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首页> 外文期刊>Radio Science >A study of the shape of topside electron density profile derived from incoherent scatter radar measurements over Arecibo and Millstone Hill
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A study of the shape of topside electron density profile derived from incoherent scatter radar measurements over Arecibo and Millstone Hill

机译:从非相干散射雷达在Arecibo和Millstone Hill上的测量得出的顶侧电子密度分布形状的研究

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摘要

The shape of the topside electron density (Ne) profile is studied using incoherent scatter radar (ISR) measurements. On the basis of more than 90,000 and 84,000 Ne profiles measured over Arecibo (18.4°N, 66.7°W, dip 49.7°) and Millstone Hill (42.6°N, 71.5°W, dip 71.6°), respectively, shape factors have been derived by fitting the ISR observed profile using a Chapman-type layer with a height-independent scale height. The results reveal that the shape factor shows a general departure from the typically used values of 0.5 (Chapman α layer) except during the night and also undergoes appreciable variation with local time, season, solar activity, and latitude. Over Arecibo, the averaged shape factor is characterized by a daytime maximum of ∼0.55–0.75, a nearly constant nighttime value close to 0.5, and a marked morning decline; over Millstone Hill, the shape factor shows pronounced seasonal variations, and the diurnal variation in summer is opposite to that in other seasons. Over both stations, the shape factor exhibits a high correlation with the F2 layer peak electron density (NmF2), and it has strong solar cycle dependence during the late morning hours. It indicates that the temperature structure of the topside ionosphere can explain much of the variation of the shape factor when the plasma density is low, especially during nighttime. During daytime hours, the topside shape factor is thought to be associated with ion-neutral drag during periods of large plasma density.
机译:使用非相干散射雷达(ISR)测量研究了顶部电子密度(Ne)轮廓的形状。根据分别在阿雷西博(18.4°N,66.7°W,倾角49.7°)和Millstone Hill(42.6°N,71.5°W,倾角71.6°)上分别测量的90,000和84,000 Ne剖面,形状因子已经确定通过使用Chapman型层与高度无关的标度高度拟合ISR观察到的轮廓而得出。结果表明,形状因子显示出与通常使用的0.5(Chapmanα层)的值大致不同,除了在夜间,并且还随当地时间,季节,太阳活动和纬度发生明显变化。在阿雷西博(Arecibo),平均形状因子的特征是白天的最大值约为0.55-0.75,夜间值几乎恒定,接近0.5,并且早晨明显下降。在磨石山上空,形状因子显示出明显的季节变化,夏季的日变化与其他季节相反。在这两个站点上,形状因子都与F2层的峰值电子密度(NmF2)具有高度相关性,并且在清晨时段具有很强的太阳周期依赖性。这表明当等离子体密度低时,尤其是在夜间,顶侧电离层的温度结构可以解释形状因子的大部分变化。在白天,顶面形状因子被认为与大血浆密度期间的离子中性阻力有关。

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  • 来源
    《Radio Science》 |2006年第4期|1-11|共11页
  • 作者单位

    National Satellite Meteorological Center, Chinese Meteorological Administration, Beijing, China., Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing, China.;

    Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing, China.;

    Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing, China.;

    Now at High Altitude Observatory, National Center for Atmospheric Research, Boulder, Colorado, USA., Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing, China.;

    Haystack Observatory, Massachusetts Institute of Technology, Westford, Massachusetts, USA.;

    Haystack Observatory, Massachusetts Institute of Technology, Westford, Massachusetts, USA.;

    Arecibo Observatory, National Astronomy and Ionosphere Center, Arecibo, Puerto Rico.;

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  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类
  • 关键词

    Shape; Ionosphere; Observatories; Databases; Radar measurements; Radar scattering;

    机译:形状;电离层;天文台;数据库;雷达测量;雷达散射;

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