Estimation of initial auroral proton energy fluxes from Doppler profiles

F. Sigernes
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引用次数: 13

Abstract

An energetic auroral proton entering the atmosphere will, by charge exchange in collisions with atmospheric constituents, alternate between being a proton H+ and a neutral hydrogen atom H. This study provides a procedure to evaluate the auroral Doppler shifted and broadened hydrogen Balmer profile as a function of initial energy, flux, pitch angle and view angle relative to the geomagnetic field. The differential proton energy flux entering the atmosphere is deduced using ground-based measurements of Hα and Hβ from Nordlysstasjonen in Adventdalen, Longyearbyen. The main assumptions are that the geomagnetic field lines are: parallel and vertical, and that the pitch angle of the H/H+-particle is preserved in collisions with atmospheric constituents before being thermalized. This numerical method estimates the fate of the auroral H/H+-particle in the atmosphere, and from measured Doppler profiles the corresponding incoming particle flux can be deduced. Optimization of the method will continue through extensive use of observational data.

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从多普勒谱估计初始极光质子能量通量
高能极光质子进入大气后,通过与大气成分碰撞的电荷交换,在质子H+和中性氢原子H之间交替存在。本研究提供了一种计算极光多普勒位移和加宽氢巴尔默剖面与初始能量、通量、俯俯角和相对于地磁场的视角的函数关系的方法。通过在朗伊尔城的Adventdalen的Nordlysstasjonen对Hα和Hβ的地面测量,推导了进入大气的差分质子能量通量。主要的假设是地磁力线是平行和垂直的,并且H/H+粒子的俯仰角在被热化之前与大气成分碰撞时保持不变。该数值方法估计了大气中极光H/H+粒子的命运,并从测量的多普勒谱图可以推导出相应的入射粒子通量。通过广泛使用观测数据,将继续优化该方法。
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