Abstract

AbstractAccurate geolocation of ionospheric backscatter measured by the Super Dual Auroral Radar Network (SuperDARN) high‐frequency radars is critical for the integrity of polar ionospheric convection maps, which involve combining SuperDARN line‐of‐sight velocity measurements originating from multiple locations. Geolocation requires estimation of the propagation paths of the high‐frequency radio signal to and from the scattering volume. The SuperDARN radars comprise both a main and interferometer antenna array to allow the estimation of the elevation angle of arrival of the returning signal, and hence its most likely propagation path. However, over the history of operation of SuperDARN (>20 years) elevation angle data have not been routinely used owing to problems with the calibration of phase difference measurements. Instead, virtual height models have been used to estimate the most likely propagation paths, and these are often of limited accuracy. Here we present a method for calibrating SuperDARN interferometer measurements using backscatter from meteor trails measured in the near field‐of‐view of the SuperDARN radars. We present estimates of calibration factors for the SuperDARN radar in Saskatoon, Canada, at different temporal resolutions: 3 months, 10 days, and 1 day. The calibration factor varies over the 9‐year interval studied, such that employing a single value for the whole interval would lead to significant errors in elevation angle measurements at times. The higher‐resolution results show the ability of the technique to determine the calibration factor routinely at a high time resolution.

Highlights

  • The Super Dual Auroral Radar Network (SuperDARN) facilitates the study of ionospheric and magnetospheric dynamics in the Earth’s polar regions (Chisham et al, 2007)

  • Doppler velocity measurements are made at locations where the high-frequency (HF) radio signals transmitted by the SuperDARN radars are backscattered to the radar from magnetic field-aligned density irregularities in the F region ionosphere (Weaver, 1965), which move under the influence of the convection electric field (Villain et al, 1985)

  • As with many other SuperDARN radars, during this epoch the Saskatoon radar operated at different frequencies at different times of the day, year, and solar cycle, in order to maximize the amount of ionospheric F region backscatter

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Summary

Introduction

The Super Dual Auroral Radar Network (SuperDARN) facilitates the study of ionospheric and magnetospheric dynamics in the Earth’s polar regions (Chisham et al, 2007). The SuperDARN radars are equipped with interferometers that make it possible to determine the elevation angle of arrival of the returning radio signals and, to estimate the most likely propagation modes and propagation path (André et al, 1998; Burrell et al, 2015; Chisham & Freeman, 2013; McDonald et al, 2013; Milan et al, 1997; Shepherd, 2017). Using this information makes it possible to accurately estimate the geographic location of the scattering volume

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