During the Juno perijove explorations from 27 August 2016 through 1 September 2017, strong electromagnetic impulses induced by Jupiter lightning were detected by the Microwave Radiometer (MWR) instrument in the form of 600-MHz sferics and recorded by the Waves instrument in the form of Jovian low-dispersion whistlers discovered in waveform snapshots below 20 kHz. We found 71 overlapping events including sferics, while Waves waveforms were available. Eleven of these also included whistler detections by Waves. By measuring the separation distances between the MWR boresight and the whistler exit point, we estimated the distance whistlers propagate below the ionosphere before exiting to the magnetosphere, called the coupling distance, to be typically one to several thousand of kilometers with a possibility of no subionospheric propagation, which gives a new constraint on the atmospheric whistler propagation.
CITATION STYLE
Imai, M., Santolík, O., Brown, S. T., Kolmašová, I., Kurth, W. S., Janssen, M. A., … Levin, S. M. (2018). Jupiter Lightning-Induced Whistler and Sferic Events With Waves and MWR During Juno Perijoves. Geophysical Research Letters, 45(15), 7268–7276. https://doi.org/10.1029/2018GL078864
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