首页> 美国卫生研究院文献>Data in Brief >Earths ionosphere D-region vertical electron density profile data during March 1-31 2017 according to high-latitudinal Tumanny observatory partial reflection radar measurements and Polar Geophysical Institutes model
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Earths ionosphere D-region vertical electron density profile data during March 1-31 2017 according to high-latitudinal Tumanny observatory partial reflection radar measurements and Polar Geophysical Institutes model

机译:地球的电离层D区垂直电子密度剖面数据在2017年3月1日至31日根据高纬度肿瘤天文台部分反射雷达测量和极地地球物理学院的模型

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摘要

The Earth's high-latitudinal D-Region ionosphere measurements are rarely performed continuously and with high temporal resolution. This data article provides the observed and modelled data on D-Region electron density variations during March 1-31, 2017 with 1-minute resolution. Both datasets share the same data-files’ structure and naming conventions. D-Region electron density observations were performed with the ground-based vertical sounding medium frequency (MF) partial reflection radar located at Tumanny observatory (69.0°N, 35.7°E). Modelling of D-Region ionosphere electron density variations were performed for the same period using Polar Geophysical Institute's theoretical model of quiet-time D-Region ionosphere. These datasets are valuable (a) to validate and cross-compare existing models of the D-Region ionosphere, (b) to verify and improve HF-band radio-waves propagation models, and (c) in investigations of the Earth's-ionosphere waveguide properties in dependence on the features of the lower part of the waveguide, i.e., the D-Region (often referenced to as the D-Layer). Both datasets are required to gain the reproducibility of results reported by Gomonov and co-authors [2019, doi: 10.1051/epjconf/201922403011].
机译:地球的高纬度D-区域电离层测量很少连续进行,并且具有高的时间分辨率。该数据文章在2017年3月1日至31日,2017年3月1日至31日的D-Region电子密度变化提供了观察和建模数据,具有1分钟的分辨率。两个数据集共享相同的数据文件的结构和命名约定。通过位于肿瘤天文台(69.0°N,35.7°E)的地基垂直探测介质(MF)部分反射雷达进行D区电子密度观察。 D型电离层电子密度变异的建模在使用极地D型电离区的理论模型的同一时期进行了同一时期。这些数据集是有价值的(a),用于验证和交叉比较D区域电离层,(b)的现有模型,以验证和改善HF频带无线电波传播模型,(c)在地球电离层波导的研究中属性依赖于波导下部的特征,即D区(通常称为D层)。两个数据集都需要获得Gomonov和共同作者报告的结果的再现性[2019,DOI:10.1051 / EPJCONF / 201922403011]。

著录项

  • 期刊名称 Data in Brief
  • 作者单位
  • 年(卷),期 2020(-1),-1
  • 年度 2020
  • 页码 -1
  • 总页数 7
  • 原文格式 PDF
  • 正文语种
  • 中图分类
  • 关键词

    机译:电离层D区域;D层;电子密度;垂直探测;部分反射雷达;观察;建模;

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