从GPS TEC、O+-H+跃迁高度和离子探空仪数据推导出的电子密度剖面

N. Jakowski, S. Stankov, I. Kutiev
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引用次数: 12

摘要

提出了一个新的峰高以上电子密度分布公式。该公式基于爱泼斯坦层,取决于O和H标度高度以及OH跃迁能级。两个标尺高度的比例都是1:16,减少的因子表示从磁力线方向到垂直方向的变化。从同一位置的gps导出的TEC中减去TEC的底部部分(通过使用foF2, M3000F2和foE测量计算)。然后使用上部TEC和经验获得的O-H过渡水平来推断未知的尺度高度。该方法在太阳活动高低两种情况下的实测数据上得到了验证。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Electron density profiles deduced from GPS TEC, O+-H+transition height and ionosonde data
A new formula of the electron density profiles above the peak height is introduced. The formula is based on the Epstein layer and depends on the O and H scale heights and the OH transition level. Both scale heights have a ratio 1:16 reduced by a factor representing the change from magnetic field line direction to vertical direction. The bottom-side part of TEC (calculated by using foF2, M3000F2 and foE measurements) is subtracted from the GPSderived TEC at the same location. The topside TEC, together with the empirically obtained O-H transition level, are then used to deduce the unknown scale heights. The method is demonstrated on actual data covering low and high solar activity conditions.
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来源期刊
Acta Geodaetica et Geophysica Hungarica
Acta Geodaetica et Geophysica Hungarica 地学-地球化学与地球物理
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