Periodic Modulation of the Upper Ionosphere by ULF Waves as Observed Simultaneously by SuperDARN Radars and GPS/TEC Technique

• Published in: Journal of geophysical research. Space physics Vol. 125; no. 7
• Main Authors: Kozyreva, Olga V., Pilipenko, Vyacheslav A., Bland, Emma C., Baddeley, Lisa J., Zakharov, Victor I.
• Format: Journal Article
• Language: English
• Published: 01.07.2020
• Subjects: geomagnetic field; ionosphere modulation; SuperDARN radar; total electron content; ULF waves
• ISSN: 2169-9380; 2169-9402
• DOI: 10.1029/2020JA028032

Recent work has demonstrated that global Pc5 pulsations observed by ground‐based magnetometers may be accompanied by periodic oscillations in the total electron content (TEC) of the ionosphere measured by GPS receivers. These TEC observations may provide new insights into magnetosphere‐ionosphere coupling mechanisms, especially when combined with other ground‐based observational techniques. Presented in this paper is a large‐scale morning sector Pc5 event which was observed simultaneously by ground‐based magnetometers, two high‐frequency Super Dual Auroral Radar Network (SuperDARN) radars, and several Global Positioning System (GPS)/TEC receivers. The transient 2.6 mHz pulsations observed by the ground magnetometers and radars are accompanied by periodic fluctuations in the time rate‐of‐change of TEC (ROT) at the same frequency. To investigate possible mechanisms for the TEC modulation by ultralow frequency (ULF) waves, we determine the ratios between the spectral amplitudes of the magnetic, ionospheric Doppler velocity and ROT oscillations. The relationship between the simultaneous magnetic field and ionospheric Doppler velocity oscillations can be reasonably well interpreted using the theory of Alfven wave interaction with the thin ionospheric layer. Though the observed ratio between ROT and Doppler velocity amplitudes can be explained by the occurrence of local steep gradient of the topside ionosphere plasma at auroral latitudes, the responsible modulation mechanism cannot be considered as firmly established. Key Points Large‐scale 2.6 mHz Pc5 waves are detected simultaneously by ground magnetometers, SuperDARN radars, and several GPS/TEC receivers Relationship between geomagnetic and ionospheric velocity oscillations is interpreted using theory of MHD wave interaction with ionosphere Observed ratio between rate‐of‐change of TEC and Doppler velocity amplitudes can be explained by occurrence of local steep gradient