A pure single chorus element can promptly accelerate seed electrons to energies of mega-electron-volts through wave-particle interactions (Foster et al., 2017). Additionally, an isolated chorus element can rapidly scatter energetic electrons over a very wide energy range in the magnetosphere into the loss cone, and then illuminate flash auroras in the ionosphere Abstract Flash aurora driven by an isolated chorus element can be a useful ionospheric indicator for identifying the source wave properties via wave-particle interactions. Using ground observation and modeling approaches, here we report the temporal characteristics of flash aurora that depend on the chorus frequency width and the sweep rate. We found that the contraction time increases more than the expansion time in patchy auroral variations, due to the difference in the minimum electron energies resonated with the chorus wave packet away from the equatorial source to higher latitudes. Especially, the contraction time strongly depends on the higher-frequency chorus waves due to cyclotron resonance with lower-energy electrons. The model calculations support that the chorus element ranges from lower-band to upper-band frequencies with respect to half the gyrofrequency at the exact generation region. Our study provides the prompt (milliseconds) chorusdriven electron dynamics through the spatiotemporal characteristics of flash aurora in the ionosphere.
Plain Language SummaryThe wave frequency of a chorus wave, which is one of the electromagnetic wave emissions in magnetized plasmas, is an important parameter for characterizing energetic particles in the Earth's magnetosphere. Even though chorus waves are classified into two bands-lower-and upper-band frequencies separated at half the electron gyrofrequency-it is not well established that both lower-and upper-band chorus are essentially the same at the generation region. In this study, we investigate temporal characteristics of specific aurora caused by discrete chorus elements to identify the whole frequency band of chorus waves at the magnetospheric generation region. The aurora reflects the physical properties of the magnetospheric processes through the geomagnetic field lines from the generation region; thus, the aurora in the ionosphere becomes an ionospheric display on which the magnetospheric chorus waves are generated. Using auroral images along with model calculations, we find that the contraction time is longer than the expansion time as auroras vary their shape, depending on the frequency width of chorus wave packets. This study provides a new insight into the role of rapid (milliseconds) resonant interaction processes between discrete chorus elements and electrons over a wider energy range.