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].

Highlights

  • 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

  • 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)

  • Earth and Planetary Sciences Earth’s ionosphere D-Region observations and modelling Compressed archive of standard ASCII plain text files Experimental data were derived from partial reflection radar measurements

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Summary

Data accessibility Related research article

Earth and Planetary Sciences Earth’s ionosphere D-Region observations and modelling Compressed (zipped) archive of standard ASCII plain text files Experimental (observed) data were derived from partial reflection radar measurements. The following models (listed in alphabetical order) could be contrasted against the published with this paper datasets: (a) the Absorption by the D and E Region of HF signals with NORMAL Incidence (ABBYNormal) model [2]; (b) D-Region Absorption Prediction (D-RAP) model [3]; (c) International Reference Ionosphere (IRI) model [4]; (d) Sodankylä Ion Chemistry (SIC) model [5]; (e) Thermosphere Ionosphere Mesosphere Electrodynamics General Circulation (TIME-GCM) model [6]; (f) Whole Atmosphere Community Climate Model with D-region ion chemistry (WACCM-D) [7] These datasets are required to gain the reproducibility of reported by Gomonov and co-auth. These datasets are required to gain the reproducibility of reported by Gomonov and co-auth. [1] results

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