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Numerical calculations of relativistic electron drift loss effect

机译:数值计算的相对论性电子漂移损失的影响

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It has been suggested that drift loss to the magnetopause can be one of the major loss mechanisms contributing to relativistic electron flux dropouts. In this study, we examine details of relativistic electrons' drift physics to determine the extent to which the drift loss through the magnetopause is important to the total loss of the outer radiation belt. We have numerically computed drift paths of relativistic electrons' guiding center for various pitch angles, various measurement positions, and different solar wind conditions using the Tsyganenko T02 model. We specifically demonstrate how the drift loss effect depends on these various parameters. Most importantly, we present various estimates of relative changes of the omnidirectional flux of 1 MeV electrons between two different solar wind conditions based on a simple form of the directional flux function. For a change of the dynamic pressure from 4 nPa to 10 nPa with a fixed IMF B Z = 0 nT, our estimate indicates that after this increase in pressure, the equatorial omnidirectional flux at midnight near geosynchronous altitude decreases by ~56 to ~97%, depending on the specific pitch angle dependence of the directional flux. The effect rapidly decreases at regions earthward of geosynchronous orbit and shows a general trend of decrease away from midnight. For a change of the IMF B Z from 0 nT to ?15 nT with a fixed dynamic pressure of 4 nPa, the relative decrease of the omnidirectional flux at geosynchronous altitude on the nightside is much smaller than that for the pressure increase, but its effect becomes substantial only beyond geosynchronous orbit. Possibilities exist that our results may change to some extent for a different magnetospheric model than the one used here.
机译:有人建议,漂移损失磁层可以是一个主要的损失机制导致相对论性电子通量辍学。物理学相对论电子的漂移确定漂移损失的程度通过磁层是很重要的外辐射带的全损。数值计算相对论的漂移路径电子对各种沥青的指导中心角度、不同测量位置不同的太阳风条件下使用Tsyganenko T02模型。漂移损失效应取决于这些如何各种参数。各种估计的相对变化全向1兆电子伏电子通量之间基于两种不同的太阳风条件简单形式的定向流量功能。变化的动态压力4 nPa 10nPa与一个固定的货币基金组织B Z = 0元,我们的估计表明在压力增加后,在午夜赤道全方位通量附近的同步高度减少~ 56~ 97%,这取决于特定的螺旋角依赖的方向变化。迅速减少的地区向地面地球同步轨道和显示的总趋势减少从午夜。国际货币基金组织(IMF) B Z从0元? 15元一个固定的动态4 nPa,压力的相对减少全向通量在同步轨道高度在阴面比这小得多压力增加,但其效果大量只超出地球同步轨道。可能性的存在,我们的结果可能会发生变化在某种程度上不同的磁性层的比这里使用的一个模型。

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