仪测量两种高度非热的案例研究( κ [math> 2.5)和约4,000 km处的弱非热/热单能电子沉淀,由此我们可以通过以下方法推断出磁层源分布的性质实验确定的数密度,电流密度和能量通量-电压关系与相应的理论关系的比较。我们还将讨论我们采用的两个新的理论数密度-电压关系的性质。矩不确定性,可以通过应用Gershman等人的方法进行解析计算。 (2015,)矩不确定性框架用于蒙特卡洛模拟,以推论磁层源人口密度,温度,κ值和高度的范围。我们通过要求从拟合实验矩-电压关系推断出的κ值范围与从直接拟合观测到的具有二维kappa分布函数的电子分布推断出的κ值范围相对应,来确定源参数的最可能范围。在第一个案例研究中,在北半球约78-79°不变纬度和4.5-5.5磁局部时间上进行的观测,与磁层源人口密度nm = 0.7-0.8cm cm -3 < / sup>,源温度Tm≈70eV,源高度h = 6.4-7.7RE,κ= 2.2-2.8。第二个案例研究的观测值是在南半球的76-79°不变纬度和21个磁本地时间进行的,与磁层源人口密度nm = 0.07-0.09 cm −3 ,源温度Tm≈95eV,源高度<数学xmlns:mml =“ http://www.w3.org/1998/Math/MathML” id =“ nlm-math-2” overflow =“ scroll”> h 6 R style =“ italic-in-any-context”> E 和 style =“ italic- in-any-context“>κ = 2-6。

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