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根据高纬度图曼尼天文台部分反射雷达测量数据以及极地地球物理研究所的模型得出的2017年3月1日至31日期间地球电离层D区垂直电子密度剖面数据。

Earth's 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 Institute's model.

作者信息

Gomonov Aleksandr, Yurik Roman, Zolotov Oleg

机构信息

Polar Geophysical Institute, Murmansk, Murmansk Region, 183010 Russia.

Murmansk Arctic State University, Murmansk, Murmansk Region, 183025 Russia.

出版信息

Data Brief. 2020 Jun 12;31:105848. doi: 10.1016/j.dib.2020.105848. eCollection 2020 Aug.

Abstract

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].

摘要

对地球高纬度D区电离层的测量很少能以高时间分辨率持续进行。本文提供了2017年3月1日至31日期间D区电子密度变化的观测数据和模拟数据,分辨率为1分钟。这两个数据集具有相同的数据文件结构和命名惯例。D区电子密度观测是使用位于图曼尼天文台(北纬69.0°,东经35.7°)的地基垂直探测中频(MF)部分反射雷达进行的。同期,利用极地地球物理研究所的平静期D区电离层理论模型对D区电离层电子密度变化进行了模拟。这些数据集在以下方面具有重要价值:(a)验证和交叉比较现有的D区电离层模型;(b)验证和改进高频波段无线电波传播模型;(c)研究地球电离层波导特性与波导下部(即D区,通常称为D层)特征的依赖关系。这两个数据集对于获得戈莫诺夫及其合著者[2019年,doi:10.1051/epjconf/201922403011]报告结果的可重复性是必需的。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/3ce1/7306606/86998210d9ca/gr1.jpg

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